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7/27/2019 ResConsVol1 http://slidepdf.com/reader/full/resconsvol1 1/102 A CONTRIBUTION TO PROMOTE CONSERVATION OF WATER STORAGE ASSETS WORLDWIDE economic and engineering evaluation of alternative strategies for managing sedimentation in storage reservoirs  June 2003
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A CONTRIBUTION TO PROMOTE CONSERVATION OF WATER STORAGE ASSETS WORLDWIDE

economic and engineering evaluation of alternative strategies

for managing sedimentation in storage reservoirs

 June 2003

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Reservoir Conservation

Volume I:The RESCON Approach

Economic and engineering evaluationof alternative strategies for managingsedimentation in storage reservoirs

Reservoir Conservation

Volume I:

The RESCON Approach

Economic and engineering evaluationof alternative strategies for managingsedimentation in storage reservoirs

 Alessandro Palmieri, Farhed Shah

George W. Annandale, Ariel Dinar 

 June 2003

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2003 The International Bank forReconstruction and Development / THE WORLD BANK

1818 H Street, N.W., Washington, DC 20433, USA

Manufactured in the United States of America

First Printing June 2003

This publication is in two volumes: (i) the present Volume 1, the RESCON Approach; and (ii)

RESCON Model and User Manual, including a CD with the Excel program. The document carr

of the authors and should be used and cited accordingly. The findings, interpretations and co

the authors’ own and should not be attributed to the World Bank, its Board of Directors, its ma

any member countries.

About the authors:

George W. Annandale, P.E., President, Engineering and Hydrosystems Inc.

 Ariel Dinar , Lead Economist, Agriculture and Rural Development, The World Bank

 Alessandro Palmieri, Leading Dams Specialist, Quality Assurance and Compliance, The WoFarhed Shah, Associate Professor, Department of Agricultural & Resource Economics, Uni

Connecticut

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FOREWORD..........................................................................................................................RATIONALE AND SUMMARY..............................................................................................

1. INTRODUCTION AND OBJECTIVES ...........................................................................

BACKGROUND AND MOTIVATION ............................................................................................

RESCON CONTRIBUTION TO POLICY MAKING.......................................................................

THE RESCON MODEL .......................................................................................................

BOOK STRUCTURE ................................................................................................................2. RESERVOIR LIFE CYCLE MANAGEMENT ..................................................................

INTRODUCTION....................................................................................................................

DESIGN LIFE APPROACH .......................................................................................................

LIFE CYCLE MANAGEMENT APPROACH ...................................................................................

COMPARISON OF THE T WO APPROACHES ................................................................................

3. RESERVOIR SEDIMENTATION MANAGEMENT.........................................................

INTRODUCTION....................................................................................................................

THE SEDIMENTATION PROCESS ...............................................................................................

AVAILABLE SEDIMENT MANAGEMENT ALTERNATIVES .................................................................

R EDUCING SEDIMENT INFLOWS ..............................................................................................

MANAGING SEDIMENTS  WITHIN THE R ESERVOIR .......................................................................

EVACUATION OF SEDIMENTS FROM THE R ESERVOIR ...................................................................

R EPLACING LOST STORAGE ....................................................................................................

DECOMMISSIONING ..............................................................................................................

APPLICATION OF RESCON..................................................................................................

4. ENVIRONMENTAL AND SOCIAL SAFEGUARDS .......................................................

CONSEQUENCES OF  IMPLEMENTING SEDIMENT MANAGEMENT ON THE DOWNSTREAM ENVIRONMENT .

TABLE OF CONTENTS

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T H E R E S C O N A P P R O A C H

THE RESCON TOOLKIT ............................................................................................................

THE RESCON MATHEMATICAL MODEL ..........................................................................................

INTERGENERATIONAL  EQUITY AND R ETIREMENT FUND .....................................................................

CAUTIONARY R EMARKS .................................................................................................................

6. EVALUATION OF RESCON MODEL ...................................................................................

INTRODUCTION...........................................................................................................................

DESCRIPTION OF DAMS ...............................................................................................................

LONG-TERM CAPACITY .................................................................................................................

R ANKING OF SEDIMENT MANAGEMENT TECHNIQUES .......................................................................SENSITIVITY ANALYSIS ..................................................................................................................

CONCLUSIONS ............................................................................................................................

7. COUNTRY DIALOGUE ..........................................................................................................

INTRODUCTION...........................................................................................................................

KENYA ......................................................................................................................................

MOROCCO ..................................................................................................................................

SRI LANKA .................................................................................................................................

8. CONCLUSION OF THE STUDY AND RECOMMENDATIONS ..........................................

SUMMARY  OF THE PROBLEM ..........................................................................................................

SUSTAINABILITY AND INTERGENERATIONAL EQUITY ...........................................................................

SEDIMENT MANAGEMENT ALTERNATIVES .........................................................................................

ENVIRONMENTAL AND SOCIAL SAFEGUARDS ....................................................................................

AN ECONOMIC APPROACH ...........................................................................................................

POLICY IMPLICATIONS ..................................................................................................................

R ECOMMENDATIONS FOR  FURTHER  WORK.......................................................................................

9. ACKNOWLEDGEMENTS .....................................................................................................

10. REFERENCES .........................................................................................................................

ANNEX A: LAUNCH WORKSHOP ............................................................................................

ANNEX B: LITERATURE REVIEW ............................................................................................

ANNEX C: WATERSHED MANAGEMENT ...............................................................................

ANNEX D: ASSESSING FEASIBILITY OF FLUSHING ...............................................................

ANNEX E: ENVIRONMENTAL CONSIDERATIONS ................................................................

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I N T R O D U C T I O N A N D O B J E C T I V E S

Among the many sessions of the Third World WaterForum, held in Kyoto, Japan in March 2003, there

was one titled “Sedimentation Management Chal-

lenges for Reservoir Sustainability”. Two main mes-

sages emerged from that session:

 Whereas the last century was concerned with

reservoir development, the 21st century will need

to focus on sediment management; the objective

will be to convert today’s inventory of non-sus-

tainable reservoirs into sustainable infrastructures

for future generations.

The scientific community at large should work

to create solutions for conserving existing water

storage facilities in order to enable their func-

tions to be delivered for as long as possible, pos-

sibly in perpetuity.

These important messages are very much in line

with the World Bank’s Water Resources Sector Strat-

egy, which calls the institution to address manage-

ment of existing infrastructure, as well as to develop

much needed new priority investments for water

infrastructure.

Many poor countries with csimilar to those of richer ones

1/100th as much water infrastruct

means that they are extremely vu

cissitudes of climate variability, a

is exacerbated by climate change.

can and must be done through b

of watersheds and of water dema

This book can help to make

already have sustainable and con

able design of new surface stora

dresses the issue of reservoir sus

economic angle, a perspective tha

limited attention to date.

 We hope that this initial step w

ers to follow, both with additional

actions aimed at conserving wate

future generations.

Vice President, Sustain

FOREWORD

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I N T R O D U C T I O N A N D O B J E C T I V E S

RATIONALE AND SUMMARY

Introduction

The current estimate of total reservoir storage world-

wide is around 7,000 km3 (ICOLD, 1998). This stor-

age is used for water supply, irrigation, power

generation and flood control. Concern about loss of 

reservoir capacity due to sedimentation was raised

by Mahmood (1987) and has recently been expressed

in many forums and publications. It is estimated that

more than 0.5 percent of the total reservoir storage

volume in the world is lost annually as a result of 

sedimentation (White, 2001). This translates into

the need to add some 45 km3  of storage per year

worldwide. Costs would be on the order of 

US$13 billion per year and the associated environ-

mental and social impacts significant. The introduc-

tion of sediment management measures in some older

dams, where appropriate, and in the design of newones could help to reduce this need for additional

storage.

In December 1999 the World Bank initiated the

RESCON (REServoir CONservation) research project

to develop an approach to the assessment and pro-

motion of sustainable management of reservoirs, with

special emphasis on the economic evaluation of sedi-

ment management and the promotion of sustainabledevelopment. This book outlines the results of the

project.

Sediment management alternatives

Sustainable development eco

Literature on sediment manageme

focused mostly on engineering a

Fan, 1998). A review undertak

revealed that there is little, if any

mation on the economics of reser

and its implication for sustainab

framework is needed to assess th

bility of sediment management st

allow the life of dams to be prolo

Such a framework should be ab

related but distinct questions:

· Is the extra cost incurred in

ment management activities w

of extending the productive l

· Is it economical to extend thdefinitely?

Common engineering practice

approach in dam and reservoir des

that over the course of its life, a wa

would recover investment costs

efits generated by the project. T

not take into account what happat the end of its design life and

problems with reservoir sediment

retirement will be addressed by f

The “life cycle management” appr

this book instead aims at design

f f

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T H E R E S C O N A P P R O A C H

for dealing with the resulting problem. This could

be achieved by establishing a retirement fund with

annual contributions made during the life of the damto pay for any actions required at its retirement. These

actions can comprise substantial plant modification

(e.g., protecting the intakes and converting to a run-

of-river scheme), change of purpose (e.g., recreation,

farming, environment creation) and in extreme cases

dam retirement using partial or complete removal

of the dam. Such a fund would best be established

at the start of the project and will require periodic

reviews and adjustments to ensure its adequacy.

Environmental and social safeguards

In too many cases in the past, insufficient attention

has been paid to the environmental and social im-

pacts of large dam projects. This is no longer toler-

able. Environmental and social issues must beaccorded a status equal to, if not higher than, eco-

nomic expediency. Potential environmental and so-

cial impacts and where possible potential

opportunities for enhancement need to be identi-

fied early on in the project life cycle (at pre-feasibil-

ity stage) so that they can be investigated thoroughly

and dealt with appropriately during project devel-

opment. This book advocates the use of the “safe-guards” approach to identify in broad terms the

environmental and social impacts of a project so that

they can be studied further in the next phase of the

project evaluation procedure and mitig

determined.

The RESCON model

A computer model of the RESCON a

developed as a demonstration tool. T

rithm of the model is an economic

function, supported by engineering rela

allow the quantification of basic par

model helps to evaluate at the pre-fe

the technical and economic feasibility o

ing the life cycle management approac

from the economic optimization routin

preferred sediment management techn

tainable use of the water resource i

 Where sustainable use cannot be achiev

computes the annuities required for t

fund.The model is intended for use by

practitioners of reservoir sedimentation

It is released as a “beta version” for f

and improving in the field and as such

edged that it may contain errors. Use

to employ caution and sound engineer

when interpreting the results. Nonet

hands of an experienced practitionshould provide guidance at pre-feasib

project appraisal.

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Background and Motivation

The current estimate of total reservoir storage world-

wide is around 7,000 km3. This storage is used for

water supply, irrigation, power generation and flood

control. Concerns about the loss of reservoir capac-

ity due to sedimentation were raised in a World Bank

publication in 1987 (Mahmood, 1987) and recently

expressed in many forums and publications. Table 1.1

shows the worldwide distribution of storage, power

generation and sedimentation rates.

It is estimated that between 0.5 and 1.0 percent

of global water storage volume is lost annually as a

result of sedimentation (White, 2001). Using an in-

termediate rate, this loss in storage is approximately

45 km3  per year. If it is further assumed that the

average reservoir volume is 150 million m3, then 300

large dams should be built annually just to main-tain current total worldwide storage. Nearly US$13

billion per year would be needed to replace this stor-

age, even without taking into account the environ-

mental and social costs associateHowever, if most existing and stil

reservoirs are managed in a susta

number of new dams required to

water and power supply could b

The “creeping” problem of

several implications. First, the lo

has an opportunity cost in the fo

costs for construction of new sto

level of supply is to be maintain

are direct losses in the form of les

duction capacity available for sale

to produce food and reduced floo

Third, the filled reservoirs, with

for their maintenance, will contin

to their owners and could becom

the fully silted reservoirs will cr

sioning problem that has both dcosts.

Dam retirement or decommi

ing gradually in developed count

1. INTRODUCTION & OBJECTIVES

TABLE 1.1

 WORLDWIDE STORAGE, POWER AND SEDIMENTATION

HydropowerNumber productionof large Storage Total Power in 1995

Region dams (km3) (GW) (TWh/yr) (%

 World wide 45,571 6,325 675 2,643

Europe 5,497 1,083 170 552

N h A i 7 205 1 845 140 658

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T H E R E S C O N A P P R O A C H

lenge for the engineering community. To date, only

small dams have been decommissioned.1  Decom-

missioning of large dams is both full of technical

uncertainties and highly contentious on social

grounds.

In December 1999 the World Bank initiated a

research project to develop an approach to assess-

ment and promotion of sustainable management of 

reservoirs. The specific objectives included devel-

opment of guidelines for evaluating alternative sedi-

ment management options from an engineering

perspective as well as a mathematical model to helppolicy makers rank the technically feasible sediment

management strategies in economic terms. The

project was named RESCON (REServoir

CONservation) and its outcomes are described here.

RESCON Contribution to Policy Making

National level policy makers have a long list of pri-

orities. Management of existing reservoirs, includ-

ing sediment management, very rarely rises close to

the top of the list. Two actions are required to change

this attitude: (i) awareness raising and (ii) develop-

ment of a decision making tool that can be used at

the policy level. The RESCON approach outlined in

this book aims to assist policy makers in makingthese decisions within the framework of promoting

sustainable development and intergenerational eq-

uity.

The RESCON Model

In order to assist policy makers in their decision

making process, an Excel based model has been

developed as part of this work. The model is de-

scribed in detail in Volume II of this book. In sum-

mary, the model evaluates alternative sediment

management options for a given (new or existing)

dam and reports on the economically optimum op-

tion. For non-sustainable options the

culates annual contributions to a ret

and takes this into consideration in th

Book Structure

The book is in a two volume format, of

Volume I. Following the Introductio

outlines the RESCON philosophy, whi

a significant departure from the conven

life approach towards dams. The chathe key ideas underlying this approac

goes on to describe the various alterna

aging sedimentation in reservoirs an

covers the difficult to quantify enviro

social consequences that may be associa

management alternatives. Chapter 5

RESCON approach and mathematica

underlies the associated computer Chapter 6 provides the results of appli

RESCON computer program to data

representative dams. Sensitivity analy

formed on key physical and econom

to test the robustness of the results. T

this chapter is to demonstrate the use

dicate possible limitations of the prog

Chapter 7 reports on results of usingapproach to reservoir sedimentation m

three trial countries. Chapter 8 provide

from the study and recommendation

work. A series of annexes to the book

ther background information.

Volume II describes the computer

tail and includes a CD-Rom with the m

format.

1 A list of 35 cases published by Americ

(1999) and relative to the US show damfrom 1 to 26 m with an average of less th

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IntroductionThe concept of intergenerational equity requires that

natural resources be developed and used in a way

that accounts for the interests of all members of 

society, including future generations. The philoso-

phy behind intergenerational equity is that a subse-

quent generation should not pay (under any terms,

whether they be economic, social, health or envi-

ronmental costs) for the legacies of previous gen-

erations. With regard to infrastructure projects this

means that future generations should not be bur-

dened with the decommissioning of assets built to

benefit their predecessors.

Application of this philosophy to dams requires

a modification of the conventional “design life” ap-

proach. The design life approach assumes a finite

project life and gives superficial attention (if any) towhat will happen to the dam at the end of its life.

This results in substantial environmental, social,

economic and safety considerations being left to

subsequent generations.

An alternative approach is that of “life cycle

management.” The ultimate goal of this approach is

sustainable use, where the major functions of the

dam are maintained, through good management andmaintenance, in perpetuity. Where this is not achiev-

able, decommissioning within a finite period is al-

lowed, provided that this is funded by the

establishment of an accumulating retirement fund.

 With this mechanism in place, all generations ben-

f f h f h d b

The links between these areas are sarrows, thick for dynamic relation

single links. A single static link r

that occurs only once and not con

out the life of a project as is the

links. The impacts generated by

lower external boxes, can generat

in the upper external boxes.

Design Life Approach

The design life approach (Figure

viewed as a linear process of finite

has been decided how long the de

say 50, 75 or 100 years, the proj

signed, constructed, operated and

period of time. Input of societal aconcerns is limited to the initial p

stage (denoted by the thin dash

process occurs once, regardless o

course of the project design life. C

economic evaluation of such pro

count for the cost of decommiss

are borne by future generations.

practice on most, if not all, projeconceived using the design life a

Residual concerns, such as inf

and reservoir sedimentation, are

nal effects in Figure 2.1. Solution

problems can include rehabilita

l d h

2. RESERVOIR LIFE CYCLE MANAGEMENT

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T H E R E S C O N A P P R O A C H

management approach, where such decisions are

formalized during the project’s initial planning stage.

This is demonstrated in Figure 2.1 by the thin dashed

line indicating a static input of societal concerns at

the initiation of a design life type project.

Life Cycle Management Approach

The life cycle management approach is illustrated

in Figure 2.2. The process contains the same ele-

ments as the design life approach but arranged in acircular fashion, indicating perpetual use of the in-

frastructure. Consequently, the opportunity exists

to incorporate changing environmental and societal

concerns, often associated with direct

facility. Operations and maintenance a

in a way that will encourage sustain

continuously evaluated for this purpo

system ages, components are replace

bished as is usual in conventional sy

voir sedimentation management, ho

additional element (not shown in the

operations and maintenance program a

the life cycle management approach. If s

mented, reservoir sedimentation man

serves reservoir capacity and allows of the facility. Figure 2.2 emphasizes

tual decommissioning of the facility,

necessary, is included within the pro

ment objectives.

The adaptation of an existing, or ex

life project to a life cycle managemen

possible. However,

to be significanhurdles to overcom

idea is that the reha

eration, or decom

an existing facility

the focus of a proje

be managed throu

the life cycle metho

able manner. The bea project may, howe

indirect in nature, o

avoidance of a nega

sociated with the p

of the facility.

To overcome an

sign limitations, e

resource infrastruct

refurbished to all

sedimentation man

continued profitabl

this is not possible

reaches the end o

requires decommi

External

SocietalConcerns

External

EnvironmentalConcerns

Climate Change &Observation

Increase Understandingof Complex Interactions

Occurrenceof Extreme Events

Depletion ofNatural Resources

Changing Societal Needs• population changes• resource use changes

Altered Land UseRiverine Impacts

End of Design Life

Static Inputat Project Inception Static Inputat Project Inception

Estuarine Impacts

Fisheries Impacts

Altered Hydrology Issues

Population Dislocation

Unmet Water &Power Needs

Increased Awareness of

Complex Interactions

Regulatory &Policy Change

Changing Societal Values

• Remaining Infrastructure Issues• Unused Physical Resources• Unmet Societal Needs

Project Focus

Design Life Management

Residual Concerns

Planning

ImpactsImpacts

Design

Construction &Implementation

Operation &

Maintenance

FIGURE 2.1

DESIGN LIFE APPROACH

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R E S E R V O I R L I F E C Y C L E M A N A G E M E N T

FIGURE 2.2

LIFE CYCLE MANAGEMENT APPROACH

petual and suimportant des

incorporation

mentation man

If operated an

rectly, such fac

in perpetuity,

intergeneratio

and future gen

the benefits of

spreading the

operations and

many generat

The two ap

ferent abilitie

external conce

cerns are thos

ered outsidepurpose, but

the approval,

cess of larg

projects. In ge

nal issues can

environmenta

as depicted in F

 While the decan introduce

outset, no cap

to incorporate

the course of t

life. The life c

plicitly allow

these issues, as it is understood th

ation is an eventual and intendedtinuing success of the project.

Another critical difference b

life and life cycle management ap

in the economic evaluation of t

using the design life approach, ec

i d d fi i lif

External

SocietalConcerns

External

EnvironmentalConcerns

Climate Change &Observation

Increased Understandingof Complex Interactions

Occurrenceof Extreme Events

Depletion ofNatural Resources

Altered Land UseRiverine Impacts

Estuarine Impacts

Fisheries Impacts

Altered Hydrology Issues

Local Sedimentation Issues

Toxicology

Cumulative Impacts &

Interaction withother Systems

Population Dislocation

Unmet Water &Power Needs

Flood Risk Exposure

Toxicology

Changing SocietalConditions with time

Changing Environmental Conditions with time

• Resolve Infrastructure Issues• Capitalize on Physical Resources• Arrange to meet continuing Societal Needs

Dynamic Input of Social and

Environmental Concerns Throughout

Life Cycle Allows for Project Reevaluation

Project Focus

Life Cycle Management

Decomissioning

Design

ImpactsImpacts

PlanningConstruction &Implementation

Operation &Maintenance

Changing Societal Needs• population changes• resource use changes

Increased Awareness of

Complex Interactions

Regulatory &Policy Change

Changing Societal Values

Comparison of the Two Approaches

Several of the differences between the two approaches

are quite obvious. The design life approach follows

a linear time line and assumes that the project would

have served its purpose at the end of its design life.

Projects previously designed following this approach

did ll f d i i i h d f h

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T H E R E S C O N A P P R O A C H

designed to be either sustainable or non-sustainable

the economic analysis using the principles of life cycle

management should tip the balance i

sustainable solution.

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IntroductionThe importance of reservoir sedimentation manage-

ment is evident when one considers that the cost of 

replacing storage lost annually due to sediment depo-

sition throughout the world is in the order of US$13

billion. If sedimentation can be managed success-

fully, as it has been in some reservoirs, the loss in

reservoir storage space due to this phenomenon can

be lowered significantly. The benefit of effective res-ervoir sedimentation management is therefore clear.

This chapter outlines the state of current knowl-

edge in reservoir sedimentation management. Fur-

ther information can be found in other publications

such as Morris and Fan, 1997; Basson and

Rooseboom, 1997; and White, 2001.

The Sedimentation Process

As sediment enters a reservoir it deposits as the flow

velocity reduces. The coarser portion of the sedi-

ment load deposits in a delta at the upstream end of 

the reservoir and the finer portion deposits in reaches

closer to the dam (Figure 3.1). The sediment profile

can be described by: the topset, the foreset and thebottom set. The topset is the gently inclining por-

tion of the delta at the upstreamvoir. The foreset is the steep slope

delta. The bottom set is the flat p

the delta. The intersection of the

is termed the pivot point. As mo

the reservoir, the bottom set grad

thickness and the foreset moves

In some instances sediments c

ervoir as a density current. This

occur when the sediment coninflowing river is much higher th

impoundment and/or there is a si

ture difference between the inco

impounded water. Under such

density current may flow under th

in the reservoir toward the dam.

rent is not allowed to flow through

of low-level gates, a technique current venting, it will curl up a

return-flow will mix with the cl

reservoir. The sediment thus mix

water will deposit with time.

Most dams have been designe

age capacity below which there

therefore the water in this zone can

designers incorrectly assumed thanaturally deposit in this dead sto

above, this is not the case and a g

the sediments deposited are fo

reaches of the reservoir, thus red

age volume.

d

3. RESERVOIR SEDIMENTATION MANAGEMENT

FIGURE 3.1

THE SEDIMENTATION PROCESS

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T H E R E S C O N A P P R O A C H

Blockage of outlets causing interruption of ben-

efits (e.g., irrigation releases or electricity gen-

eration) and reducing the ability of the dam to

pass floods safely (e.g., by blocking emergency

outlet gates)

Increased loads on the dam.

This book concentrates on the reduction of stor-

age caused by sedimentation. However, the other

consequences listed above should also be taken into

account when assessing reservoir sedimentation

management alternatives.

Available Sediment Management Alternatives

It is possible to successfully manage reservoir sedi-

mentation by using one or more of a host of well

publicized techniques. The techniques can be cat-

egorized as follows:

Reducing sediment inflows

watershed management

upstream check structures

reservoir bypass

off-channel storage

Managing sediments within the reservoir

operating rules tactical dredging

Evacuation of sediments from the reservoir

flushing

sluicing

density current venting

mechanical removal (dredging, dry excava-

tion, hydrosuction)

Replacing lost storage

increased dam height

construction of new dam

Decommissioning

The techniques are outlined in the

following sections

mon. Soil erosion reduces land fertili

treme cases can result in large areas b

ren. Soil erosion is caused by many fact

soil type, sur face gradient, temperatur

rainfall and wind. Natural erosion rate

accelerated dramatically by human ac

poor land management techniques, p

of infrastructure and deforestation. In N

alone the economic damages associa

erosion are estimated to be in excess of

per year (Osterkamp et al, 1998). It is

surprising that a great deal of effort is ebally to control and reduce soil erosion

watershed management techniques. Co

ticed techniques include bunding, te

Figure 3.2), contour plowing and affo

 Where properly undertaken, water

ment has been effective in reducing so

therefore it is seen as an effective wa

reservoir sedimentation rates also. Uresearch and literature (e.g., Mahmo

the subject do not support this belief

Research  (Hufschmidt, 1986) has s

tensive conservation efforts spanning se

may be needed to reduce sediment yie

percent for catchments that exceed 1

thermore, in very large catchments

measures are often, from a reservoir s

EXAMPLE OF GOOD WATERSHED MANAG

CATCHM

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R E S E R V O I R S E D I M E N T AT I O N M A N A G E M E N T

management point of view, considered to be inef-

fective because of the large time lag between imple-

mentation of erosion control measures and realization

of their effect in reducing sediment discharge in riv-

ers. The reason for this is that the sediment delivery

ratio2  of large catchments is low,3  which means that

large volumes of eroded material are stored at vari-

ous locations in the watershed. See Figure 3.3. Eroded

material does not immediately enter streams and riv-

ers, but instead is washed into the streams and riv-

ers over many successive storm events. Therefore,

the effect of erosion protection measures is not im-mediately reflected by a similar change in sediment

yield.

In some catchments, however, where sediment

delivery ratios approach unity (e.g., where the eroded

material is very fine and is quickly transported into

the river systems) watershed management can be

effective in reducing river sediment yields in rela-

tively short time spans. This has been demonstratedin the Loess Plateau Watershed Rehabilitation Project

in China (Voegele, 1997).

From a management point of view it is impor-

tant to quantify the effectiveness of alternative wa-

tershed management measures in order to identify

the economically optimal technique. Furthermore,

the cost effectiveness of watershed management

measures needs to be compared with that of other

measures to reduce reservoir se

This is a complex subject requirin

ies.

The current state of knowledge

port in rivers and in catchment

how the two sets of variables rela

to allow prediction of the impact

ment management techniques on

in rivers. It is recommended that

experts in the field of sediment tr

ment management, who have app

and experience in judging the povariety of catchment managemen

simple solution exists and assess

tial effect of optional catchmen

proaches requires detailed study

under consideration and assessm

available data and local knowled

Good catchment managemen

ber of benefits, including benefitsenvironment, food production,

availability. The concomitant red

yield from catchment that could

catchment management is an add

should be included with the rest

Further information is provid

Upstream check structuresDebris dams are used on mountain

coarse-grained sediments occur.

located on one or more tributaries

ervoir and sediments should be per

Ease of access to remove sedime

dams and the potential to re-us

the application of d

tially feasible. In the

conditions, the life

likely to be short an

limited.

Care needs to be

design and construct

In particular conside

FIGURE 3.3

EXAMPLE OF CATCHMENT SEDIMENT YIELD (INDUS

CATCHMENT, PAKISTAN)

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T H E R E S C O N A P P R O A C H

given to how flood flows will be handled. Often debris

dams are small and are designed to be overtopped

by floods. Attention must also be paid to the design

of the embankment and the downstream energy dis-

sipation measures to prevent failure due to erosion.

Such failure will not only result in the release of the

trapped sediments, thereby negating the benefits of 

the structure, but may also pose a hazard.

Reservoir bypass

The purpose of a bypass is to divert sediment laden

flood flows around a reservoir. By-passing a reser-voir by making use of conveyance structures is of-

ten only feasible when favorable hydrological and

morphological conditions exist. Operating costs of 

the conveyance structures due to the high erosion

rates of the sediments, as well as the benefits lost by

not capturing the flood flows, must be taken into

account.

An example of a successful bypass project isshown in Figure 3.4. Nagle Dam in South Africa is

located in a high sediment yield catchment. Sedi-

ment deposition in the reservoir has been kept to a

minimum throughout its life by use of a bypass. The

dam has been designed to impound water in a long

river meander. At the upstream end of the meander

and reservoir, a set of floodgates has been installed

that are closed when large floods occur. By closingthe gates the flood is diverted past the reservoir,

carrying large volumes of sediment that would oth-

erwise have deposited in the reservoir with it. The

project has been in operation for severa

very little sediment deposition.

Off-channel storage

Off-channel storage reservoirs are bui

the main river channel (e.g., a small tr

the flood plain). Water from the ma

verted into the reservoir during time

ment concentrations. Although this

available for the management of sedim

ing reservoirs, it should be consid

projects.

Managing Sediments within the R

The behavior of sediments within th

sensitive to reservoir water levels. If

level is kept high during the flood seas

sediments will tend to deposit in the uof the reservoir as the incoming flows de

entering the still water. This holds the s

from the dam and importantly the dam

it also means that sedimentation occu

storage, leading to a loss in yield du

reduction in live storage and the resu

to draw down the reservoir to its full

versely, if the reservoir level is drawnvance of the flood season, the incom

erode the previously deposited delta

sediments towards the dam. While thi

FLOOD W EIR

FIGURE 3.4

NAGLE DAM BYPASS, SOUTH AFRICA (FROM BASSON AND ROOSEBOOM, 1997)

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R E S E R V O I R S E D I M E N T AT I O N M A N A G E M E N T

the deposition of sediments in the

dead storage zone of the reservoir,

thus allowing for greater yield from

the live storage, it may pose a haz-

ard to the dam outlets.

From the above, it can be seen

that the selection of reservoir

operating rules can control how

sediment deposition occurs. Math-

ematical models exist to predict this.

In a study undertaken for Tarbela

Dam, Pakistan (WAPDA, 1998) itwas shown that by modifying the

operating rules of the reservoir, the

accumulating sediments could be

held at a safe distance away from

the power house intakes. This

would protect the intakes from the

ingress of sediments and hence pre-

serve the power generating capabili-ties of the project for a further ten

years at no capital cost. Figure 3.5

shows the results of the mathemati-

cal modeling.

As a reservoir fills with sediments there is a dan-

ger that the outlets from the reservoir will become

blocked. This is a particular problem if the reservoir

is used for hydropower production. It is howeveroften possible to protect the dam outlets from be-

coming blocked with sediments using a number of 

techniques. These include: tactical dredging in the

vicinity of the outlets and the construction of physical

barriers to keep the outlets clear.

Tactical dredging is the term

dredging. It is used to keep outlets

and can be an effective means of pr

life of a reservoir which is filling uThe method is currently being us

Ethiopia. The dredged quantities a

pared to the annual sediment bu

reservoir. However, the dredging

low-level outlet and will keep

powerhouse clear. See Figure 3.6

Evacuation of Sediments from

Flushing

Flushing is a techniqu

velocities in a reservo

such an extent that de

1100

1150

1200

1250

1300

1350

1400

1450

1500

1550

0 5 10 15 20

Distance Upstream from Dam (mile

    E    l   e   v   a    t    i   o   n    (    f   e   e    t    )

TARBELA DAM PREDICTED DELTA PROF

OF OPERATION UNDER DIFFEREN

FIGURE 3.6

KOKA DAM – TACTICAL DREDGING NEAR DAM OUTLETS

Source: WAPDA, 1998. “Tarbela Dam Sedimentation Management S

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T H E R E S C O N A P P R O A C H

Two approaches to flushing exist: complete draw-

down flushing and partial draw-down flushing.

Complete draw-down flushing occurs when the res-

ervoir is emptied during the flood season, resulting

in the creation of river-like flow conditions in the

reservoir. Partial draw-down flushing occurs when

the reservoir level is drawn down only partially. In

this case the sediment transport capacity in the res-

ervoir increases, but usually only enough to allow

sediment within the reservoir to be re-located, i.e.,

sediment is moved from upstream locations in the

reservoir basin to locations further downstream andcloser to the dam.

Low-level outlets for flushing operations should

be close to the original river bed level and of suffi-

cient hydraulic capacity to achieve full draw-down.

The intent with flushing operations is to re-create

river-like flow conditions in the reservoir. By doing

so, the sediment that has deposited is re-mobilized

and transported through the low-level gates to theriver reach downstream from the dam. This opera-

tion is usually performed during the flood season.

The low-level gates are closed towards the end of 

the flood season to capture clearer water for use

during the dry season.

Flushing with partial draw-down may be used

to move sediments from the upper reaches of a res-

ervoir to zones closer to the dam. If this is done,

studies should be completed beforehand to ensure

that intake structures and other ancillary facilities

are not impacted. Flushing with partial draw-down

may be used to clear more live storage space and

locate the sediment in a more favorable position for

future complete draw-down flushing.

Further information on flushing is included in

Annex D.

Sluicing

Sluicing is an operational technique by which a sub-

stantial portion of the incoming sediment load is

passed through the reservoir and dam before the

sediment particles can settle thereby reducing the

creased sediment transport capacity of t

ing through the reservoir reduces the v

ment that is deposited. After the floo

pool level in the reservoir is raised to s

clear water.

Effectiveness of sluicing operati

mainly on the availability of excess r

grain size of the sediments and on re

phology. In many cases sluicing and flu

in combination.

Density current ventingAs noted earlier, density currents may

der exceptional conditions, causing m

to be transported towards the dam than

ships for turbulent suspension indica

rents occur because the density of

carrying water flowing into the reserv

than the density of clear water impou

ervoir. The increased density, increasedconcomitant reduction in turbulence

sult in a coherent current with a high s

centration that dives underneath the cl

moves towards the dam.

If it is known that density curren

particular reservoir, installation and

low-level gates in the dam will make

pass the sediment current through th

charge downstream. By passing the de

through the low-level gates sediment th

deposited in the reservoir is released

thus reducing the possibility of stora

sity current venting is an attractive wa

sediment laden flows because, unlike

erations, it does not require the lower

ervoir level.

Mechanical removal

Mechanical removal of deposited se

reservoirs takes place using conventio

techniques, dry excavation and the

removal system (HSRS)

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R E S E R V O I R S E D I M E N T AT I O N M A N A G E M E N T

Sediment dredging is commonly used to reclaim

storage lost to sediment deposits. However, conven-

tional hydraulic dredging is often much more ex-

pensive than the cost of storage replacement and it

is generally not economically viable to remove all

sediment from reservoirs by means of dredging alone.

 With large contracts the cost of dredging can ap-

proach the cost of building a new dam.

Disposal of dredged material can constitute an

environmental problem and suitable mitigating

measures, which can occasionally be quite expen-

sive, have to be found on a case by case basis. If discharged directly downstream from the dam, the

high sediment concentrations generally associated

with dredging can be unacceptable from an envi-

ronmental point of view. However, it may be pos-

sible to reduce the sediment concentration of the

water flowing in the river by releasing clean water

from the reservoir concurrently with the release of 

dredged material. If the material is not depositeddownstream of the dam, then large expanses of land

fill may be required.

Although dredged material can be a liability, it

can be seen as an asset also (USACE, 1985). Uses of 

dredged sediments include:

Habitat development

Agriculture and forestry—to

soils

Construction—e.g., brick ma

Dry excavation

Dry excavation (also known as

the lowering of the reservoir dur

when the reduced river flows c

controlled without interference w

works. The sediment is excavate

for disposal using traditional earment. Excavation and disposal c

as such this technique is generally

small impoundments. Reservoirs

trol may be more amenable to s

ment by trucking, such as has b

Cogswell Dam and Reservoir in C

ment from this reservoir has be

conventional earth moving equipused as engineered landfill in th

the reservoir.

Hydrosuction removal system (

This is a variation of traditional

ference is that the hydraulic hea

dam is used as the energy for d

TABLE 3.1

EXAMPLES OF RESERVOIR DREDGING1

Required dredging rate AchieveCountry Dam to meet inflow rate (t/yr)

Algeria Cheurfas No Data

Sig No Data

Fergang No Data

Hamiz No Data

China Xuanwei 280,000

Shuichaozi 1,900,000

Tianjiawan 350,000

Japan Akiba 560,000

Sakula 4 260 000

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T H E R E S C O N A P P R O A C H

pumps powered by electricity or diesel. As such,

where there is sufficient head available, the operat-

ing costs are substantially lower than those of tradi-

tional dredging. Roveri (1984) promotes applicationof the hydrosuction removal system (HSRS) that uses

the hydrostatic head at the dam to provide energy

for sediment removal. The system consists of a barge

that controls the flow in the suction and discharge

pipe and can be used to move the suction end of the

pipe around. The upstream end of the pipe is lo-

cated at the sediment level in the reservoir and its

downstream end is usually draped over the dam todischarge sediment and water to the downstream

river. The arrangement of the pipe layout essentially

creates a siphon and the suction at the upstream end

of the siphon is used to evacuate sediment. The sys-

tem can be used in relatively short reservoirs, not

longer than approximately 3 km and also depends

on the elevation of the dam and reservoir.

Replacing lost storage

Lost storage can be replaced by the construction of 

a new dam (upstream, downstream or on another

river), or the raising of the existing dam. These op-

tions require careful engineering considerations that

are beyond the scope of this book. .

Decommissioning

Reservoirs can generally be expected to experience

serious operational constraints by the time half of 

their original capacity is lost. When dam decommis-

sioning becomes a potential alternative, because of 

advanced reservoir sedimentation, it is very often asign of overdue decision on sedimentation manage-

ment

Dam decommissioning should be regarded as the

last possible option. Although several dams have been

decommissioned in developed countries most of

There are other options available a

commissioning silted reservoirs. Thes

In many situations it may be techninomically feasible to continue to o

power plants as run-of-river station

increased operational and mainten

Maintaining the dam (perhaps at

and using the now silted reservoi

enhancement, e.g., creation of wet

for farming; or recreation.

Each site will have specific oppo

beneficial use. It is recommended tha

plored before opting for decommissio

Application of RESCON

The preceding sections have provided methods that can be used to manage

reservoirs. These management techniq

wide range of activities, from attempts

source of the problem, i.e., sedimen

managing sediment flow and depositi

ervoir, to removing deposited sediment

management approaches prove ineffe

ervoir volume can be increased by rai

finally, the dam and reservoir can be dec

if the sedimentation problem becomes

it renders them useless.

The RESCON software develope

course of this project can be used to as

nical and economic feasibility of applyi

niques. The software focuses on remova

sediment and is capable of assessing th

of flushing, dry excavation (truckinHSRS and decommissioning. Routin

such as bypassing and pass-through s

not represented in the software, nor

management.

Recommendations on watershed ma

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Consequences of implementing sediment man-agement on the downstream environment

Dams have serious environmental and social impacts

which require mitigation actions. Some of the more

important aspects are outlined in Annex E. Dam

decommissioning and the implementation of sedi-

ment management techniques outlined in Chapter 3

also have impacts that need to be taken into consid-

eration. This book does not purport to detail these,but merely to draw the reader’s attention to some of 

the key aspects.

Dam decommissioning and many of the sediment

management techniques that involve the release of 

reservoir sediments downstream need to be appraised

within the framework of environmental and social

impacts. Downstream impacts may include:

Geomorphological changes to the downstream

river channel

Increases in turbidity

Changes in flooding frequency and patterns

Reduction of dissolved oxygen in the river

Poisoning of the ecosystem especially where toxic

sediments are released.

All of the above will have an impact on the natu-

ral environment as well as on human activity.

Sediment management can both mediate and

exacerbate some of the negative effects caused by

dams. Some sediment management alternatives in-

l d d h b

native fish fauna, while sediment

ing would maintain the status q

rary reduction in ecosystem service

of fine sediments into the stream

dam during the cleanout operation

further downstream in the San

tem, sediments had been manage

result of the sluicing (and dam m

dures governing water release) th

erine habitats have been destroysupport the native aquatic fauna.

in this case that the cost of the en

gation required as a condition o

ing was lower, at least in the

alternative sediment managemen

A study undertaken by Zhou an

cites numerous occasions where i

eration of the ecological effects ofresulted in serious impacts dow

depend on whether sediments ar

river flow or are deposited in the r

sediments may fill pools and in

production, as well as kill adult

other aquatic wildlife by cloggin

suffocation. Some species may b

even small increases in turbidRasmussen, 1995 noted that occ

increases in river turbidity (e.g.,

lease of sediments from a dam) m

75 percent of some fish species.

Damages to the downstream e

h d

4. ENVIRONMENTAL AND SOCIAL SAFEGUARDS

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T H E R E S C O N A P P R O A C H

care needs to be exercised. Large increases in flows

and sediment concentrations in addition to damag-

ing the ecosystem may result in large scale geomor-

phological changes to the river regime. Such changesmay include changes to meander patterns, scouring

or infilling of river beds, deposition of sediments at

manmade intakes, undermining of flood defense

works and blockage of bridges or culverts. Such ef-

fects in addition to having far ranging social and

economic impacts may have safety implications also.

If sediment removal measures are employed from

the start of a project, the impacts are likely to be lessthan if measures are introduced late in the project’s

life. If no removal is practiced and the dam is ulti-

mately decommissioned, impacts may be severe. An

example of this was observed when the Fort Edwards

dam was removed in New York. The process released

over 400 000 m3 of sediment and resulted in partial

blockage of the east channel of the Hudson River as

well as increased risk of flooding of the town of FortEdward. See Zhou and Donnelly, 2002.

Any method of sediment management that re-

sults in the return to a more natural hydrograph or

incorporates an environmental flow requirement will

probably yield positive environmental results or at

least a mix of positive and negative impacts. Use of 

release flows for environmental reasons or sediment

management may result in a short-term reduction

in financial returns from the project, but will likely

lead to increased sustainability and a re-distribution

of the benefits of the dam.

Large reservoirs sited closely upstream of estu-

aries and deltas have in some cases caused wide-

spread environmental, social and economic impacts

by reducing the flow of sediments. The release of 

sediments from such a reservoir due to the imple-

mentation of sediment management may have posi-tive impacts on the estuary or delta downstream.

Creative sediment management options such as

watershed management directed to the upper reaches

of the watershed may have direct environmental

benefits Recent studies on headwater streams

The degree to which sediment man

yield positive environmental impact

function of its ability to mitigate som

tive effects of the storage project. Comment management with environme

restore downstream ecosystem service

greatest positive result. Environmen

enhance fisheries, support flood rece

ture, stabilize riparian vegetatio

biodiversity, etc. Other approaches su

ing or preserving portions of the wa

duce sediment yield can also henvironmental effects.

A Safeguard Approach

In previous decades, relatively little im

attached to the environmental and soc

development projects. Today much grsis is placed on such considerations.

ingly, sediment management plans for

now expected to include environmen

impact analyses.

A complete impact analysis is rar

at the pre-feasibility level due to lack o

information. The intention of the RESC

on the other hand, is to identify, alrea

sibility level, the reservoir sedimenta

ment techniques that will maximi

benefits without conflicting with tech

ity requirements and environmental/

ability. When conducting inves

pre-feasibility level, it is usually nec

ploy approximate evaluation techniqu

answers as a basis for detailed further

Unfortunately, such preliminary methbeen fully developed for assessment of

ronments. In other words, despite scien

in environmental science, no generi

relationships exist between changes in s

and environmental quality that can be

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E N V I R O N M E N TA L A N D S O C I A L S A F E G U A R D S

TABLE 4.1

SAFEGUARD RATINGS

Safeguard Value Descriptor Discussion of Assignment Criteria

Natural Habitats 1 Potential Enhancement Potential enhancement of natural ecosystems d

of sediments, restoration of overbank flows, do

movement of nutrient, etc.

2 Minor Impact Either minor permanent impacts to natural func

ecosystems, or temporary impacts.

3 Moderate Impact Permanent impacts to natural ecosystems, una

significant conversion or degradation of natura

4 Significant Impact Significant conversion or degradation of critica

Human Uses 1 Potential enhancement Benefits to floodplain agriculture/grazing, down

coastal fisheries, preservation of beaches, etc.

2 Minor Impact Minor or temporary impacts to floodplain agric

downstream fisheries, etc.

3 Moderate Impact Permanent impacts to downstream fisheries, lo

agriculture/grazing, short term impacts to potab

4 Significant Impact Significant loss of agricultural or f isheries poteimpacts to potable water, etc.

Resettlement 1 No Resettlement No resettlement necessary.

2 Minor Resettlement Limited population impact, and impacted popul

suffer loss of income or assets.

3 Moderate Resettlement Significant numbers of individuals displaced, no

but some potential for loss of income, assets, or

4 Significant Resettlement Displaced population is likely to suffer loss of a

and/or means of livelihood. Resistance to rese

cultural/social displacement as a result of reset

Cultural Assets 1 None Affected No cultural assets affected by project (assets w

paleontological, historical, religious, or uniq

including remains left by previous human inhab

2 Minor Impact Cultural assets can be protected, salvaged, or t

without significant loss of cultural value.

3 Moderate Impact Minor to moderate loss of cultural assets, or sig

diminution of cultural value due to salvage.

4 Significant Impact Significant loss of cultural assets, or devaluatio

 to translocation.

Indigenous 1 No Impact Indigenous peoples may derive direct, socially

Peoples appropriate benefit from the project or indigen

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T H E R E S C O N A P P R O A C H

logical processes with biota dynamics over varied

spatial and temporal scales.” Ecology as a scienceappeared at the end of the nineteenth century and

was devoted initially to the description of the struc-

ture of ecosystems, leading to the first observations

and descriptions of succession, predator/prey

relationships and other phenomena that drive the

dynamics of the ecosystem. However, the science

lacked the predictive capability to manage aquatic

systems.As a result, two extremes have appeared in lit-

erature: over-engineered management of aquatic

environments on the one hand and restrictive envi-

ronmental conservation, with the general assump-

tion that the aquatic environment should be

maintained in its pristine condition, on the other.

The former approach sometimes results in unsatis-

factory management of the environment and the latter

is unrealistic. The integration of ecology and hydrol-

ogy promises to accelerate the process of moving

ecology and environmental sciences from a descrip-

tive stage to an analytical, functional, operational

stage. Once this has been accomplished, the chances

f f ll i i

sive environmental assessments as n

procedure detailed below may be usemaking at the pre-feasibility level. Th

emerge should be reviewed in detail

quent feasibility studies, prior to imple

the optimal management approach.

Application of Safeguard Policies

Outlined in Table 4.1 are the releva

policies of the World Bank,5 as they w

a generic reservoir conservation prog

the concerns mentioned in the first

values ranging from one (1) to four (4

the value of one (1) is assigned to no

possible benefits and the value four (

to the worst condition. The safeguard

when a RESCON investigation is exec

ues (1 to 4) are assigned to each conc

score is determined by adding the safe

Decisions pertaining to the potential e

and social feasibility of the project are

d i i T bl 4 2

TABLE 4.1

SAFEGUARD RATINGS (continued)

Safeguard Value Descriptor Discussion of Assignment Criteria

Trans-boundary 1 No Issues Project will not affect any river, lake, or body of wate

Impacts a boundary or flows between two states. All states w

beneficiaries of the project.

2 Minor Impacts The project may have minor or transient impacts to o

impact aspects of a state other than the beneficiary s

3 Moderate Impacts The project may have moderate and/or permanent im

one or more impact aspects of a state other than the

state.

4 Signif icant Impacts The project will l ikely have significant impacts to one

of the impact aspects of a state other than the benefi

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E N V I R O N M E N TA L A N D S O C I A L S A F E G U A R D S

also reports the highest ranked management alter-

native that meets the safeguards standard of accept-

ability. This standard is specified by the user and is

based on the final score in Table 4.2.

Conclusions

In addition to technical and economic feasibility,

environmental and social impacts of sediment man-

agement play pivotal roles in determining project

selection. Studies of such impacts could use a nor-

mative approach, in which the monetary conse-

quences of implementing different levels of safeguard

compliance are compared with o

economically and technically o

rejected because it does not meet t

dard, the RESCON program resulno safeguards imposed are used

nancial opportunity cost of impl

guard approach. This cost is the d

the NPVs of the environmentally

strained and unconstrained alter

In order to implement a no

cause-effect relationships for the s

be needed and typically these areable. The insights provided by th

method described in this chapte

of the terms of reference of feasi

required for moving the process

 When selecting options for

ment, emphasis should be placed

mitigating against the environm

impacts a particular option may hing this into the decision making

as discussed above, some alterna

sediments have positive impacts

ones and these need to receive a

thermore, when outlining the op

nity exists for identifying environ

enhancement measures which if

included in the option.

TABLE 4.2

INTERPRETATION OF SUM OF SAFEGUARD RATINGS

Sum of Ratings Interpretation

6 No impact and potential benefit

6 to 12, with no 3’s Minor impact

12 to 15 or

at least one 3 Moderate impact

16 or higher, or

at least one 4 Significant impact

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The Need for RESCON

A decision as to whether sustainable management

of dams and reservoirs should be implemented on a

national or regional scale as a matter of policy is

subject to considerable uncertainty. Engineering

methods are available to analyze a specific project

in detail, but the detail is proportional to the quan-

tity and quality of the data used. Obtaining all the

necessary data, choosing the appropriate ana-lytical tools and making a decision requires signifi-

cant amounts of time and resources. For this rea-

son, in most situations it is impractical to execute

feasibility studies on large dam and reservoir sys-

tems to determine the potential for success of such

a policy.

To fill this gap, a tool is needed that can provide

reasonably reliable information to decision makersas to whether sustainable management of dams and

reservoirs in an existing water resource system is an

achievable goal. The RESCON project aims to do so

by providing a tool kit that can be used for decision

making purposes at the policy level. The technique

is designed to use dam and reservoir data that are

readily available. Should such data not be available

the approach directs users’ attention to the acquisi-

tion of critical data. The RESCON approach also

promotes policy makers’ awareness of the importance

of reservoir conservation at the national level.

P li i A t f

the dams for RESCON analysis a

on the output of the model.

There are four parts to the fig

Watershed management potenti

the RESCON model does not h

tine for assessing watershed ma

Figure 5.1 can be used as pre

as to whether further watersstudies should be undertaken.

agement is a potential option

model can be “tricked” into

reducing the annual average

an appropriate amount.

Environmental and social co

RESCON model has a routine

The notes given in the Figuresome of the more important c

Potential for mechanical remo

model has a routine for asses

cal options. From the figure th

ascertain whether these optio

technically feasible or not.

hydrosuction option shows t

is unlikely to be effective in co

tation if the annual inflow of s

than 100,000 m3 per year or

much more than 3km long.

Reservoir operation diagram. T

work done by Basson and R

h d d

5. RESCON APPROACH AND PROGRAM

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T H E R E S C O N A P P R O A C H

oritizing actions fo

reservoir manageme

ing the groundwor

terms of reference tailed feasibility stu

The RESCON ap

reservoir owners a

to prioritize mana

sions at the policy lev

and justify budgets f

tation of sediment

strategies or to justion of new storage

ate. The typical

RESCON approach

lined as follows.

Current sedimen

These allow the

cast the evolutiomentation proc

reservoirs exam

ated impacts at so

mental and econo

also be assessed

can be made of s

rates among ind

and identificatio

ervoirs in which

is causing the h

economic impac

Basis for manag

sedimentation. R

mentation man

compasses in

together with m

well as structurstructural measu

ter 3).

Basis for prioriti

management m

actions required

PRELIMINARY ASSESSMENT OF RESERVOIR SEDIMENTATIONMANAGEMENT OPTIONS

CHECK POTENTIAL FOR M ECHANICAL REM OVAL TECHNIQUES:

Flushing / Sluicing / Storage Options

0.1

1

10

100

1000

10000

100000

0.001 0.01 0.1 1 10

Storage Capacity/ M ean Annual River Run-Off

    S    t   o   r   a   g   e   c   a   p   a   c    i    t   y    /    A   n   n   u   a    l    S   e    d    i   m   e

   n    t    L   o   a    d

Storage normally notfeasible in this area

Storage

Most existing reservoir

fall below this line

Sluicing

Flushing

ENVIRONM ENTAL AND SOCIAL CONSIDERATIONS:

CHECK W ATERSHED MANAGEMENT POTENTIAL:

If catchment area <100 km2 and soils are fine grained there is good potential for effectivewatershed management.

Dredging

Hydro Suction

Trucking

0.1 1

Sediment Yield (Mm3 /year)

10

CHECK RESERVOIR OPERATION TYPE:

Check sediment contamination

Check river use by downstream communitiesAssess possibility of sustaining/improving d/s habitatsAssess possibility of releasing sediments during high river flowsAssess sediment re-use

pipeline length <3km

check disposal area s/reuse potential

reservoir empied @ 1-5 yr intervals

FIGURE 5.1

PRELIMINARY ASSESSMENT OF OPTIONS

R E S C O N A P P R O A C H A N D P R O G R A M

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R E S C O N A P P R O A C H A N D P R O G R A M

Investigations needed to better understand res-

ervoir sedimentation trends, or to support de-

sign work, should also be prioritized.

Reservoir Conservation Action Plan. The scope

and format of the outcomes should be adapted

to meet the needs of the reservoir owner and

other stakeholders. The decision making entity

should be provided with a clear, concise picture

of the current storage loss trends and of the

improvements that the proposed action plan

can introduce. A schematic view

of a generic reservoir conserva-

tion action plan is shown in

Figure 5.3.

The action plan, which is based

primarily on available information,

should be seen as a “living docu-

ment” that is periodically updated

The RESCON mmodel

OverviewSeveral models h

for the engineer

ment manageme

of them are suita

outside the spe

which they were

cases the detailed

quired for such munsuitable for us

sessment level. T

plied instead at

detailed design s

In some cases, s

been employed f

sis of sedimentat

ervoirs and to forof the phenome

existing models

economic parameters.

The following list of mathemat

in part on Morris and Fan (1998

GSTARS, Molinas and Yang (

FLUVIAL, Chang (1988)

HEC-6, U.S. Army (1991)

FIGURE 5.2

THE RESCON TOOLKIT

GUIDELINES(Vol. I)

Life Cycle Management Approach

Sedimentation Management Techniques

Environmental and Social SafeguardsInter Generational Equity

Economic Optimisation

Case Studies

MATHEMATICAL

MODEL(Vol. II)

Economic and Engineering

Excel based model using readily available datato determine technical feasibility

and perform economic optimisation

Guidance on Inputs

OUTPUT

Compare and prioritise options at pre-feasibility level

Key element for preparing terms of reference & follow-on actions

1009080706050

5 10 15 20 25 30 35

o   r   a   g   e    l   o   s   s    (    %    )

Past loss rateSediment Managem

RESERVOIR CONSERVATION ACTION PLAN tyTime (years)

SCHEMATIC RESERV

MANAG

T H E R E S C O N A P P R O A C H

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T H E R E S C O N A P P R O A C H

SSIIM, Olsen, et al. (1994)

MIKE 11-RFM, Basson and Rooseboom (1997)

RESSASS, HR Wallingford (2001).

The RESCON model aims to provide a tool to be

used at the planning stage when data are scarce and

strategic decisions need to be made.

The overall aim of the RESCON model is to se-

lect a sediment management strategy that is techni-

cally feasible and also maximizes net economic

benefits. The model is built on the Microsoft Excel

platform. The model explicitly considers the follow-ing sediment removal techniques: (1) Flushing; (2)

Hydrosuction; (3) Traditional Dredging; and (4)

Trucking. In addition, the “do-nothing” alternative,

(i.e., no sediment removal) where eventual decom-

missioning will be required, is also analyzed. The

program may be used for existing dams as well as

proposed dams.

Economic optimization is performed for each of the sediment removal techniques in separate sub-

programs and the net present value (NPV) is reported.

The objective is to maximize net returns from prac-

ticing each technique. Reservoir yield, which is based

on remaining reservoir capacity and the unit value

of this yield are key determinants

of annual revenue. The unit value

of reservoir yield, or water price,

depends on water use (e.g., irri-

gation, domestic, industrial, en-

ergy, etc.) as well as political

factors. Annex F presents a range

of observed water prices from vari-

ous countries and sectors. Costs

include annual operations and

maintenance and any periodic

sediment removal expenses. Rev-enues and costs that accrue over

time are discounted prior to ag-

gregation. The program also allows

initial construction costs (for pro-

posed dams) to be included in the

of the dam is terminated within a finite

(1) is called “sustainable” while case

“non-sustainable.” The non-sustainab

self involves two possibilities: 2(a) thcommissioned at an optimally determi

2(b) the dam structure is maintained

river” project even after the reservoir

2(a) allows a salvage value to be co

terminal time. This value would norm

tive if, for example, decommissionin

Another point to note is that the opt

time (and terminal capacity) in this pend on the magnitude of the salvag

program calculates an annual replacem

ment which, if invested, will earn inte

mulate to equal the costs of decommis

optimal terminal time.

RESCON Model Structure

This section provides general informmathematical model. Further inform

detailed use of the model is presented

TECHNICALFEASIBILITYASESSMENT

TECHNICALFEASIBILITYASESSMENT

FLUSHING

PASS PASS

TOTALREMOVAL

PARTIALREMOVAL

USER INPUT:(A) TECHNICAL & ECONOMIC DATA

(B) ENVIRONMENTAL & SOCIAL SAFEGUARD RATINGS AND POLICY

HYDROSUCTION

RUN OF RIVER

TRADITIONALDREDGING

TRUCKING

ASSUMEDTECHNICALLY

FEASIBLE

ASSUMEDTECHNICALLY

FEASIBLE

RUN OF DAM

PROGR

R E S C O N A P P R O A C H A N D P R O G R A M

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R E S C O N A P P R O A C H A N D P R O G R A M

 

Maximize NB d C V dtt

Tt T

=∑   ⋅ − + ⋅

0

2

Figure 5.4 illustrates the main steps in RESCON

which are described below.

Project-specific technical and economic data areentered by the user

The user is also prompted for environmental and

social safeguards (see Chapter 4)

The model assumes dredging and trucking are

always technically feasible6 and tests the techni-

cal feasibility of flushing and hydrosuction.

For the baseline case of no sediment removal the

model assumes two alternatives: run-of-river andeventual decommissioning.

All options are taken through an optimization

routine to find economically optimum values for

each.

The results of economic optimization are com-

pared and ranked.

Economic Optimization Routines

7

The general economic optimization problem is to

choose a sediment removal option and the manner

in which it is to be used (i.e., schedule and amount

of sediment removed) so as to maximize the life-

time aggregate NPV of the project. The life of the

dam is also determined optimally and could be fi-

nite or infinite. The various sediment management

options are assumed to be mutually exclusive. The

problem is solved in two steps.

Step 1

The following optimization is performed for

each sediment management option:

subject to St+1 = S t – M + Xt, (1)

given initial reservoir capacity, S0 and other

physical and technical constraints.

The symbols used in the above formulation

are defined as:

M = trapped annual inc

Xt = sediment removed i

NBt stands for annual net bis defined as annual revenue fr

the dam minus costs of opera

nance and costs of any sedim

occurs during that year. Ann

product of the unit value of

reservoir yield, Wt (which is b

reservoir capacity St). The latt

Gould’s Gamma function as folland Mein, 1978).

where:

Vin = incoming flow volumsd = standard deviation of in

nual runoff),

Zpr = standard normal var

Gd = adjustment factor to

Gamma distribution (of

mal distribution).

The use of Gould’s Gamm

instrumental in the developmemodel. However, the user sho

for Wt/Vin < 0.2 the function

able results. For 0.2<Wt/Vin<

vised to exercise caution.

The above maximization

solved using optimal control th

Sydsaeter, 1987). The standar

select a time path of the contmaximize a Hamiltonian func

ing a co-state equation, appr

conditions and all other const

the statement of the problem. T

tonian function is:

 

 W  S V Zpr sd

S  Gd

Vs

tt in

t

in

=  ⋅ ⋅ − ⋅ +

⋅ + ⋅  

4

4

2 2

T H E R E S C O N A P P R O A C H

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T H E R E S C O N A P P R O A C H

Ht = (NB

t)(d) t + q

t(– M + X

t) (3)

where qt is the co-state variable associated with

St and has a shadow price interpretation (i.e., itmeasures the discounted value of a marginal in-

crease in remaining storage capacity). It is pos-

sible to interpret Ht as a discounted net benefit

function that accounts for the value of reduced

reservoir capacity in the future due to current

choice of Xt.

Maximization of Ht with respect to X

t requires

more information about the relationship betweenannual net benefits, NB

t and X

t. For the sediment

removal techniques under consideration, we as-

sume that cost functions are linear in Xtbut sub-

 ject to technical constraints on removal. Under

this assumption, the Hamiltonian function is lin-

ear in Xt. The consequence is that, depending on

the technique used and the nature of physical

constraints, the solution may involve annual re-

moval (partial or complete) of incoming sediment

or there may be cyclical patterns of sediment ac-

cumulation and removal. Furthermore, technical

or economic optimization considerations may

sometimes necessitate an initial phase that involves

declining storage capacity, followed by annual

removal or a cyclical but stable pattern of accu-

mulation and removal. A detailed discussion of 

the solution for each individual technique is avail-able in Volume II.

Aside from maximization of Ht and satisfac-

tion of all the aforementioned constraints (includ-

ing equations (1) and (2)), optimization also

requires the co-state equation stated below to hold:

qt+1

 – qt = – ∂H

t / ∂S

t(4)

Solutions in which at least a minimally accept-

able storage capacity is maintained forever are

termed sustainable.9  Non-sustainable solutions, on

the other hand, involve an end to storage related

services in finite time If the dam is to be decom-

reduce it. There may also be situat

decommissioning can be avoided by

dam as a “run-of-river” project ev

plete siltation. The NPV of a damscenarios is calculated by assuming

related benefits end when the dam

pure “run-of-river” benefits contin

indefinitely.

Step 2

After the optimization proce

above has been carried out fnique, the next step is to c

NPVs and that of the “no re

egy. The latter strategy invol

= 0 for all t, but the terminal

mined optimally for the scen

decommissioning occurs. A

“run-of-river” scenarios are

in the comparison. The high

ternative is then highlighted

If flushing, dredging or t

niques are adopted, the outc

sustainable. Under HSRS, ho

tainable outcome occurs only

all annual incoming sediment

feasible. The “no sediment re

egy obviously leads to a non-s

lution. Detailed explanations apaths of sediment accumul

moval for each technique are

Volume II.

Intergenerational Equity and Retir

If the optimal strategy turns out to expensive dam modification is requ

salvage value, V, is negative), future

would end up paying this cost without

of the services of the dam. Such inte

R E S C O N A P P R O A C H A N D P R O G R A M

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equity or fairness concerns may be addressed by

setting aside some of the annual net benefits (NB)

as a retirement fund for use at time T. While it is

possible to construct sophisticated contributionschemes that reflect the declining services from an

aging dam, RESCON proposes a less perfect but easy

to calculate plan. Under this plan, a constant amount,

k, is invested in each period so that the accumu-

lated proceeds from the investment at time T are

equal to – V. With optimal T calculated using equa-

tion (5) and letting m stand for the interest rate at

which the retirement fund is invested, the desiredvalue of k is given by:

k = – mV/((1+r)T – 1) (6)

Observe that the interest rate m is allowed to differ

from the discount rate r. Also, if V is not known

initially with certainty, it may be necessary to adjust

the amount k (up or down) as more is learnt about

the true value of V. Any other unforeseen changes in

parameters that impact optimal T and/or HT may also

call for appropriate modification in k. The general

procedure for making this modification would be as

follows. First, optimal T is re-calculated for the re-

maining storage capacity and new parameter values.

The new value of k is then determined using equa-

tion (6), but with a revised “net” V that has been

adjusted for any exogenous cha

existing retirement fund savings

est) which will be accumulated b

T. Of course, continued contribument fund would be needed only

propriately adjusted “net” V is n

Cautionary Remarks

The RESCON model has been re

use by experienced practitioners management. The following shou

ers:

The model always assumes dr

ing are technically feasible and a

these two options through to th

sis. Clearly if the annual inflow o

large, it is unlikely to be practical

the required quantities. The use

note the annual volumes of sedim

removed and make an assessmen

are realistic or not. (See Table 3.

Even where two or more optio

aggregate NPVs, RESCON will p

as the economically optimal solu

also outputs the detailed results

the user is advised to check thes

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Introduction

The RESCON computer program has been applied

to several case studies for purposes of validation and

sensitivity analyses. These case studies represent res-

ervoirs that have either been subjected to reservoir

sedimentation management with flushing or at least

have been extensively studied for such management.

RESCON predictions and results have been compared

to field data and research findings. Sensitivity analyseshave examined the response of the RESCON pro-

gram to changes in input parameters. The objective

was to determine whether the results are logical and

consistent with worldwide experience.

The RESCON program has been applied to the

following reservoirs: Tarbela, Pakistan; Sefid-Rud,

Iran; Ichari, India; Gebidem, Switzerland; Baira,

India; Unazuki, Japan; and Sakuma, Japan. Detailsof the dams and the results of the RESCON applica-

tions are detailed below.

Description of Dams

Tarbela Dam, Pakistan

Tarbela dam was substantially completed in 1973.

The dam provides almost 50 percent of the nations

regulated irrigation water and over 30 percent of its

electricity. The pre-impoundment capacity of the

reservoir was 14,300 Mcm (million cubic meters).

The mean annual runoff (MAR) at the site is

h l l d f d d

The Tarbela Dam Sediment M

(WAPDA, 1998) commissioned bdetailed reservoir sediment mode

ture sedimentation of the reservo

sibility of undertaking different ma

The study recommended the im

three phase action plan.

Phase I: Modify reservoir opera

down the advance of tPhase II: Construct protection m

outlets.

Phase III: Construct new large

 m3 /s) low-level outlets

voir annually.

The study predicted that the

operation of the flushing devicesustainable solution to the sedim

at Tarbela and maintain approxi

of the original storage for many

recommended action plan was sho

cally attractive with an internal

return (EIRR) of 20 percent.

Gebidem Dam, Switzerland

Gebidem is a hydrologically sma

capacity/inflow ratio of 2.1 percen

are high due to glacial activity, w

to 100mm and the potential to r

storage by more than 4 percent pe

d h

6. EVALUATION OF RESCON MODEL

T H E R E S C O N A P P R O A C H

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Baira Dam, India

Baira reservoir is hydrologically very small with a

capacity on the order of 0.1 percent of the mean

annual runoff from the catchment. In the first 18months of operation, almost 20 percent of the origi-

nal capacity was lost due to sediment deposition,

representing a sediment load at least double the

average annual sediment load assumed during the

design. The diversion tunnel originally used during

the construction period was fitted with gates to fa-

cilitate flushing and model studies suggested that

this modification would be capable of removing vir-tually all the deposited sediment. The first flushing

operation was successful, removing over 80 percent

of the deposited sediment in 40 hours and it appears

that annual flushing should be effective in maintain-

ing a large proportion of the original storage capac-

ity, approximately 85 percent.

Ichari Dam, India

Ichari Dam is hydrologically very small, with a ca-

pacity of only 0.2 percent of the mean annual in-

flow. The highly variable annual sediment load has

the potential to replace about 20 percent of the origi-

nal storage per year. This was borne out in the first

year of operation, when the storage capacity was

reduced by 23 percent, increasing to a total storage

loss of 60 percent after six years. The sediment sizes

range from fines up to cobbles and has severely dam-aged the spillway roller bucket.

Although the dam includes facilities for exclud-

ing coarse sediment at the hydropower intake, there

is no low-level outlet for flushing sediment from the

storage impoundment. Flushing via the gated spill-

way has been undertaken annually since 1976 and

an approximate equilibrium has been maintained

since about 1980. Long-term active storage is likelyto average about 35 percent of the original.

Unazuki Dam, Japan

The multipurpose Unazuki dam was completed

in June 2000 on the Kurobe River which has high

Sakuma Dam, Japan

The Sakuma Dam, a hydroelectric faci

pleted in June 1956 on the high sedim

basin of the Tenryu River. The reservlogically small, the original capacity b

percent of the inflow. The sedimen

around 1.6 Mt per year and the mean

is approximately 5,000 Mcm. The dam

flushing outlets. About 35 percent o

capacity of the reservoir storage was

mentation by 2000. A combination of flu

ing and hydraulic suction techniqueemployed to manage sediment at Sak

Sefid-Rud Dam, Iran

This reservoir is hydrologically larger

ers cited above, with a capacity/inflo

percent. Sedimentation was a serious

the first seventeen years of operation

storage capacity at a mean annual ra

cent with a total storage loss of 63 per

1983. Flushing measures have been

since then to remove deposited sedim

reservoir by first emptying the reservo

ber to February to create river-like flo

and then refilling it in time for the star

in May.

Lateral erosion, piping and the use

dinal diversion channel have aided inmaintenance of storage capacity. It is an

by creating a new diversion channel eac

term storage capacity of 90 percent mig

compared with 75 percent by flushin

Long-term Capacity

The long-term capacity (LTC) of a re

achievable with flushing can be expres

sionless terms by making use of the L

pacity Ratio (LTCR), which is de

long-term sustainable storage capacity

E VA L U A T I O N O F R E S C O N M O D E L

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TABLE 6.1

COMPARISON FOR LTCR

Prototype RESCONReservoir Data Estimate

Tarbela, Pakistan 50%a 36%

Gebidem, Switzerland 99% 39%Baira, India 85% 50%

Sefid-Rud, Iran 75% 8%

Ichari, India 35% 44%

Unazuki, Japan Unknownb 41%

Sakuma, Japan Unknown 72%

evacuate sediments from the reservoir. Tarbela has

by far the most comprehensive data set in terms of 

hydrology, hydraulics, sediment inputs and sediment

deposition. Unazuki and Sakuma Dams in Japan havebeen flushed to varying extents, but no LTCR val-

ues were reported to the RESCON team.

The LTCR values calculated with the RESCON

software were compared to the estimates based on

the field trials and, in the case of Tarbela, the results

of the detailed modeling. The comparison of calcu-

lated and observed LTCRs is presented in Table 6.1.

a results of detailed hydraulic modeling using RESSASS software

b reported to be less than 40 percent

In general, the RESCON model appears to un-

derestimate LTCR and therefore provides a conser-

vative estimate for planning purposes. This is

probably partially due to the fact that RESCON pro-

vides the economically optimum solution which does

not necessarily coincide with the maximum storage,

whereas the prototypes presumably attempt to maxi-mize storage.

The RESCON estimate of LTCR for Gebidem is

significantly lower than the field value. This could

be attributed to more frequent flushing operations

at higher discharges than what is reported in the lit-

mate of 75 percent for the actual L

probably be investigated in more

Ranking of Sediment Managem

The sediment management techn

the RESCON model for technical

sibility include:

Sediment flushing

Hydrosuction sediment remo

Dredging

Trucking.

The economic ranking of te

approaches to management of re

tion, as estimated by RESCON,

6.2.

The rankings presented in Tab

with experience or study findings

ing projects. However, there are e

needs to be exercised when interpr

results. In particular, RESCON d

technical feasibility of dredging o

it assumes these are always feasib

output quantities that are assume

trucked and the user needs to exe

the feasibility of these. For exaRESCON ranks dredging as the h

an annual dredged quantity in ex

 With the largest ever attempted d

in the world not exceeding 10 M

likely that this result is credible.

Experience with sediment

Gebidem indicates that flushing i

nique for removing sediment fromagrees with the RESCON findin

dredging are also potentially feas

economic and technical point of v

that one dredge would be requir

reservoir for sustainable operatio

T H E R E S C O N A P P R O A C H

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the reservoir. Experience on site confirms this find-

ing and led to the development of a concept to cre-

ate additional longitudinal channels to enhance

flushing. Such features, typical of an advanced de-

sign level, are not considered by the RESCON model.

Trucking and dredging are considered technically

infeasible for removing sediment from the reservoir

because it would require 129 years to remove the

sediment at 100 truckloads per day, or 66 dredges to

remove the same amount of sediment.

Baira Reservoir has been successfully flushed,

which agrees with the findings of RESCON. The

economically close second choice of RESCON is the

HSRS technique for partial removal of sediment andcontinued use of the facility in the long term as a

run-of-river facility. Thus, the first choice is not only

more economical, but also sustainable.

The findings for the Ichari Reservoir also seem

to confirm practical experience. The dam contains

no low-level gates for flushing, but if the gated spill-

way is used for flushing the achievable long-term

capacity is estimated at 35 percent, which is close tothat predicted by RESCON. The economic solution

from RESCON indicates that a sustainable manage-

ment approach for Ichari is optimal, which compares

well with the findings of the dam owners and op-

erators The optimal economic solution that is also

feasible from a technical point of vie

would require approximately 5 years

ment from the reservoir if 100 truck

ment were removed from the reservoi

RESCON predicted that sustainable

flushing would have the highest posit

return for Unazuki Dam in Japan. No

either the run-of-river or decommissio

once the reservoir has filled with sedim

dicted to have the next highest econ

Because the owners have successfull

reservoir twice to maintain flood con

RESCON proved to be effective for U

The Sakuma Dam in Japan was RESCON to be sustainable through i

of all four removal techniques, with d

ducing the highest economic benefit

have employed various techniques in

to provide successful sediment manag

RESCON’s predictions are correct for

economic value of each alternative;

assessment and prediction of the NPV bined techniques is a more complex ta

 ject for more detailed, i.e., feasibility l

Sensitivity Analysis

TABLE 6.2

SUMMARY OF RESCON ECONOMICS RESULTS

Reservoir Sustainable? Technologies (in order of Net Present Value)

Tarbela, Pakistan Sustainable Dredging / Flushing / HSRS (partial removal, run of river)

Gebidem, Switzerland Sustainable Flushing / Dredging / Trucking/ HSRS

Baira, India Sustainable Flushing / HSRS (partial removal, run-of-river)

Sefid-Rud, Iran Sustainable Flushing / Dredging

Ichari, India Sustainable Dredging / Flushing

Unazuki, Japan Sustainable Flushing / No Removal (run-of-river and non-sustainable)

Sakuma, Japan Sustainable Dredging / HSRS (partial removal run-of-river and non-sus

E VA L U A T I O N O F R E S C O N M O D E L

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sensitivity analysis of economic parameters for the

Tarbela case study was also performed. Results of 

all these tests are reported below.

The first set of general sensitivity tests was con-ducted on three existing reservoirs. The reservoirs

were selected to represent narrow, medium and wide

widths with respect to length. The reservoir choices

were: Strontia Springs Reservoir, USA, for the nar-

row option; Cabora Bassa Reservoir, Mozambique,

for the medium option; and Guanting Reservoir,

China, for the wide option. Testing of these three

reservoirs provided enough data to draw conclusionsas to the sensitivity of the model to reservoir geom-

etry.10

The second set of sensitivity results was gener-

ated from the general sensitivity testing by format-

ting the results according to Basson and Rooseboom

(1997), who studied empirical data from many res-

ervoirs and developed Figure 6.1, making use of 

experience and judgment to delineate ranges where

flushing is considered to be technically feasible. The

graph demonstrates the relationship between reser-

voir capacity, mean annual runoff and annual sedi-

ment load. Each data point in Figure 6.1 represents

a reservoir that has been flushed and whose flush-

ing success in terms of sediment removal has been

noted. Based on their findings, th

unsuccessfully flushed reservoirs

the right of the top inclined line

ing on a seasonal basis in tesustainability occurs in reservoir

inclined lines in the centre of th

ervoirs where single event-type f

ful fall below and to the left of th

A third set of sensitivity tests

RESCON’s ability to predict wat

teen reservoirs. Gould’s Gamma

reservoir yield as a function of theity, mean annual inflow, standar

inflow and the required reliabili

(probability of failure to deliver y

the Gould equation in Chapter 5.

cally shows that reservoir yield

ability of failure increases (reliab

other words, as more water is dra

ervoir for various uses, less is av

reliability for future stock.

Details of the sensitivity tes

presented in Annex J. The follow

marize the results.

General Sensitivity Testing

By selecting pre-existing geometr

variables that are arbitrarily var

pected range of possibilities arerelationships for the various geo

to the capacity

metric param

according to

taken from th

available for ea

The mode

changes in therameters gene

ticipated tren

increasing wid

a constant valu

result in lower10

100

1000

10000

100000

P    /    S    E    D

    L    O    A    D

    (   y   r    )

Note: CAP/Q10 (hour) shown as labels in graph

Strontia SpringsReservoir

Flood SeasonFlushing/sluicing

Flood Flushing:

44

15

8

12

15

1739

722

58

88

8

4824

629

7

102

531

82

6456

24

328

114

26

12533

8343 96

77

47

3

10

27

3

7441   41303

22

424

10

29

8

510

173016

19

26

236

22

21

29

1910

33

8217

32

26

7

11

26

4

14

104

33

9

78

8

11

FIGURE 6.1

EMPIRICAL FLUSHING RESULTS (BASSON AND

ROOSEBOOM 1997).

T H E R E S C O N A P P R O A C H

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load results in more sediment being deposited in the

reservoir prior to removal. Inspection of the results

leads to the conclusion that the RESCON model is

consistent.A summary of results from the sensitivity analy-

sis for RESCON as it relates to the technical feasi-

bility of flushing was developed. Similar to Basson’s

and Rooseboom’s Figure 6.1, Figure 6.2 relates the

ratios of capacity to mean annual runoff and capac-

ity and annual sediment load (with the axes reversed).

The figure shows that RESCON results imply that,

in general, flushing is potentially technically feasiblein cases where the reservoir capacity to mean an-

nual runoff ratio is less than 0.3 years and where

the capacity to sediment load ratio is less than 100

years. This implies that flushing could be the pre-

ferred sediment management technique when res-

ervoirs are hydrologically small and the sediment

loads are relatively high. The ratio of reservoir ca-

pacity to sediment load approximates the number

of years it will take for a reservoir to completely fill

with sediment if it is assumed that all the inflowing

sediment deposits in the reservoir. Whether the cut-

off should be at 100, 200 or more years should be

determined by economic analysis such as that of-

fered by RESCON. However, the general trend of 

the recommendation appears to make sense. For

example, in the extreme case, when a reservoir will

take, say, 1,000 years to fill with sediment, it is un-likely that pro-active sediment management tech-

niques will be required to ensure sustainable use of 

the resource. At the other extreme, if a reservoir

would fill with sediment within,

say, one year, pro-active sediment

management would definitely be

required to ensure sustainable

use.The lines indicating the areas

below which flushing is consid-

ered to be technically feasible by

Basson and Rooseboom (1997)

are also shown on Figure 6 2 It

The model was run and the yields for se

were determined using RESCON. The

that there are definite cases where th

applicable and where it is not. In genevoirs with yield/MAR greater than 0.

trend that increasing probability of failu

reliability of supply) allows more yiel

from the reservoir. This agrees with

ever, when yield/MAR is less than 0

predicts a reduction in yield for an in

reliability of supply. Clearly this is no

summary:RESCON performs well for reservo

reservoir yield is at least 40 percent

annual runoff. For situations where th

than 20 percent of the mean annual run

results are unreliable.

Sensitivity to Economic Parameters

Changes in economic parameters may

the ranking of desirable sediment mana

egies, but could also affect the amoun

removed with each strategy and magn

ables such as the timing of decomm

any retirement fund contributions. Sen

sis was performed on key economic

the Tarbela Dam case study to investi

fects and test the model for consisten

nomic intuition. The following par

10

1

100

A    R

    (    Y   e   a   r    )

F

F F

3%

1%

F = Flushing Technically Feasible according to RESCON

RESCON FLU

E VA L U A T I O N O F R E S C O N M O D E L

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varied: price of net reservoir yield (P1), rate of dis-

count (r), market rate of interest (m), cost of opera-

tions and maintenance coefficient (omc) and costs

of sediment removal for different techniques. Theresults of this sensitivity analysis are reported be-

low.

Sensitivity to P1: Unit Value of Reservoir Yield

 When P1 is doubled from US$0.1/m3 to US$0.2/m3,

the NPV for all strategies increases by nearly US$140

billion. However, the increase in NPV for sustain-

able solutions is somewhat higher than that for non-sustainable solutions. Also, the Long Term Capacity

Ratio (LTCR) increase by 31 percent and 6 percent

respectively for dredging and trucking. It follows that

the higher water prices generate incentives to keep

more storage capacity. In the case of flushing, changes

in economic parameters do not affect LTCR because

the latter is determined by engineering features rather

than economic optimization.

Sensitivity to r: Discount Rate

The discount rate determines the weight of future

benefit and cost relative to the present. When the

discount rate is lowered from 5 percent to 3 per-

cent, NPV for each strategy increases by nearly 50

percent but there is no change in rankings. Further-

more, the long-term capacity for dredging and truck-

ing increases, respectively, by 33 percent and 4percent. Thus, as with the increase in unit benefit of 

reservoir yield, lowering of the discount rate also

encourages retaining higher storage volumes.

Sensitivity to m: Market Rate of Interest

The annual retirement fund is calculated using the

market interest rate (i.e., the rate of return on in-

vesting the fund). The value of this annual contri-bution is reported only when decommissioning cost

exceeds any benefit of dam removal. For the Tarbela

case study simulation, it is assumed that US$2.5

billion is the net cost of decommissioning the dam.

The corresponding annual retirement fund is US$2

Sensitivity to omc: Operations a

Costs

Operations and maintenance cos

in the model by the parameter omficient defined as the ratio of ann

maintenance cost to initial constr

an omc value of 0.01 means that

tions and maintenance cost is 1

construction cost. The results of

efficient from 0.01 to 0.05 have

annual operations and maintenan

dent of sediment management strin omc reduces the NPVs for al

same amount except for non-sus

decommissioning. As no annu

maintenance cost is incurred afte

change in NPV for non-sustainab

ing) strategies is slightly lower. L

frequency of sediment removal a

sediment removal are all indepen

in annual operations and mainte

Parameters Describing the Cost

Removal

Costs of sediment removal depen

used. The parameters associated w

have been varied as shown below

Flushing: S2 (fraction of storacan be used in a year in whic

increased from 0.5 to 0.75.

HSRS: PH (unit value of wat

stream during hydrosuction

creased from US$0.005 to US

Dredging: CD (unit cost of dr

from US$2.62 to US$2.00/m 3

Trucking: CT (unit cost of trfrom US$50 to US$40/m3.

 When the cost of sediment re

NPV increases regardless of the st

term capacities for dredging an

T H E R E S C O N A P P R O A C H

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Conclusions

The case studies and sensitivity analysis results are

encouraging for the RESCON software, indicatingthat it is meeting the objective for which it was de-

veloped, i.e., to identify a management approach and

optimal techniques for management of sediment in

reservoirs at  pre-feasibility level. The possible ap-

proaches evaluated are:

Sustainable management with sediment removal

Non-sustainable management with no sedimentremoval

Non-sustainable management with partial re-

moval of sediment.

 With non-sustainable management, the reservoir

is either decommissioned at an optimally determined

time, or it is allowed to operate as a run-of-river

facility after complete siltation. Sediment manage-

ment techniques considered include flushing, dredg-

ing, trucking and HSRS. Of the seven reservoirs

tested, sustainable dredging and flushing were the

overwhelming choices by RESCON in terms of net

economic benefits.

The case studies indicate that the RESCON re-

sults are, within limits, confirmed by practical ex-

perience. The long-term capacities predicted by

RESCON for the reservoirs are generally lower thanwhat is anticipated in practice, which reflects the

simplifying assumptions made in the calculation of 

LTCR, as well as the RESCON model’s inability to

consider multiple techniques in parallel.

The case studies also brought to li

and Sakuma reservoirs) the need to c

control functions to better model wate

at certain reservoirs. Furthermore, it sirable to assess multiple managemen

in order to allow judgment regarding

ity of such management at a given sit

In the sensitivity analysis, exami

RESCON version of Basson and Roos

(Figure 6.2) confirmed, on economic

flushing could be the preferred sedim

ment technique when reservoirs are hsmall and the sediment loads are relativ

as a part of sensitivity analysis, RESC

hydrologically small reservoirs (Se/M

0.1) was tested, where yield is calculate

Gamma function using a 1 percent p

failure. It was decided that the 1 perce

of failure would be used for all values

eliminate discontinuities in cases where

fall below 1 percent during the lifetim

voir. Although this is a simplification

acceptable, it is an example of why R

pre-feasibility tool and why judgme

exercised in interpreting results.

Finally, sensitivity analysis on key

rameters was performed for a particul

namely, Tarbela Dam. The results show

with economic intuition and are alsointeresting policy implications in ter

water prices and returns on research

ment removal costs.

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Introduction

In many regions of the world there is an urgent need

to make the best use of existing reservoirs, improv-

ing the performance of their operation and incorpo-

rating the lessons learnt into the planning and

construction of new assets. In consideration of this,

the RESCON project undertook country dialogues

and training activities with the aim of launching con-

crete actions or projects on the ground. The objec-tive of such projects is the sustainable management

of reservoirs within the framework of life cycle

management.

Three countries were visited: Kenya, Morocco and

Sri Lanka. Each has specific sedimentation problems

and varying degrees of management established. The

RESCON field team met with local engineers and

managers to determine what the perceived needs are,

conducted reconnaissance of the problem reservoirs

and surveyed sedimentation volumes at some sites.

The RESCON team applied the RESCON model11

to a selection of reservoirs in an effort to aid the

countries in their planning strategies.

Kenya

The RESCON team visited Kenya in December 2001

to confirm findings pertaining to sediment yield and

reservoir sedimentation that were made during the

first Integrated Water Resource Management Strat-

h k l b d

the resulting system knowledge w

velop a plan of action for future ment. The Kenya project is disc

Annex G.

Although the RESCON mode

Kenya, the country report is inclu

book because it covers two impor

tershed management; b) sedimen

Morocco

Country dialogue began with Mor

A RESCON team worked with sta

Générale d’Hydraulique (DGH) t

isting reservoirs. Discussions wi

neers indicated that the results

analysis were in line with their e

derstanding of the reservoirs that

The RESCON approach produced

sedimentation management strat

ervoirs.

An interesting observation o

rocco is the sensitivity of the m

unit cost of dredging assumed.

As a follow-up step, the stud

pre-feasibility study that will extecation to all ninety-seven reservo

with the objective of identifying

management strategies.

Details on the Morocco appli

A

7. COUNTRY DIALOGUE

T H E R E S C O N A P P R O A C H

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Sri Lanka

In Sri Lanka, a pre-feasibility level sediment man-

agement study began in May 2002 by prioritizingthe existing reservoirs and dams in terms of relative

importance. The Mahaweli Authority of Sri Lanka

(MASL) and the RESCON team surveyed three res-

ervoirs in the Mahaweli River cascade to determine

sedimentation rates in August 2002. Sri Lankan

engineers were trained to use survey equipment.

Thereafter the five reservoirs were analyzed using a

specialized cascade system-version of the RESCONmodel to preliminarily identify management strate-

gies for the reservoirs.

A workshop was given in Sri Lan

the preliminary results of the RESCON

sis. Engineers were also given a tutoria

on experience in using the RESCONstudy allowed the preparation of draft

erence for a Reservoir Conservation

Plan. The reservoir conservation man

will include recommendations pertain

ecution of more detailed feasibility stud

mentation actions. Details of the Sri La

in Annex I.

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Summary of the Problem

Dams and associated water reservoirs are aging

around the world. Dam aging can be counteracted

when necessary with appropriate operation, main-

tenance and management policies and rehabilitation

interventions. Reservoir aging is determined by sedi-

ment accumulation rates. The “creeping” problem

of lost storage and reduced production capacity in

the water sector has several facets:

The lost storage capacity has an opportunity cost

in the form of replacement costs for construc-

tion of new storage if the present level of supply

is to be maintained.

There are direct economic losses in the form of 

less hydropower production capacity available for

sale, less irrigated land to produce food and re-

duced flood routing capacity. The filled reservoirs, with no benefits to pay for

their maintenance, will continue to be a liability

to their owners and may become a hazard.

The filled reservoirs may create a problem of de-

commissioning that has both direct and indirect

costs.

Storage retirement or decommissioning is emerg-ing gradually, in developed countries, as a new chal-

lenge for the engineering community. To date only

small dams have been decommissioned. Decommis-

sioning of large dams is very costly, full of technical

uncertainties and highly contentious on environmen-

Sustainability and Intergener

Dams are part of our strategic in

potentially very long life span. P

ful life of storage reservoirs cons

portunity for sustainable develop

not be missed by the engineerin

by society at large.

Inter-generational equity is a

to be applied to water storage pro

discourages the utilization of an

eration if a subsequent generati

with its consequences.

 Where the annual inflow of se

ervoir can be balanced by an eco

and environmentally acceptable

ment technique an opportunity e

sustainable use of the reser

intergenerational equity. Where it is forecasted that th

be achieved and that the reservoir

filled with sediments, appropria

quired for dealing with the resu

tions can comprise substantial p

(e.g., protecting the intakes and c

of-river scheme), change of purp

ation, cultivation, environmentextreme cases dam retirement usi

plete removal of the dam. Financia

actions can be achieved by establi

fund into which sufficient sums

posited annually to pay for any a

8. CONCLUSION OF THE STUDY AND RECOMMENDAT

T H E R E S C O N A P P R O A C H

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Sediment Management Alternatives

There are numerous ways of managing and mitigat-

ing reservoir sedimentation problems. These includemeasures to:

Reduce sediment inflows into the reservoir

Manage sediments within the reservoir

Evacuate sediments from the reservoir

Replace lost storage.

Each measure can be further sub-divided and each

has technical, environmental and economic benefits

and consequences. Each has been used for manag-

ing sedimentation problems around the globe and

sufficient expertise and tools are available for their

technical appraisal at the feasibility level and beyond.

Environmental and Social Safeguards

In too many cases in the past, insufficient attention

has been paid to the environmental and social im-

pacts of water storage projects. As a result there have

been some notable environmental and social impacts.

Environmental and social issues must be accorded a

status equal to economic expediency. Potential en-

vironmental and social impacts and where possible

potential opportunities for enhancement need to beidentified early on in the project life cycle (i.e., at

pre-feasibility stage) so that they can be investigated

thoroughly and dealt with appropriately during

project development. Where environmental and

social impacts that are unlikely to be mitigated suf-

ficiently are identified, a mechanism for abandon-

ing an option or the offending element of that option

must be in place. This book promotes the use of the“safeguards” approach to identify in broad terms the

environmental and social impacts of a project so that

they can be studied further in the next phase when

the project evaluation procedure and mitigation ac-

tions are designed

parently very little, if any, published in

the economics of reservoir sedimen

implication for sustainable developm

work is needed to assess the economicsediment management strategies that

the life of reservoirs to be prolonged ind

a framework should be able to answe

but distinct questions:

Is the extra cost incurred in unde

ment management activities worthw

of extending the productive life of

Is it economical to extend the life

definitely?

National level policy makers have

priorities. Management of existing rese

ing sediment management, very rarely

the top of the list. Two actions are requ

this attitude: (i) awareness raising; a

opment of a decision making tool thaat the policy level.

Planners and policy makers need a

to quickly and with little data apprais

cal, economic, environmental and so

of various methods available for manag

tation problems in order to prioritize c

ditures. The RESCON approach prov

assessing whether a project is sustainabwhen not, allows for the costs of esta

tirement fund.

The RESCON computer model w

as a demonstration tool of the RESCO

The model does not evaluate all poss

management methods. However, the

able should enable the user to ascert

feasibility level, what type of method most effective. The model also has b

environmental and social safeguardin

which, as well as acting as a checklis

ing major impacts, also guides the use

tification of a particular option that is

C O N C L U S I O N O F T H E S T U D Y A N D R E C O M M E N D AT I O N S

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The model has been tested against data from

numerous dams around the world and has been

shown to yield results in agreement with prototypes

and proven detailed mathematical models. TheRESCON approach to reservoir sedimentation man-

agement was also field-tried in Morocco and Sri

Lanka, where managers and engineers were trained

and the approach used to appraise methods of sedi-

ment management on a representative sample of res-

ervoirs.

Policy Implications

The RESCON concept, as its application develops,

has important policy implications, including:

Influencing the way policy makers and engineers

approach dam design

Promoting sustainable dam projects through the

application of the life cycle management approach Introducing the concept of intergenerational eq-

uity

Encouraging the establishment of a retirement

fund.

Recommendations for Further Work

The RESCON project has stepped up to the chal-

lenge of finding a way to achieve reservoir conser-

vation and sustainable management of dams. It is

hoped that this small, initial step will encourage other

key players to follow in this path, which will require

considerable effort to reach its goal.

There is a lot of work still to be done. Some of 

the more important aspects are outlined below.

Watershed management

Too little is understood about catchment erosion and

its relationship to river sediment yields. This im-

pacts the ability to develop mathematical relation-

Multi-criteria analysis

The method developed in RESCO

rily on an economic analysis of

mental and social impacts are de“safeguard” approach. This is a ty

prevent options which have una

that cannot be mitigated from be

preferred solution.

An alternative means of con

mental and social issues (and

other issues that may be of conc

concept of multi-criteria analysis

plest form MCA appraises each o

criterion independently and repo

dependently.

One of the benefits of using t

to option appraisal is that it allo

ment of options where environ

enhancements have been include

Improvements to the RESCON There are more than forty 45,00

reservoirs worldwide, and about

facilities are added each year, ma

countries. Each dam and reserv

characteristics. Users should reg

model as a preliminary tool to

adapted as necessary. Based on pr

tions, we recommend the follow

Further runs of the model us

to identify errors or limitation

Explicit inclusion of flood man

Explicit inclusion of other sedi

options, such as: density curr

ing and reservoir bypass

Ability to model a cascade of“Better at

Ability to model seasonal flow

to better distinguish hydrologi

are more favorable to flushin

Ability to set a limit to sedim

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 We are grateful for the comments and contributions

provided by the reviewers of this book, namely:Khalid Mahmood, Dale Whittington, John Nestler

and Giampaolo Di Silvio. Atila Bilgi undertook the

review and editing of the final draft. We are also

grateful for the direct contribution to the project

made by Rodney White, Ed Atkinson, Katherin

Golitzen, Hideki Otsuki, Thomas Haglund and Faten

Saihi and for the for assistance provided to us by

Beatriz Saenz-Shahin (US Army Corps of Engineers).Thanks and acknowledgements go to the authori-

ties of Kenya, Sri Lanka and Morocco for their co-

operation during the country missions.

The international experts who participated in the

launching workshop (Washington December 9-10,

1999) provided invaluable assistance with helpful

comments and advice in the early stages of the

project. They are: A. Benavidez, Dan Deely, Edmundo

Garcia Agudo, Emilio Colon, Gene Sturm, Gerrit

Basson, Guido Testa, Henrique Chaves, John Demus,

Mohammad bin che Jusof, Rando

ert Mendelsohn, Rollin HotchkiTed Yang, Tetsuya Sumi and Dirk

The suggestions and encourag

 World Bank colleagues have been

the research. We would like in p

Andrew Macoun, Satoru Ueda, Joh

Lopez-Rivera, Safwat Abdel-D

Hanbali, Vahid Alavian and Adel

fully acknowledge the assistance othe World Bank Research Commi

the University of Connecticut fo

search possible and would like

leagues who facilitated the fundi

Finally, we would like to th

assistants Shigekazu Kawash

 Johndrow and Mustafa Kapadia.

not have been accomplished with

astic help.

9. ACKNOWLEDGEMENTS

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 Workshop Objectives

The first step of the RESCON team was to seek ad-

vice from a group of highly qualified experts in a

workshop session held in Washington, DC, USA on

December 9-10, 1999. The workshop was attended

by twenty-five representatives from a broad range

of stakeholders, including end-users (owners), aca-

demic and other research institutions, development

organizations and consultants. Several Bank staff 

attended as well. The objectives of the workshop

were as follows:

Describe the processes that define relationships

within and between the various parameters that

determine the economic feasibility of sustainable

management of water storage reservoirs

Identify the principal parameters that impact sus-

tainable management of storage reservoirs Determine whether, in principle, it is possible to

develop functional relationships, which can be

presented mathematically or graphically, to de-

scribe the behavior of the identified parameters

Formulate mathematical relationships for the se-

lected parameters, where possible

Propose alternative means to analyze and incor-

porate the impacts of identified parameters thatcannot be expressed in terms of mathematical

relationships in the economic optimization

Identify criteria that can be used to evaluate the

technical feasibility of managing sediment in res-

d l l

 Workshop outcomes

The expert input in the early stag

proved to be invaluable. Consens

several key aspects that substanti

RESCON project. The conclusion

are summarized below.

Reliability of Current PredictiSediment Related Problems

Catchment soil erosion is les

than the process of reservoir

The Universal Soil Erosion eq

be used in other environme

which it was developed and c

nia), not even for sensitivity

The most reliable approaches fsion rates are considered to b

creasing complexity): (i) sed

(where available); (ii) flow-sed

(when sufficient data are avail

stream power equations (pro

Stochastic Nature of ErosionProcesses

Long-term average values of sedim

sitivity analysis should be used at

f b l l l A

Annex A: LAUNCH WORKSHOP

T H E R E S C O N A P P R O A C H

Catchment Management financial plan for funding asset retirem

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Catchment Management

Catchment management should be considered as a

factor influencing the sediment deposited annuallyin the reservoir by means of a coefficient that takes

into account management practices. Until a litera-

ture review has produced better data, a sensitivity

analysis based on current evidence should be used

at option assessment and at pre-feasibility level. At

the project feasibility level, more specific analysis

by experts in the subject may be required. However,

except in very small catchments, catchment man-

agement alone should not be relied on to signifi-

cantly reduce sediment inflows to reservoirs.

Environmental and Social Aspects

Environmental and social aspects are complex is-

sues that are difficult to quantify in monetary terms.

Nonetheless they should be given the same “weight”as technical and economic aspects and be consid-

ered at an early stage of the option assessment pro-

cess using a classification/ranking approach. This will

help to inform the subsequent feasibility analysis.

Economic Analysis in the Presence of Long Life

Span Periods

The choice of discount rates to assess the economic

viability of reservoir projects is a controversial and

extensively studied subject in academia. However,

there is no reason why reservoir projects, although

having a much longer life span than most other in-

frastructure projects, should be granted discount rates

different than other project types. The workshopconcluded that a constant discount rate rather than

one that varies over time should be used and, as with

all projects, the sensitivity of the economic viability

of the project should be tested using a range of dis-

count rates

financial plan for funding asset retirem

ment.

Financial Approach for Funding Ament/Replacement

Retirement is only one of the available

necessarily the preferred option, or e

table one. At the feasibility stage, the re

should be addressed on a conceptual le

should ensure resources for project re

site restoration. Monitoring of a res

(notably sedimentation, structural co

terials, change in use) should assist in

how the residual life of the asset comp

one anticipated at project conception

posits to the fund should be increased

estimate of residual life falls short o

pated. Deposits could be reduced in

case (longer residual life). This mechprovide an incentive for allocating s

for recurrent operation and manag

assets.

LIFE CYCLE

Operation

Development

Planning

LIFEC

L A U N C H W O R K S H O P

Available Technologies for Recovering Heavily Life Cycle and Evaluation Pro

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g g ySilted Reservoirs

Several sediment management techniques have beendeveloped and validated on reservoirs around the

world. There is consensus on the readiness of such

techniques for reliable application, provided well

identified pre-conditions are fulfilled.

y

The life cycle of a dam should be

framework for sediment manSustainability should be define

reservoir’s purpose. Planning, dev

eration are the key phases of a co

The benefits the dam provides s

cally reviewed through an evalua

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Introduction

Sediment accumulation leads to reductions in stor-

age capacity, flood control benefits, power genera-

tion capability, regulation of irrigation and water

supply releases, navigational and recreational use;

and in extreme cases it can lead to dam failure. The

purpose of this review is to provide a brief introduc-

tion to various aspects of reservoir sedimentation as

they relate to the needs of the RESCON project. The

focus is on economics and policy issues pertaining

to sediment management, with some coverage of the

engineering and physical sciences literature. The

major topics included in the review are:

General benefit-cost analysis and its application

to sediment management

Sustainability and intergenerational equity

Reservoir sedimentation management  Watershed management

Multipurpose dams and multi-objective optimi-

zation

Retirement of dams.

Benefit-cost Analysis

The literature on benefit-cost analysis in relation to

dams has traditionally focused on individual dams

(e.g., Paranjpye. 1988; Goldsmith and Hildyard,

) h h h f

is equal to dredging cost, provid

tional cost is utilized to store sedEconomic analyses of water p

uncertain flow of costs and ben

the stochastic nature of stream flo

problem for the benefit-cost analy

porating this uncertainty into me

benefits (see, for example, Quirk

Some studies of wider econom

also exist. For example, Alesey

Isserman (1998) examine the e

country income, earnings and em

in local regions in the United Sta

between 1975 and 1984. They f

built for flood control and thos

cities and with fewer people with

impact on the economy. They a

project may be recommended on

tive impact on the nation but cousite effect on the local economy.

In the past, dam projects did

consider sediment accumulation a

environmental effects. An indicat

importance the environment has w

becomes apparent when a hydro

up for re-licensing; authorities in

for example, consider the effecspecies, fisheries and other dow

The costs of minimizing downstr

substantial.

In general, environmental con

f l l

ANNEX B: LITERATURE REVIEW

T H E R E S C O N A P P R O A C H

count rates. This is discussed further in the follow- in benefits obtained. Sediment manag

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ing section.

Sustainability and Intergenerational Equity

Sustainability may be broadly viewed as “meeting

the needs of the present without compromising the

ability of future generations to meet their own needs”

 WCED (1987). However, there is much ongoing

debate over the precise definition of sustainability,

sustainable development and related terms. Some of 

the key papers for the reader interested in followingthe debate are Asheim, Buchholz and Tungodden

(2000), Chichilnisky (1997), Costanza and Patten

(1995), Dasgupta and Maler (1995), Farmer and

Randall (1997), Howarth, (1997), Howe (1997), Lele

(1991), Norton and Toman (1997), Pezzey (1997),

Solow (1992). The conclusion is that sustainability

and intergenerational equity are closely linked. For

example, Solow (1974) proposes that sustainabilityshould allow intergenerational trade-offs, but no

generation should be favored over any other. Indeed,

independent sustainable preferences can define

shadow prices for sustainable solutions, which can

be used for project evaluation and for the character-

izations of optimal solutions (Chichilnisky, 1997).

Howe (1997) links sustainability to the supply side

and to the capacity of a society to maintain or in-crease the level of some measure of aggregate utility

while Howarth (1997) argues that intergenerational

 justice can be assured by endowing future genera-

tions with a structured bequest package. According

to Norton (1995) this package includes specific en-

dowments of reproduced capital, technological ca-

pacity, natural resources and environmental quality.

There have been a few case studies conducted

on sustainable management of water resources, e.g.,

by Arntzen (1995), Bobba (1997), Carroll (1997),

Charlton (1997), Nguyen (2000). These studies

strongly call for incorporating the sustainability cri-

teria in early stages of planning A balance must be

practiced on sustainable basis, if the am

ment removed is equal to the incomin

Even under non-sustainable aintergenerational equity can be achiev

ably defined retirement fund.

Estimate the NPV of a project requ

a discount rate. Higher discount rates

utilization of the endowment, leaving

ture generations. Controversy still ex

the proper choice of a discount rate an

lighted in a special issue of the  Journ

mental Economics and Management (199to Moore and Viscusi (1990), 2 perce

able rate to be used for many cases, wit

for positively correlated net benefits

negative benefits. Lyon (1990) addres

lem of determining discount rate poli

into account economic principles an

constraints. He suggests the use of a

of capital approach to improve discoScheraga (1990) argues that discoun

vary according to resources under cons

the time period involved. There is co

no particular discount rate is suitabl

sible applications (see, for example,

There is also the opinion that “a defe

sophical basis for long-term intergen

counting has yet to be found” Howe

Reservoir Sedimentation Manage

Dam construction disrupts transport

in rivers causing an imbalance betwee

outflow. The problems this causes ar

they can occur upstream and downstr

widely from one site to another. A m

sedimentation on reservoirs is the lo

capacity. The extent of storage loss de

sediment yield as well as other physic

teristics Average annual storage loss

L I T E R AT U R E R E V I E W

Sedimentation reduction measures include up-

l l f d

trol, sedimentation control, as

b f l k h d

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stream soil conservation practices, control of distri-

bution of deposits, construction of debris basins and

control of turbidity (Yang, 1999). Sediments may

also be removed from the reservoir by various means.

Common techniques for such removal include flush-

ing, hydraulic dredging, trucking and hydrosuction.

These techniques are described briefly below. See

also Morris and Fan (1998).

Watershed Management

 Watershed management is a broad concept incor-

porating the plans, policies and activities used tocontrol water and related resources and processes

in a given watershed. Watershed management ac-

tivities can range from hands on guidance to farm-

ers about how to control runoff to multi-state

initiatives like those under way to improve the health

of the Chesapeake Bay in the USA. Successful wa-

tershed management strives for a better balance

between ecosystem and watershed integrity and pro-vision of social and economic goals. Stanford (1997)

discusses several general objectives that can be man-

aged within a watershed context.

Government attempts at watershed management

have been ongoing in the United States for more than

half a century, but the science of watershed man-

agement is still evolving and many of our current

activities are, in essence, experimental. Organizationsfor watershed management are most likely to be ef-

fective if their structure matches the scale of the

problem.

 Watersheds release soil and water to downstream

areas with consequences that may have beneficial

and/or harmful dimensions (see White and Runge,

1994). Watershed management can be important for

environmental issues like water quality, flood con-

benefits like hydropower gener

Hufschmidt (1986) report that w

ment could be economically attra

Pong water resources project on

count rate. Two possibilities wer

with watershed management and

results are shown in Table B.1.

 Wang, Hu and Kao (1998) de

of watershed management on the M

Tan reservoirs in Taiwan, the pri

ing reduction of sediment d

consequent increase in hydropowbenefit-cost analysis of such man

dams (using a discount rate of 5

period from 1981 to 2010, with

yielded a benefit-cost ratio of 1.18

million new Taiwan dollars.

Flushing

Flushing is the term given to threservoir level by means of low-l

dam to induce riverine conditio

reservoir and thus mobilize and e

previously deposited. The techni

ticed on many dams throughou

with great success.

Factors influencing flushin

2000):

Reservoir shape (best results f

row reservoirs)

Reservoir volume (the smalle

ume in comparison to the an

the better the results)

Hydraulic conditions (best re

tion of riverine conditions in

Predictability and magnitude o

Mobility of reservoir sedimen

Major factors limiting the ap

ing are: downstream effects and

TABLE B.1

50 YEAR GROSS BENEFITS OF NAM PONG WATER

RESOURCES PROJECT (million Baht)

T H E R E S C O N A P P R O A C H

sediment. Dredging may focus on removing silts,

i di d l i ifi h

gramming is a valuable tool for assistin

i i

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organic sediments and cleaning specific areas such

as hydropower intakes, navigational channels and

recreational areas. An important issue with dredg-

ing is availability of suitable disposal sites. When

calculating dredging costs, the cost of disposal land

should be included. A compilation of dredging cost

has been carried out by Basson and Rooseboom

(1999).

Trucking

This technique, like hydraulic dredging, involves

physical removal of sediment but requires drawdownof the reservoir. After the water is removed, sedi-

ment is transferred into trucks and transported to a

suitable site. A limitation hindering its frequent use

is the availability of a suitable site to dump the ex-

cavated sediment. The cost of drawdown, transpor-

tation cost and, if applicable, land cost of the dumping

site should be included in the benefit-cost calcula-

tions.

Hydrosuction

This is one of the lesser used techniques for sedi-

ment removal (Hotchkiss and Huang, 1995). The

technique is similar to that of traditional dredging

but uses the hydraulic head created by the dam as

the source of energy for sediment removal. Sediments

are deposited downstream of the dam. Hydrosuctionmay be of two types, hydrosuction dredging and

hydrosuction bypassing. Dredging involves the re-

moval of previously deposited sediments, while by-

passing intercepts incoming sediments before settling

in the reservoir. According to Hotchkiss and Huang

(1995) this technique has certain criteria of appli-

cability, such as particle size, reservoir elevation and

turbidity, which need to be verified in advance.

Economics of Multipurpose Dams andMultiple Objective Programming

managing water resource systems in p

socio-ecological systems in general.

applications includes transportation,

tion for research activities, economic

quality of life, managing an academic

game theory and many others. The m

signed to find the preferred solutions

in which discrete alternatives are eval

criteria or factors ranging from cost (q

rion) to aesthetics (quality criterion

provides a viable way for structuring

ing a problem that is otherwise not wThere is considerable literature on t

applications of multi-objective (mult

cision techniques—see, for example, C

and Harboe (1992). A special edition

Resources Bulletin (28, 1992) is devote

and explains the various techniques in

(1992) provides an overview of all the

lished in this special issue. Ko et al several multi-objective tasking method

programming, compromise programm

off development programming to th

Reservoir system in Korea in order t

best method. Also, a manual publishe

partment of the Environment, Trans

Regions (DETR), UK, explains in deta

pects of MCA. It describes MCA as a t“can be used to identify a single most

tion, to rank options, to short-list a lim

of options for subsequent detailed appra

to distinguish acceptable from unacc

bilities” (Dodgson, et. al, 2000). An

approach is presented in Krawcyzk

develops an optimization model usin

support tool to arrive at environmenta

decisions. This model makes use of con

levies which provides a range of fea

each with a different trade-off between

environmental indicators.

L I T E R AT U R E R E V I E W

pacity, affects the turbines and consequently increases

the cost for electricity production and reduces ben

with case studies, is available in

Retirementof Dams and Hydroelectr

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the cost for electricity production and reduces ben-

efits. As these benefits decrease, the pressure to re-

tire or decommission increases.

There are three basic options for managing an

aging dam. The dam can be rehabilitated, modified,

or completely removed. Decommissioning should

consider sediment management in detail as removal

of a dam might cause an uncontrolled release of sedi-

ment downstream affecting the ecosystem, geomor-

phology and human activities. See Zhou and

Donnelly (2002).

Partial or complete removal may be accomplishedas a staged process extending over a period of years

to reduce the rate of sediment release. An in-depth

explanation of the evaluation method for this, along

Retirement of Dams and Hydroelectr

1997). An example of retiremen

four dams built on Lower Snake R

States. See Lansing (1995) and als

sion on Dams (2000).

Economics requires analysis

ment alternatives, calculation of

alternative and finally compariso

costs. The benefits and costs sho

a manner that is equitable from an

perspective. According to Solow

generations are entitled to draw long as they add to the stock of

tal.”

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State of Knowledge

Some of the principal reasons for the current lack of 

understanding of sediment transport processes and

how they relate to catchment processes are a lack of 

accurate and appropriate data, inability to correctly

formulate the physics of sediment transport processes

in mathematical terms or to successfully simulate

sediment transport or catchment processes in a way

that allows solution of practical problems. Erosion

and sediment transport processes are extremely com-

plex and are driven by interaction of large numbers

of variables.

Measurement of sediment load in rivers requires

determination of the magnitude of the sediment load

that is in suspension in the water as well as the pro-

portion of the load that is transported along the ri-

verbed. The suspended load varies as a function of 

space and time in the water column and accuratemeasurement is almost impossible. Similarly, bed load

transport varies over the width of the river in both

space and time, making its measurement very diffi-

cult. Adams (1980) indicated that the measurement

error in the data that he used to estimate sediment

yield could vary between +100 percent and -50 per-

cent, which is not unusual.

The current formulation of sediment transportand catchment processes is empirical in nature. All

sediment transport equations that are now used to

simulate sediment transport phenomena are empiri-

cal correlations of experimental or field observations,

f l f h l

data it is found that the error is b

and 150 percent (Yang 1996).Sediment transport in rivers i

nent of the whole process, from t

of sediment particles in a catchm

riverbanks and streambeds, to the

re-suspension of sediment as it i

source to sink. This increases the

problem—compounded by vari

cesses in both time and space, w

related—making it difficult to so

racy. For example, the amount

ported in a river is dependent on

the sediment and the sediment tr

the river. It may happen that the s

capacity of a river is very high, bu

sists of rock. While transport cap

this is not a guarantee that large

are actually carried by the river. ply may vary in time; further, a

sediment transport can result in a

ment discharges.

Sediment Delivery Ratio

The relationship between catchmthe amount of sediment discharg

complex and is affected by proc

space and time. Sediment that is

ers originates from riverbanks, r

b d ll h h

ANNEX C: WATERSHED MANAGEMENT

T H E R E S C O N A P P R O A C H

is related to catchment erosion by

making use of a coefficient known DRAINAGE AREA VS SEDIMENT D

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making use of a coefficient known

as the Delivery Ratio, which is cal-

culated as the ratio between the

volume or mass of sediment dis-

charged in a river and the volume

or mass of soil eroded in its catch-

ment.

An example of the relationship

between Delivery Ratio and catch-

ment area for selected areas in the

United States is shown in Figure

C.1.11  This figure indicates thatthe Delivery Ratio can vary be-

tween 5 percent and 70 percent,

depending on the size of the catch-

ment. For catchments greater than

100 km2 the figure indicates that

delivery ratios can be significantly

lower than 10 percent. This dem-

onstrates the large amount of sedi-ment storage that can be found in

the river systems of a catchment.

Furthermore, for a given catch-

ment size there is significant

spread of sediment delivery ratios. Catchment size

is obviously not the only factor defining Delivery

Ratio. Topography, stream pattern, climate and a

number of other factors determine this relationship.Full understanding of these relationships is lack-

ing. For example, by using exactly the same data

set, Griffiths (1979) and Adams (1980) estimated

sediment yield from rivers in the Southern Alps of 

South Island, New Zealand that differed by 70 per-

cent. On one of the rivers there was a 48-fold differ-

ence in sediment yield estimates (Morris and Fan

1997). In spite of these differences these two au-

thors view their results as being in “general agree-

ment.” This degree of uncertainty is typical of 

sediment transport work.

the bigger the catchment the lower the s

per unit of area. This is demonstrated

Pemberton (1982) for the semi-arid r

 Western United States (Figure C.2).Satisfactory determination of the i

tial parameters on sediment yield is com

of the large number of factors involved

should be considered include the strea

order, climate and climate change, veg

ogy, soil types, catchment activities lik

and urbanization, rainfall characteristi

of stream bank and streambed erosion

and frequency of landslides, topograp

etc.

Temporal variability

1

10

100

0.01 0.1 1.0 10.0 100.0

Drainage Area (Square Mile)

    S   e   d   i   m   e   n   t   D   e   l   i   v   e

   r   y   R   a   t   i   o    (   P   e   r   c   e   n   t   o   f   E   r   o   s   i   o   n    )

Red Hills Psysiographic Area - Texas and Oklahoma

Missouri Basin Loess Hills - Iowa and Nebraska

Blackland Prairies - Texas

Sand - Clay Hills - Mississippi

Piedmont Psysiographic Area - North Carolina,South Carolina and Georgia

DRAINAGE AREA VS SEDIMENT D

Details related to certain procedural and technical as Figure C.1 Drainag

Sediment Delivery Ratio

Source:  Boyce, R.C.,1975. “Sediment Routing with Sediment-Delivery Rations,” p

and Prospective Technology for Predicting Sediment Yields and Sources . ARS

mentation Lab., Oxford, Miss.

 W AT E R S H E D M A N A G E M E N T

the river is depe

ability of sed

FIGURE C.2

CATCHMENT AREA VS SPECIFIC SEDIMENT YIELD

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concentration during the course of a flood in the

Mississippi River at Chester, Illinois, USA. The fig-

ure is a good example of a typical phenomenon—

where sediment concentrations are often higher

during the rising limb of ahydrograph and lower at the

peak.

This phenomenon causes par-

ticular problems for the hydrolo-

gist trying to predict sediment

inflows to a reservoir. Sediment

data are often scarce compared to

hydrological data. Therefore the

hydrologist will be tempted to de-rive a relationship from sediment

concentrations and flow records

in an effort to predict sediment in-

flows even though there is no

y

point in time.

Seasonal ch

transport resu

in rainfall and s

in vegetation ch

catchment and

tors. Inter-ann

occur for the s

Long tem c

from changes

ditions. Roosesents a mass c

load in the Oran

tion of time fr

(Figure C.5).

is observed a

exact reason f

slope is not kn

nation could bvation structure

but the exact re

when they we

the effect materialized is unknown

10

100

1000

10 000

10.0

1.0

0.1

1

0 10 100 1,000 10,000

10 100 1000 10 000 100 000

A = DRAINAGE AREA, IN SQUARE KILOMETERS

A = DRAINAGE AREA, IN SQUARE MILES

    Q   s

  =    S    E    D    I    M

    E    N    T    Y    I    E    L    D

    (    C    U    B    I    C

    M    E    T    E    R    S

    P    E    R

    S    Q

    U    A    R    E    K    I    L    O    M    E    T    E    R

    P    E    R

    Y    E    A    R    )

    Q   s

  =    S    E    D    I    M

    E    N    T    Y    I    E    L    D

    (    A    C    R    E    F    E    E    T    P    E    R    S

    Q    U    A    R    E    M    I    L    E    P    E    R

    Y    E    A    R    )

Sediment yields from survey of28 reservoirs in semi-arid climate of U.S.A.

Qs = 1.84A-0.24

(Qs = 1.08A-0.24) metric

VARIATION OF SEDIMEDU

20,000

25,000

Susp. Sed. Conc.

Streamflow

30,000

    S    t   r   e   a   m    f    l   o   w

    (   m

    /   s    )

Source:  Strand, R.I., and Pemberton, E.L., 1987. “Reservoir Sedimentation,” In Design of Small Dams .

U.S. Bureau of Reclamation, Denver.

T H E R E S C O N A P P R O A C H

period, the number of sheep in the

catchment of the Orange River in- DISCHARGE VS SEDIMENT C

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g

creased quite significantly. Follow-

ing conventional argument, one

would reasonably expect that ero-

sion and therefore sediment yield

should increase if the sheep popu-

lation increases. Sheep graze grass

down to the roots and expose

more soil to the erosive forces of 

water. Although a change in sedi-

ment load has been observed, the

relationship between catchmentprocesses and yield is not clearly

known. Prediction of the impact

of alternative catchment manage-

ment techniques is therefore not

reliable at this point in time.

3.00

2.80

2.60

2.40

2.20

2.00

1.80

1.60

1.40

1.20

1.000.80

0.60

0.40

0.20

0.000 50 100 150 200 250 300

Discharge (m3

 /s)

    C   o   n   c   e   n   t   r   a   t    i   o   n    (    %

     M   a   s   s    )

1550

1000

500

0

2000

    C   u   m   u   l   a   t   i   v   e    S   e   d   i   m   e   n   t   L   o   a   d    (   1    0    6   t    )

Cumulative Sediment Discharge1929 – 1969Orange River, South Africa

FIGURE C.5

LONG-TERM VARIATION OF CATCHMENT SEDIMENT YIELD

Source:  Rooseboom, A., 1992. “Sediment Transport in Rivers and Reservoirs: A S

spective,” Report to Water Research Commission of South Africa, by Sigma Bet

neers, Stellenbosch.

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Introduction

In many areas of the world the life span of reser-

voirs is determined by the rate of sedimentation,

which gradually reduces storage capacity and even-

tually prevents facilities from reliably supplying water

and power. Many major reservoirs are approaching

this stage in their life.

One way of preserving reservoir storage is to flush

sediments through purpose built outlet works. This

technique can be applied to existing dams (withmodification of the engineering works) and to new

dams. However the technique is only effective un-

der certain favorable conditions and is not univer-

sally applicable. This section outlines the criteria

required to make flushing successful.

A recent study carried out by HR Wallingford

(White, 2001) has evaluated where and when the

flushing of sediment may be an appropriate methodof sustaining reservoir storage. The study included

the following aspects:

An assessment of the scale of the problem of res-

ervoir sedimentation

An estimation of the volume of storage that

is likely to be required to meet continuing de-

mand internationally A review of the current state of knowledge of the

mechanism of sediment flushing from reservoirs

A review of the worldwide experience of sedi-

ment flushing from reservoirs

d f l f h f

by making use of the natural ene

water.

There is a distinction betwee

ing and sediment sluicing. Sedim

cerned with the removal of sedi

settled in the reservoir at a previo

passing through incoming sedi

flushing event, whereas sedimen

cerned with only passing sedim

reservoir during times of flood.

sometimes difficult to make but, gflushing is used to remove sedim

cluding sands and gravels where

ing generally removes only the fi

Factors that Influence Viabiliof Sediment Flushing

The following sections outline t

fluence the viability and efficienc

reader is referred to Atkinson (1

the methodology for estimating

ing at a given reservoir based on r

sediment types, discharge regime

pacity, etc. The relationships pre

been used to determine the techflushing of a given reservoir in th

 Where more detailed studies are

tionships in Atkinson together w

be used. Volume II of this book o

d l d l d b A k

ANNEX D: ASSESSING FEASIBILITY OF FLUSHING

T H E R E S C O N A P P R O A C H

The hydraulic capacity of the outlet must be suf-

ficient to maintain the reservoir at a constant level

Site-specific factors

The most suitable conditions for flush

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during the flushing period.

Flushing discharges of at least twice the mean

annual flow are required.

Flushing volumes of at least 10 percent of the

mean annual runoff should be anticipated.

For best results the flushing outlet should be situ-

ated close to the dam and as near as possible to

the original river bed elevation.

Quantity of water available for flushing

There must be enough water available to transportthe required volume of sediment. This has the fol-

lowing implications:

Reservoirs where the annual runoff is large com-

pared with the volume of the reservoir are best

suited for sediment flushing.

A regular annual cycle of flows and a defined flood

season provide optimum conditions for sedimentflushing. This favors sites in monsoon areas and

sites where flood flows are generated by annual

snowmelt in the spring and summer months.

A balance must be achievable between the sig-

nificant quantities of water required for sediment

flushing and water required to satisfy demands

at other times of the year—for irrigation and hy-

dropower, for example.

Mobility of reservoir sediments

The nature and quantity of river sediments are im-

portant factors in determining whether the quantity

of water available for flushing is adequate to remove

the desired quantity of sediment from the reservoir.

Graded bed sediments produce conditions which

are the most conducive to efficient flushing. Such

conditions are typical of gravel rivers with a varying

bed material composition. In large rivers this situa-

tion is found where the longitudinal bed gradient is

between, say, 0.001 and 0.002. In smaller rivers the

equivalent range may be 0 002 to 0 005

found in reservoirs which approximat

incised channel that develops during fl

relatively narrow reservoirs are better s

ing than short, wide, shallow reservoi

 Where reservoirs are very wide, flus

produce a narrow incised channel th

posited materials and only a portion o

capacity can be regained.

Summary

Reservoirs in the “upper and middle rers are likely to be best suited to sedim

for the following reasons:

In the lower reaches reservoirs are

inundated areas that had previous

plains and these areas would not b

the incised flushing channel which

of limited width. The longitudinal slope available fo

channel is relatively small thus

amount of sediment transported.

Reservoir volumes in the lower rea

to be larger compared with the mea

off and hence water availability b

straint on sediment flushing.

 Worldwide Experience of Sedime

 White, 2001, looked at fifty reservoirs w

or have been flushed. In some cases the

successful, in others there was little o

The main findings from this worldwid

of which confirm directly the semi

analysis of those hydraulic factors th

ment flushing, are:

The hydrology and sedimentology

ment: The hydrology and sedimen

A S S E S S I N G F E A S I B I L I T Y O F F L U S H I N G

a storage capacity less than 30 percent of the mean

annual inflow. The smaller the reservoir, the

h h f i b i f ll fl h d

tion of sediment load, may be

native during the early life of

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greater the chance of it being successfully flushed

and the larger the likely residual storage capacity.

The sediment deposition potential: Flushing is vital

for the preservation of long-term storage in res-

ervoirs where the sediment deposition potential

is greater than 1 percent to 2 percent of the origi-

nal capacity.

The shape of the reservoir basin: Worldwide ex-

perience confirms that the shape of the reservoir

basin can have a large impact on the practicabil-

ity of effective flushing and the residual storagecapacity. Narrow steep-sided reservoirs in valleys

with a steep longitudinal slope are the easiest to

flush. Wide valleys where the impoundment cov-

ers former floodplains can be less effectively

flushed, because the deposits tend to consolidate

and are remote from the flushing channel.

The deployment of full or partial drawdown: Full

drawdown and empty flushing have been foundto be much more effective than partial drawdown.

The low-level outlet facilities provided:  World-

wide experience confirms that, for effective flush-

ing, the low-level outlets must be both low

enough and of sufficient capacity to allow sig-

nificant drawdown of water levels to be controlled

during the time of year when flushing is under-

taken. Proportionately larger outlets are requiredfor flood-season sediment sluicing during the

flood season than for sediment flushing at the

outset of the flood season.

The scope for enhancements to flushing: Fluctua-

tions in water level and discharge during flush-

ing are beneficial to the promotion of bank

slumping, increasing the rate of sediment move-

ment. Also, the deployment of lateral and longi-

tudinal diversion channels has been successfulin promoting flushing in reservoirs which are hy-

drologically large or contain significant propor-

tions of deposition in areas remote from the main

flushing channel

Geographical Areas Suited to

Climatic zones

An understanding of the prec

throughout the world may allow

climatic zones based on tempera

tion regimes. This may in turn pe

of areas of high and low erosion

to classify distinct climatic zonemerge into one another rather

boundaries, but a number of ge

been produced.

There have been many clim

produced but one of the most co

the original Koppen classification

with eight climatic regions based

ture zones and one moisture zondomination of air masses. These

lows:

Tropical Wet

Tropical Wet and Dry

Tropical Desert

Mid-Latitude Wet

Mid-Latitude Winter Dry Mid-Latitude Summer Dry (M

mate)

Polar Wet and Dry

Polar Desert.

Hydrological characteristics

Experience has shown that low r

els provide the most effective co

ment flushing. To allow water lerequires confidence that rainfall

to refill the reservoir. It follows

wet and dry seasons will be favora

flushing regime Such a climate is

T H E R E S C O N A P P R O A C H

The availability of water will also affect the dura-

tion and discharge rate of the flow required for flush-

i g Wh th i li it d t f t it i

Such flows are highly abrasive and ex

lining will normally be required to

d g t th t t H it i i

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ing. Where there is a limited amount of water it is

better to use a high discharge for a short period of 

time than a low discharge for a long period of time.

This increases the amount of sediment that is re-

moved.

Areas of the world best suited to reservoir

flushing

It is not possible to define precisely which specific

areas of the world will provide conditions for suc-

cessful flushing. In reality there is a spectrum of conditions ranging from those sites where conditions

are ideal to those sites which are quite unsuited to

sediment flushing.

Given the foregoing, the requirements for suc-

cessful flushing are most likely to be met in the fol-

lowing locations:

Parts of Central America extending into SouthAmerica

Areas in North and South America where the riv-

ers are fed by the Rockies and the Andes

Parts of Central Africa from the Ivory Coast in

the west to Sudan in the east

Areas in Central Asia where the rivers are fed by

the Himalayas including Pakistan, India and

Nepal

Parts of Asia including Cambodia, Vietnam and

Thailand.

Design Implications for Flushing Facilities forNew and Existing Reservoirs

The requirement to establish riverine conditions in

a reservoir for successful flushing results in construc-tion of low-level outlets that are often very large.

 Where flushing is being investigated as an option

for managing sediments in an existing dam this poses

particular problems and will require specialist in-

damage to the structures. Hence it is im

the site allow for construction of relati

flushing facilities, either orifices withi

self or relatively short tunnels or cha

dissipation works will normally be re

downstream side and it is an advanta

cilities can be shared with other outlet

head spillways or irrigation outlets. I

have the flushing facilities discharge

stream channel well away from powe

lets as any local deposition of sedimenttailwater levels and reduce power out

The reservoir itself requires a deta

establish its topography. This is nee

whether the reservoir basin is a suita

sediment flushing and also to provide

detailed modeling of the sedimenta

within the reservoir.

Hydrological investigations

As noted above, there are certain req

successful sediment flushing related t

of water available and its annual and

ability. Hence inflows to the reservo

established with confidence. This inv

quisition of historical records of rive

back at least 30 years and preferably lo

of river flows can often be extended fu

time by considering local rainfall record

go back 100 years or more and under

ment modeling to convert rainfall int

The rate of sediment transport is r

discharge through a power function. Se

port rates are therefore highly sensitiv

in river flows. Mean values of inflow

equate to estimate sedimentation ratesthe time step the better the predictions

ever, for most situations a daily time s

adequate.

The ideal situation for sediment f

A S S E S S I N G F E A S I B I L I T Y O F F L U S H I N G

This requires measurements over many years to es-

tablish the results with confidence. There are vari-

ous approaches to this task Most commonly

long-term simulations, decades

or days. They have reached relia

permit them to be used “cold”

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ous approaches to this task. Most commonly

sediment transport is measured at a gauging station

not too far upstream of the reservoir and a relation-

ship between flow rate and sediment transport rate

is established. The long hydrological record is then

used to compute the total amount of sediment pass-

ing the gauging station by integrating over the pe-

riod of the record. There are some dangers in doing

this because there is no unique relationship between

flow rate and sediment transport rate for fine cohe-

sive sediments, the quantities of sediment being de-termined by the amount being washed off the

catchment, not the capability of the river to trans-

port them. Bed load is difficult to measure and is

often estimated as 10 percent of the total sediment

load. An alternative approach is to calculate the bed

load using established predictive techniques.

In the case of existing reservoirs, information

about the amount of sediments entering the reser-voir can be augmented by surveys of the amount

and nature of the material settling within the reser-

voir. This can be undertaken using bathymetric sur-

veys and borehole samples taken from the sediments.

Care is required, however, to allow for the amount

of mainly fine material that passes through the res-

ervoir without deposition.

Bed material sampling should be undertaken in

the reservoir and in the rivers that feed the reser-

voir. A sound knowledge of the nature of these sedi-

ments, including their size and specific gravity, is

an essential requirement to provide inputs for nu-

merical models that simulate sediment movement.

Hydraulic modeling

Sophisticated numerical (computer) modeling of the

way sediment is likely to behave within the reser-voir and the amount and nature of the sediment that

will be passed to the downstream reach is the cor-

nerstone of any detailed evaluation of flushing fa-

cilities One dimensional models with quasi

permit them to be used cold

that are only at the investigative

on existing reservoirs they have

of measured sedimentation data fo

poses.

Computer simulations of res

representative, long-term sequen

sediment inflows to the reservoi

capable of looking at the effect

aspects that affect reservoir susta

ods of up to 50 or 60 years, inclu

Measures to reduce the amoun

tering reservoirs such as catch

or upstream storage.

Measures to manage sediment

such as variations in the ope

for the reservoir. Rules that p

the reservoir annually promotement towards the dam. Rules

water levels ensure storage o

upstream end of the reservo

tend reservoir life albeit with

duced water yield.

Measures to evacuate sedime

voir including dredging and s

Engineering and costs

The design of the civil works i

options for helping to sustain reser

to be estimated so that the best sol

System simulation modeling

System simulation modeling is re

the conflicting demands of hydro

irrigation and other requirementto assess the impacts of the vario

ating strategies. The simulation m

to replicate the outputs of water a

range of operating strategies so th

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Introduction

This annex provides an expanded discussion of the

environmental considerations outlined in the main

text. While the safeguards approach presented there

is an important step, a more careful consideration

of environmental costs is necessary to determine the

true costs of alternative sediment management strat-

egies.

The world’s ecosystems are an asset that, if prop-

erly managed, yields a flow of vital services. Unfor-tunately, relative to other forms of capital, ecosystems

are poorly understood, rarely monitored and many

are undergoing rapid degradation and depletion.

More often than not, the importance of ecosystem

services is widely recognized and appreciated only

upon their loss.

 Worldwide, ecosystems are being protected or

restored to control floods, filter water, enhance soilfertility, mitigate climatic extremes and provide for

human enjoyment. These developments all involve

putting a “price tag” on nature. Individuals and so-

cieties already assess the value of nature implicitly

in their collective decision making, often consider-

ing ecosystem services as “free.” Until recently, such

an approach was generally acceptable, because gen-

erally speaking ecosystem capital was abundant andthe impacts of economic activity were minimal.

However, as ecosystem capital becomes increasingly

scarce, it is critical to understand both how to value

ecosystems and the limits of such valuations.

bl h d l h d f

of services and in the time fram

vices are amenable to repair. Yet

poorly known and are likely to re

systems typically respond to pert

linear fashion. Putting theory

require locally based information

There are three fundamental

making. The first step, identificat

is probably the most important a

most underrated. In this decisio

RESCON Model provides the firsis of the model will provide a se

natives for sediment managemen

requires that all impacts be identi

for each alternative; everything fro

for labor, capital and other input

physical and social impacts. Rar

knowledge exist to make precise

important to try to quantify uncrisks of proceeding. This annex

view of the impact parameters, th

should be considered in determ

mental cost of each of the feasibl

erated by the RESCON Model. T

step, valuation, translates the con

taining the status quo and optin

tive into comparable units of iwellbeing, now and in the futu

measuring unit is typically moneta

backs associated with most ways

and coupled with the functional l

l

ANNEX E: ENVIRONMENTAL CONSIDERATIONS

T H E R E S C O N A P P R O A C H

sion making, not a solution. As a result the annex

provides a discussion of the factors that should be

considered in the decision making process without

impacts cannot be adequately m

project will be prohibited from pro

analysis should be conducted for

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considered in the decision making process without

proposing any weighting of factors or specific valu-

ation process. These considerations in valuation canthen be placed in a context within the conceptual

decision making flow model described below. This

suggested decision making process implicitly suggests

that environmental costs be added to the costs of fea-

sible sediment management strategies, in order to

determine a true cost for sediment management.

It must be remembered that each application of 

this analysis will be unique, because the flow of eco-system services is site-specific.

Description of the Decision making Process

Step 1.

Run the RESCON Model. Output of the RESCON

Model will provide feasible engineering alterna-

tives for sediment management.Go to Step 2

Step 2.

Determine the environmental impacts (tempo-

rary and/or permanent loss of ecosystem services).

This will require a site-specific analysis. This

annex provides an overview of possible consid-

erations.

Go to Step 3

Step 3.

Determine if there is an applicable regulatory

framework in which a decision will be made. In

many developed countries there is a complex

regulatory framework in which the project will

be evaluated. In some countries there are no ap-

propriate regulations. If a regulatory frameworkexists:

Go to Step 4.

If no regulatory frame exists:

analysis should be conducted for

tive, recognizing that the environm

rather than the engineering feasibilibe the primary determining factor

4-A.

If various alternatives are acceptabl

of the mitigations should be det

added to the cost of the sediment

alternatives to determine the econ

ferred alternative.

4-B .

If no alternatives are permitted, th

proposed dam is not sustainable.

No Regulatory Framework Exists:

Step 5 .There is no regulatory framework

termine the decision making.

The value of ecosystem services th

manently lost should be calculated

the value of interim loss of ecosys

The sum of these two factors will e

ronmental cost for each alternativ

added to the sediment manageme

tain total cost. Any ecosystem ben

exist should also be evaluated and

project benefits.

Step 6

If the total environmental cost is

economic benefit derived from th

then the project should go ahead. Ivironmental cost is more than the e

efit derived from the proposed pro

project should not go ahead.

E N V I R O N M E N TA L C O N S I D E R A T I O N S

and reaching stakeholder agreement on results, rep-

resents the real challenge.

as it enters the sea, resulting in th

of the delta. Deltas and estuaries

systems that support many habit

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Environmental Impacts to be Considered in aValuation Procedure

The following is a brief discussion of the environ-

mental impacts that should be considered when at-

tempting to evaluate the environmental cost of any

sediment management alternative. The list cannot

be regarded as exhaustive, because the number of 

potential variables is enormous. It is also importantto remember that all listed parameters may not ap-

ply to each dam, or even each sediment manage-

ment alternative at a specific dam.

The environmental variables discussed here are

in relation to sediment management only. They are

not intended to provide a comprehensive evaluation

of whether a new dam should be built, except to the

extent that if sediment management cannot be costeffective because of the environmental cost, then

implementation should be reconsidered.

In order to evaluate the benefits/costs of sedi-

ment management it is necessary to examine the

overall impacts of dams and then evaluate how sedi-

ment management would yield positive or negative

value to the system.

Geomorphology and Turbidity

Reservoirs act as a sediment trap, holding back sedi-

ments, especially gravel and cobbles. The river down-

stream of the dam, deprived of its sediment load,

tends to erode the downstream channel and banks.

This can result in the undermining of bridges and

other riverbank structures. Within nine years of the

impoundment of Hoover Dam Reservoir in the

United States, the riverbed below the dam had beenlowered by more than four meters. River deepening

will also lower the groundwater table along the river,

threatening native vegetation and requiring the irri-

gation of agricultural products where it had been

y pp y

marshes) and species and therefo

protected.However, the decommissioni

implementation of a sediment ma

which passes sediments downstr

essarily improve the geomorpholo

downstream; detailed studies by

required.

Hydrological EffectsReservoirs change the flow patte

fecting their seasonal variations.

impacts depends on the size of th

parison with the annual inflows

eration of the dam, among ot

estuaries are particularly rich e

depend on the volume and timin

freshwater. It has been estimatedthe world’s fish catch comes from t

The alteration of flows reaching

of upstream consumptive water u

to the decline of sea fisheries in t

the Black and Caspian Seas, Cal

cisco Bay, the eastern Mediterra

Overall hydrological changes ca

stream riverine habitats. Detaile

data are lacking for most dams, b

the habitat alterations caused by

pear to have been severe. The red

ter flows to the mouth of the rive

saltwater intrusion, a problem i

River Delta of California, United

Flood Patterns

The impounding of water by reseflood peaks. Riverine and floodpl

closely adapted to a river’s flood

tive plants and animals depend o

reproduction hatching migratio

T H E R E S C O N A P P R O A C H

systems. In the West Fork of the San Gabriel River

system in southern California, United States, flood-

ing removes riparian trees and opens the canopy in

the resultant effects on hatching suc

vival etc. have been most completel

salmonids. However, most of these st

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patches. This improves the habitat for an endemic

sucker, which feeds on the epilithic diatoms thatflourish under the open patches in the canopy. The

canopy, however, keeps summer water temperatures

down for a sympatric trout. The alterations in river

hydrograph and the temperature of releases have

significant effects on the fauna. Since the Waitaki

River in New Zealand was dammed, the river has

become excellent habitat for the exotic Chinook

salmon, while the black stilt (bird) has become soendangered that fewer than 100 individuals remain,

largely as a result of patterns of sandbar formation

and stabilization. A similar pattern has been seen in

the Colorado River of the southwestern United States

where dam releases of cold clear water have pro-

duced an excellent non-native trophy trout fishery

at the expense of the native big river fish of the

Colorado River, all of which are now listed as en-dangered.

The floodplain itself is also affected. Studies on

the floodplain of the Pongolo River in South Africa

have shown a reduction in forest species after it was

dammed. Forests along Kenya’s Tana River appear

to be slowly dying out because of the reduction in

high floods due to a series of dams. The eucalyptus

forests of the Murray floodplain in Australia depend

on periodic flooding for germination, which has been

curtailed by the water impoundment.

The Kainji Dam on the Niger River is reported

to have adversely affected hundreds of thousands of 

people by reducing yam production and fisheries.

Also, former wetlands that had been seasonally in-

undated no longer provided essential grazing for live-

stock at the end of the dry season or water for flood

recession cultivation of rice and other crops.

Environmental considerations of flushing

only single factor analyses. Even when

tors such as dissolved oxygen, flow velgravel, fine sediment size/quantity, etc

they are treated independently and pr

tionships are developed only for singl

clear from the results of these studies

in-gravel incubation environments are

tems, which are simultaneously affec

factors. Fu-Chun Wu, 2000, attempte

three quantitative relationships in ordembryo survival as a function of sedi

tion. His model integrates variations

permeability with sediment depositi

velocity with substrate permeability

survival rate with apparent velocity.

indicate that embryo survival is mos

fine sediment-gravel size ratio. Wu th

model to analyze the timing of flushinresults were not tested experimentally

fied and they do not address factors

critical, such as dissolved oxygen, pH,

interspecies variation and other temp

tial variables.

Flushing Flow Prescriptions

It is recommended that Wu’s relations

timing of the flushing flows and sur

used as a guideline for determining

flushing flows. Among Wu’s assumptio

sonally high periods of runoff are freq

lated with spawning times, so that spaw

affected by sediment deposition as a

seasonally high runoff (releases of se

reservoirs may follow a similar patter

ally, it is suggested that one managema controlled stream is to allow sedime

tion and then flush the sediments peri

concept can be extended to sediment

in reservoirs Because almost any sedim

E N V I R O N M E N TA L C O N S I D E R A T I O N S

in question. The next value to consider is the mag-

nitude of the flushing flow; again data from indi-

vidual rivers are best but general guidelines are

Environmental Valuation

Some of the potential ecosystem

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available. Parker and Klingman (1982) suggest that

fine sediments can be removed from the gravels whenthe flushing flows are sufficient to break up the ar-

mor layer. Such a method would be an alternative

when there are sufficient gravels, but if sufficient

gravels are not available, such a flushing flow could

result in armoring of the stream with material too

large for spawning and could scour any eggs/larvae

currently in the substrate.

The above only provides initial guidelines thatmay require adjustment depending on the actual

stream parameters and target species. In order to

accurately determine the needs of a specific river,

natural flows should be studied, but in the absence

of actual stream data, the above guidelines can be

applied, then modified as necessary based on col-

lection of data documenting the results of the gen-

eralized flushing flow prescription.

General Applicability

The above recommendations are based on studies

of salmonids. Salmonids are a widely distributed

Boreal species. Their range has been significantly

expanded due to introductions in both the north-

ern and southern hemispheres. They frequently pro-

vide important commercial and/or recreational

fisheries throughout their distribution. The recom-

mended flow prescriptions should be generally ap-

plicable. Flushing flows are by definition,

predetermined discharges for a specific duration de-

signed to remove fine sediments from river gravels

(Reiser et al., 1989). Therefore, the above generali-

zations should be of use as general guidelines when-

ever the purpose is to remove fines from potential

spawning gravels (some tropical species are alsogravel spawners, i.e., some cichlids), as long as the

limitations of the guidelines are recognized and lo-

cal measurements are collected to refine the initial

generalizations

able, while others are not. Measu

productivity of floodplain agricutilizer, reduction or increase in f

are readily quantifiable. Biodivers

of ecosystem integrity, on the oth

ally impossible to quantify. The

losses of subsistence activities suc

eries is also difficult to quantify.

simply account for the economic

while neglecting to account for ththe loss of a particular way of life

community as a whole.

In order to go beyond the sa

presented in Chapter 4, it is nec

split valuations into two categor

that involve the permanent loss

ecosystem service and second ar

there is only an interim loss of eValuation of cases that involve a

reduction may be based on the c

of the lost services. Permanently

sometimes be “replaced” by sim

example, at Morris Dam (San Gab

nia, USA), sluicing has been used

voir sedimentation but has caus

destruction of downstream ecosy

result, the project was mitigated

sition of similar habitat on anot

this was done in the United State

regulatory framework, the efficac

was evaluated within that framew

proponent had to demonstrate th

habitat supplied the same ecosys

one destroyed. Replacement w

purchase or donation of land is diRestoration costs are also quanti

volve the cost of restoration alon

the interim loss of services.

Valuations of interim service

T H E R E S C O N A P P R O A C H

for each year during the recovery period, the dis-

counted effective fisheries loss could be calculated.

The total interim loss is therefore the sum of the

l d d ff f h l A

ment in this scenario. This scenario a

ral recovery without restoration. This v

cedure has been borrowed from habita

l h h l d

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annual discounted effective fisheries losses. A very

simple example is shown in the table below. In thisexample there is a 50 percent loss of fisheries catch

due to sediment management, but the system recov-

ers in a linear fashion in a period of four years. The

baseline catch is assumed to be 100 tons.

The monetary value of 97.9 tons of fish repre-

sents an environmental cost of sediment manage-

analysis, which is commonly used to v

of natural resource damages.In the case of biodiversity loss or oth

tifiable impacts, the valuation proced

the very least involve an enumeration o

to be considered in the decision maki

TABLE E.1

EXAMPLE OF USING DISCOUNTING TECHNIQUES TO QUANTIFY ENVIRONMENTAL LOSSES

Effective Fisheries Discount Factor Discounted EffectYear % Service Loss Loss (in tons) (3% discount rate) Loss (to

2001 50.0 50.0 1.00 50.0

2002 33.3 33.3 0.97 32.3

2003 16.6 16.6 0.94 15.62004 0.0 0.0 0.91 0.0

Total Discounted Effective Fisheries Loss 97.9

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One of the inputs necessary for the RESCON analy-

sis is the value of the water that is stored in the res-

ervoir. While this parameter has great implicationsfor optimal management of the reservoir, it is usu-

ally unavailable to the decision maker.

There exist several sources for calculation of the

value of water in various uses, including Gibbons

(1986), Young (1996 and 2003). However, quite

extensive preparatory work is needed in order to

estimate the value of water using the procedures

suggested in these sources.A range of water prices in various sectors and

uses could also be used as a reference. Available

sources include: Dinar and Sub

Ahmad (2000), OECD (1998a)

OECD (1999), Jones (2000) and S(1999), Dinar (2000).

A compilation of observed p

countries and sectors is provide

below. The prices are expressed in

so they should be easy to use and

be emphasized that the values in

necessarily represent the true wor

based on water prices that havevarious countries. Therefore, app

caution should be exercised when m

numbers.

ANNEX F: WATER PRICING

TABLE F.1

RANGES OF WATER PRICES FOR VARIOUS SECTORS AND COUNTRIES

(1997 US$)

Agriculture Domestic In

Fixed Variable Fixed Variable Fixed

(per hectare (per household (per plantper year (per cubic per year (per cubic per year

Country or season) meter) or month) meter) or month)

Algeria 3.79–7.59 0.019–0.022 0.057–0.27

Australia 0.75–2.27 0.0195 9-162 0.23–0.54

Austria 0.36–0.98 0.85

Belgium 2.06–2.47

Botswana 0.28–1.48

Brazil 3.50 0.0042–0.032 0.40

T H E R E S C O N A P P R O A C H

TABLE F.1

RANGES OF WATER PRICES FOR VARIOUS SECTORS AND COUNTRIES (continued)

(1997 US$)

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Agriculture Domestic IndustrFixed Variable Fixed Variable Fixed

(per hectare (per household (per plantper year (per cubic per year (per cubic per year

Country or season) meter) or month) meter) or month)

Greece 92–210 0.021–0.082 1.14

Hungary 0.82

India 0.164–27.47 0.824 0.0095–0.082 5.49 0

Israel 0.16–0.26 0.36

Italy 20.98–78.16 0.14–0.82

Japan 246 1.56

Jordan 0.01–0.04 0.27–1.03

Lebanon 8.71

Luxembourg 1.01

Madagascar 6.25–11.25 0.075–0.25 0.392

0.325–1.25

0.9–1.75

Mexico 33-60

Namibia 53.14 0.0038–0.028 1.54–4.28 0.22–0.45

0.33–1.38

Netherlands 3.16

New Zealand 6.77–16.63 16–164 0.31–0.69

Pakistan 1.49–5.80 0.25–1.63 0.06–0.10

Palestinian 0.33Authority (Gaza)

Palestinian 0.79–1.12

Authority (WB)

Poland

Portugal 0.0095–0.0193 4.46–1937 0.1526–0.5293 8.86–2,705

Saudi Arabia 0.04–1.07

South Korea 0.27

Spain 0.96–164.48 0.0001–0.028 0.0004–0.0046 0Sudan 4.72–11.22 1.67–3.33 0.08–0.10 1.67–3.33

Switzerland 0.33–1.96 1.29

Syria 50.00 3.21 0.11–0.53

Taiwan 23 30 213 64 0 25 0 42

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Introduction

GeneralThe Masinga Dam created the largest storage and

regulatory structure on the Tana River for regulat-

ing flows for four downstream hydropower dams. It

was designed on the basis of annual sediment input

of 3 million tons/yr and commissioned in 1981. By

1988, the Masinga Reservoir was actually receiving

10 million tons of sediment per year according to a

reservoir survey conducted during that year.The City of Nairobi is concerned about loss of 

storage due to sedimentation in its reservoirs and

negative impact on efficiency of their Mwagu Intake,

also as a result of sedimentation.

The Athi-Galana-Sabaki River sediment dis-

charges into the Indian Ocean have increased from

an estimate of about 50,000 tons/yr (0.7 t/km2 /yr)

in the late 1950s to an estimate of 8,400,000 t/yr(120 t/km2 /yr) in 1992 (JICA, 1992), a 170 fold in-

crease.

On the same river, the World Bank financed the

Mombassa Water supply intake at Baricho. This water

supply project was commissioned in 1982, but be-

cause of siltation problems and high turbidities

(about 6,000 NTUs13 ) and the associated extremely

high operations and maintenance costs (tripled co-

agulant doses at the treatment plants, daily manual

de-silting of the intakes and replacement of pump

bearings every two weeks because of the abrasive

action of the sediments), the entire scheme was aban-

d d b b l f

Deforestation: Impacts on Water a

Kenyan forests play an importan

a sustainable and reliable water suprivers in the country originate in

have always been considered to b

ponents of water supply in Kenya

including the forests on the Mau

Kenya, Aberdares Mountains, M

Cherengani, have been fondly nic

ter Towers.”

There is an extensive literaturdeforestation and, to a lesser exte

on runoff and river flows (Bruijn

estation has a number of hydrolog

ing decreased canopy interce

(usually) decreased transpiration

ment vegetation, (usually) incr

from the exposed soil surface, d

tration because of changes in soicreased velocity of runoff after r

litter and roughness. In addition

the trees intercept mist and this s

is lost after logging. The “mist

amounts to between 5-20 percen

tion (Bruijnzeel and Proctor 19

evidence that extensive areas of

convective currents that increase

but the size of this effect is diffic

Some of these effects increase

reduce it. There is strong eviden

ducted, paired catchment studie

f f l ff

ANNEX G: COUNTRY REPORT – KENYA

T H E R E S C O N A P P R O A C H

tors such as annual rainfall, soil characteristics, type

of replacement vegetation (Zhang, et al, 2001). Flows

following moderate to large storms also increase in

size and flashiness because of the quicker runoff when

groundwater in the region rather than f

ance of forests  per se.

In addition to the impact on the a

water and the magnitude of floods, def

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size and flashiness because of the quicker runoff when

the forest is replaced with crops and grasses. How-ever, the vegetation cover (forest, crop or grass) has

very little effect on runoff from very large storms,

either because the ground rapidly becomes saturated

or the precipitation is so intense that it cannot infil-

trate into the ground quickly enough.

The effect of deforestation on flows during non-

rain periods, or baseflows, is less clear cut. It de-

pends on factors such as the vegetation cover thatreplaces the trees, the quality of the land manage-

ment and the aquifer structure. For most replace-

ment vegetation, the decrease in evapotranspiration

is the dominant effect particularly when annual crops

(such as maize) and grasses replace the forest. Thus,

more water accumulates in the soil and baseflows

increase after deforestation. There are exceptions to

this generalization, such as when the “mist harvest-ing” effect is lost in cloud forests, when the infiltra-

tion is severely reduced and when deep-rooted

perennial plants (e.g., mature tea plantations) replace

the trees. In these cases, there is experimental evi-

dence that baseflows will remain the same or even

decrease after deforestation.

The clearance of forest in the “Kenyan Water

Towers,” below the level of cloud forest, is most likely

to result in increases in both storm flows andbaseflows, as seen at Mbeya, as long as the soils re-

tain good infiltration and there is no widespread use

of surface and groundwater. Flows are likely to de-

crease if cloud forest is cleared.

However, the reality is that, when forest is cleared

for gardens there are many other hydrological ef-

fects apart from just those from the vegetation re-

moval. The density of settlement is such thatsignificant groundwater is abstracted, surface run-

off is intercepted in pans, and areas such as paths

and around houses become heavily compacted, al-

though cropped areas retain good infiltration char-

water and the magnitude of floods, def

also result in increased erosion and higloads in rivers. As the sediment that i

by rivers deposits in reservoirs behi

storage capacity of these facilities red

quires building additional and larger

ties to ensure the reliability of water s

Reservoir Survey Methods

A Starlink Invicta 210S DGPS receiver

the Omnistar Satellites was used to

locations of the depth measurements (

latitude) throughout the surveys. The

duct differential calculations that impr

racy of the longitude and latitude r

accuracy that can be obtained with the ellites is within one meter, whereas

without the use of the same provides a

plus or minus three meters. Using the

ellites in Kenya was the most cost eff

benefit from Differential GPS (DGPS

tion of the locations of depth measure

tude and latitude) with the DGPS is

be significantly more accurate than an

ous surveys.A Garmin GPSmap 168 Sounder w

20o Transducer was used to determin

to the reservoir bottom throughout th

depth soundings were correlated with

ments at the beginning and end of su

The manual depth measurement an

sounder depth sounding correlated ver

a few centimeters.The survey was analyzed and bath

produced to calculate reservoir volum

tion/storage curves.

C O U N T R Y R E P O R T – K E N Y A

Given the field conditions under which the sur-

vey was conducted and the urgency to collect data

for this project a limitation was introduced. Three

of the four reservoirs that were surveyed were not

that has occurred over the last 5

cates that the average sediment yi

ment upstream of Ruiru Dam is on

km2 /yr.

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y

full. The survey data that were collected had, there-fore, to be enhanced.

Ruiru Dam was the only facility with a full reser-

voir, allowing the survey data to be directly analyzed

for determination of the total reservoir capacity.

Topographic maps for the other dams were obtained

from the owners and the full supply level was digi-

tized from these maps for incorporation into the

survey database.The map for Ndakaini Dam (also known as Thika

Dam) was shifted and rotated from the actual coor-

dinate system making application of this informa-

tion difficult. The topographic maps for Masinga Dam

had a slight, inconsistent distortion at some loca-

tions. Coordinates were converted where possible.

The fact that the Masinga Reservoir was not full

furthermore resulted in some of the deposited sedi-

ment in the upstream reaches of the reservoir not

being incorporated into the survey. These sediments

were located above the water surface elevation that

existed when the reservoir was surveyed.

The map for Sasumua Dam is based on a local

coordinate system that was not readily convertible

to UTM15  coordinates. Furthermore, the reservoir

of this dam contains extensive borrow pits with un-

usual (non-natural) shapes. The vertical cliffs of theborrow pits make extrapolation of the results less

reliable. Sasumua Reservoir appears to have experi-

enced significant siltation, which caused the boat to

get stuck a number of times, jeopardizing the accu-

racy of the data collection. These difficult conditions

were exacerbated by problems with navigation and

adverse, cold and windy atmospheric conditions. The

survey data for Sasumua Dam and Reservoir were of poor quality and could not be analyzed.

Results

y

Ndakaini Dam (Thika Dam)

Ndakaini Dam (also known as T

cently constructed. It is located o

and has a catchment area of 71 k

plies water to the City of Nairo

original capacity was 70 Mcm. T

ecuted when the water surface el

ervoir ranged between 2,036.01mThe original capacity of the rese

tion was 56 Mcm. The survey

current reservoir storage capacit

is still 56 Mcm, which indicates t

up to this elevation is negligible

tively new and if any storage loss

tion occurred, it is likely to be very

deposits most probably occurring

tion than what the dam was surv

Thika was the first reservoir

during this mission and the resolu

was used is very high. Approxim

vey elevations of the reservoir ba

to determine the reservoir capac

these readings is likely to be signif

that of any other survey that was

The original storage/elevation Reservoir is still valid and a new

veloped.

Masinga Dam

Masinga Dam, located on the Ta

missioned in 1981, has a catchm

km2 and regulates water for hydro

in the Seven Cascades System. Thnal capacity was estimated as 1,5

that was conducted in 1988 found

has lost 5.57 percent of its storag

was equivalent to 87 2 Mcm This

T H E R E S C O N A P P R O A C H

The 2001 survey indicates a total volume of 

1,100 Mcm giving an average annual loss of 23 Mcm/ 

year corresponding to a catchment yield of 4,000 t/ 

km2 /yr. This is unrealistically high.

dam was raised over the period 1965

creasing the total capacity to 13.25 M

The survey data that were collecte

Dam and Reservoir proved to be unusa

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y y g

Further investigations of the 1988 survey and theoriginal pre-impoundment height capacity curves

indicated that these are likely to be erroneous. There-

fore the original and 1988 storage volumes are un-

known and it is not possible to determine the annual

average sedimentation in the reservoir.

Sasumua Dam

Sasumua Dam, located on the Chania River and origi-nally commissioned in 1956 has a catchment area

of 12,800 ha and supplies water to the City of Nairobi.

The reservoir’s original capacity was 7.57 Mcm. The

p

cipal reason for this is that the weathon the day of the survey were bad, wi

and cold impacting the survey. Navig

ficult and the boat was stuck in depos

a number of times.

It was not possible to determine th

pacity of Sasumua Dam and Reservo

the poor quality of the data.

The team however observed that deposition in this reservoir is potentia

importance of this dam to the water sup

makes it advisable that another survey

TABLE G.1

ESTIMATED STORAGE LOSS IN SELECTED RESERVOIRS

Original Capacity Current Capacity Percentage StorageReservoir (106  m3) (106 m3) Loss (%) Date Co

Ruiru 2.98 2.496 16%

Thika 56 56 0%

Sasumua 7.57 to 13.25 Not determined Not determined Commissi

dam rai

Masinga 1,560a 1,100 29%a

(a) The original height-capacity curve on which these figures are based has been called into question by this study.

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Introduction

Morocco is an arid country that relies heavily onwater supplied by surface water reservoirs. Dams are

built to form reservoirs that store floodwater for later

use. Floods generally occur on an irregular basis and

long periods of drought, spreading over several years,

are not uncommon. To ensure the reliability of wa-

ter supply, it is therefore important to conserve res-

ervoir storage space. Loss of storage space due to

sediment deposition in surface water reservoirs isinevitable and poses a significant problem to Mo-

rocco. The reservoirs behind the 97 dams currently

owned by the Kingdom of Morocco on average lose

65 million cubic meters of storage space per year,

which is equivalent to losing the average storage space

of one reservoir every two years. Implementation of 

technically and economically feasible reservoir sedi-

mentation management techniques can lead to thesustainable use of water resources and associated

infrastructure.

The RESCON approach wa

Morocco in order to identify optim

agement strategies on a selection

Objective

The study was undertaken in Ma

ernment of Morocco selected 10 d

for analysis using the RESCON

tive was to identify the optimal ment techniques that are both

economically feasible and to dem

RESCON to the Government of M

its potential value in developing

support sustainable management

and water resource infrastructure

Reservoirs Analyzed

The ten reservoirs that were sele

are shown in Table H.1. The per

ANNEX H: COUNTRY REPORT – MOROCCO

TABLE H.1.

LIST OF RESERVOIRS ANALYSED

Reservoir Original Capacity (million m3) Current Capacity (mil

Abdel Karim El Khattabi 11.3 8.9

Bin El Quidane 1,507.5 1,253.4

T H E R E S C O N A P P R O A C H

that was used in the RESCON analysis, for each of 

the dams, is presented in Table H.4

The selected dams range from relatively small,

with a reservoir capacity of 5.6 million m3, to large,

gies, showing the first, second and thi

each facility.

A sensitivity analysis was conducted

ing cost, using the dredging cost pro

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with a reservoir capacity of 1.5 billion m3. The tablealso shows that the storage loss in some of these

reservoirs is significant.

The Timi N’Outine Dam and Reservoir is used

as a diversion structure downstream of Moulay

Youssef. Because of its use and location, the process

of sedimentation and determination of its economic

value is complex. It has therefore been omitted from

the analysis at this point in time.

Results

A summary of the results of the RESCON analysis is

provided in Table H.2. It contains a summary of the

optimal reservoir conservation management strate-

roccan engineers and that calculaRESCON program. This analysis was

to determine how sensitive the result

dredging cost. The results in the table

recommended optimal managem

changes, depending on the dredging

using the default dredging costs calc

RESCON program (which are higher t

m3

; see Table H.3 for values), the opticonservation management approach s

ing for three of the reservoirs.

Interesting results are shown for

Oued El Makhazin, which indicate tha

TABLE H.2.

RESULTS OF STUDY

16 Where the user does not input a cost

model calculates a unit cost of dredging b

ternal algorithm.

Sustainable Run-of-River Non

Option Name Flushing Dredging HSRS Trucking HSRS No Action HSRS

Abdel Karim El Khatabi

Hassen I

Ibn Battouta

Mohammed V

Mouley Youssef

Sidi Driss

Bin El Ouidane

Timi N’Outine

Ennakhla

Qued El Makhazin

Abdel Karim El Khatabi

Hassen I

Ibn Battouta

Mohammed V

    D   r   e    d   g    i   n   g    C   o   s   t  =    U    S    $    2 .    5    0

    /   m    3

g   c   o   s   t

C O U N T R Y R E P O R T – M O R O C C O

I    f   c   o   m   p    l   e   t   e

s   m   o   s   t   p   r   o  -

    T    h   e   n   e   t

r   u   c    k    i   n   g   a   r   e

y .    F    l   u   s    h    i   n   g

   m   a   y   n   o   t    b   e

a   t   e   r .

s   e    d    i   m   e   n   t

i   n   m   o   r   e

o   c    k   e    d   a    f   t   e   r

e   q   u    i   r   e

d   n   o   a   c   t    i   o   n ,

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E    T    H    O    D    F    O    R    R    E    S

    E    R    V    O    I    R    C    O    N    S    E    R    V    A    T    I    O    N

    O   p   t    i   m   a    l    A   p   p   r   o   a   c    h   e   s

    L   o   n   g    T   e   r   m    C   a   p   a   c    i   t   y

    Y   e   a   r   s

    F   r   e   q   u   e   n   c   y   o    f

    N   o .   o    f

    M   e

   t    h   o    d

    1    0    6     m    3

    %

    t   o    L    T    C

    1   s   t    P    h   a   s   e 

    2   n    d    P    h   a   s   e

    E   q   u    i   p   m   e   n   t

    C   o   m   m   e   n   t

    D   r   e    d   g    i   n   g

    3 .    4

    3    0    %

    3    3

     3   y   e   a   r   s

    1   y   e   a   r

    1

    C   o

   n   s    i    d   e   r    i   n   g    “    f    l   u   s    h    i   n   g   r   e   a   c    h    ”   o   n    l   y .

    

   r   e   s   e   r   v   o    i   r    i   s   c   o   n   s    i    d   e   r   e    d ,    d   r   e    d   g    i   n   g    i   

    b   a

    b    l   y   a   p   p   r   o   p   r    i   a   t   e   t   e   c    h   n    i   q   u   e .

    N   o

    A   c   t    i   o   n

    0

    0    %

    1    4    0

     N    /    A

    N    /    A

    N    /    A

    D   r   e    d   g    i   n   g

    4 .    4

    1    0    %

    3    2

    3    2   y   e   a   r   s

    3   y   e   a   r   s

    1

    F    l   u

   s    h    i   n   g   n   o   t   t   e   c    h   n    i   c   a    l    l   y    f   e   a   s    i    b    l   e .

    b   e   n   e    f    i   t   o    f    d   r   e    d   g    i   n   g ,   n   o   a   c   t    i   o   n   a   n    d   t   r

   v   e   r   y   c    l   o   s   e .

    D   r   e

    d   g    i   n   g

    7    2 .    6

    1    0    %

    3    5

    1    0   y   e   a   r   s

    1   y   e   a   r

    3

f

    D   r   e    d   g    i   n   g

    1    9    7 .    2

    1    0    0    %

    1    8

    1    8   y   e   a   r   s

    5   y   e   a   r   s

    1

    B   e

   n   e    f    i   t   s   s    l    i   g    h   t    l   y    d    i    f    f   e   r   e   n   t .

    F    l   u

   s    h    i   n   g

    3 .    4

    4    7    %

    2

    2   y   e   a   r   s

    N    /    A

    D   r   e    d   g    i   n   g

    1 .    8

    2    0    %

    1    9

    2   y   e   a   r   s

    1   y   e   a   r

    1

   z    i   n

    N   o

    A   c   t    i   o   n

    0

    0    %

    3    2    4

    N    /    A

    N    /    A

    N    /    A

    F    l   u

   s    h    i   n   g

    4

    3    5    %

    3    0

    3    0   y   e   a   r   s

    2   y   e   a   r   s

    N    /    A

    C   o

   n   s    i    d   e   r    i   n   g    “    f    l   u   s    h    i   n   g   r   e   a   c    h    ”   o   n    l   y

   e   v   e   r   y   t   w   o   y   e   a   r   s    i   n   s   e   c   o   n    d   p    h   a   s   e

   p   o

   s   s    i    b    l   e    d   u   e   t   o    l   a   c    k   o    f   e   n   o   u   g    h   w   a

/   m    3    )

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    A   c   t    i   o   n

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    0    %

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    N    /    A

9 .    7    0    /   m    3    )

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    0

    0    %

    6    0    0

    N    /    A

    N    /    A

    N    /    A

    I   s    8    2 ,    0    0    0   m   e   t   r    i   c   t   o   n   s   p   e   r   y   e   a   r   o    f   s

    i   n    f

    l   o   w    i   n   t   o   t    h   e   r   e   s   e   r   v   o    i   r   c   o   r   r   e   c   t    ?

    F    l   u

   s    h    i   n   g

    2    9 .    8

    4    %

    3    7

    3    7   y   e   a   r   s

    2   y   e   a   r   s

    N    /    A

    F    l   u

   s    h    i   n   g   n   e   e    d   t   o    b   e    i   n   v   e   s   t    i   g   a   t   e    d    i

     d   e

   t   a    i    l    b   e   c   a   u   s   e   g   a   t   e   s   c   o   u    l    d    b   e    b    l   o

    3    7

   y   e   a   r   s ,   m   a    k    i   n   g    i   t    i   m   p   o   s   s    i    b    l   e .    R   e

    f   e   a

   s    i    b    i    l    i   t   y   s   t   u    d   y .

f

    N   o

    A   c   t    i   o   n

    B   e

   n   e    f    i   t   s    f   o   r    d   r   e    d   g    i   n   g ,   t   r   u   c    k    i   n   g   a   n    d

T H E R E S C O N A P P R O A C H

management solution is to allow the reservoirs to

fill with sediment over the long term and use the

head provided by the dam to generate run-of-river

hydroelectric power, having foregone the benefit of 

The table also shows the frequency

ing sediment operations for two pha

phase is the period prior to reaching

capacity and the second phase is the pe

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storage. This result is independent of the cost of dredging used.

The recommended solution for Moulay Youssef 

using a cost of dredging of US$2.50/m3 is to dredge

the annual inflow of sediments to achieve a sustain-

able solution. However, if RESCON is allowed to cal-

culate its own cost of dredging (US$4.02/m 3) the

results are balanced such that the economic value

of reservoir use is maximized to approximately thesame value, whether it is done by conserving reser-

voir storage by means of dredging or trucking, or

allowing the reservoir to silt up completely and us-

ing the head at the dam to generate run-of-river

power.

Table H.3 shows further detailed results, includ-

ing the estimated long-term capacity and more de-

tail pertaining to the frequency of executing sediment

management operations. Results are shown for the

two optional dredging cost estimates. The dollar value

per cubic meter in the first column of the second

part of the table is the cost of dredging calculated by

RESCON.

The table shows more detailed information per-

taining to what is estimated to be achievable in terms

of reservoir conservation. For example, in the case

of Sidi Driss it is estimated that the stable long-termcapacity would be on the order of 3.4 million m3,

which is 47 percent of the original storage capacity

and that the optimal sediment management tech-

nique is flushing. In order to maintain this capacity,

it is required to flush the reservoir every two years

to maximize the economic benefit.

long-term capacity has been reached. Tof implementing sediment manageme

during the first phase sometimes dif

frequency of implementation in the s

For example, Mohammed V reservoir i

once in the first phase (after 37 years) if

calculated cost for dredging is used,

flushed every 2 years in Phase 2 to main

term capacity. This frequency of operatithe long-term value of Mohamed V re

Recommendations

Preliminary discussions with Moroccan

the outcome of the study indicated th

of the RESCON analysis are in line wi

rience and understanding of the reserv

investigated. In order to maximize the

survey, a pre-feasibility study should b

to identify optimal sediment managem

for all 97 reservoirs in the country.

The pre-feasibility study should c

prioritizing the existing reservoirs and

of relative importance. Thereafter the re

be analyzed using the RESCON progroptimal management strategies for ea

ervoirs. This study will indicate which

ing reservoirs can potentially be m

sustainable manner and which ones s

to be used in a non-sustainable fashio

C O U N T R Y R E P O R T – M O R O C C O

    A   v   g .   a   n   n   u   a    l

   s   e    d    i   m   e   n   t

    i   n    f    l   o   w

    (   t   o   n   n   e   s    )

    2    1    7 ,    0

    0    0

    7

    2    3    5 ,    2

    0    0

    2 .    6

    5

    8    2 ,    0

    0    0

    1    2 .    8

    6    5    1 ,    0

    0    0

    3

    2    4    3 ,    0

    0    0

    0 .    1

    5

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L    Y    S    I    S

   a    l

    C   u   r   r   e   n   t

g   e

   s   t   o   r   a   g   e

    R   e   s   e   r   v   o    i   r

    R   e   s   e   r   v   o    i   r

    N   o

   r   m   a    l

    B   e    d

    F    l   u   s    h    i   n   g

    R   e   s

   e   r   v   o    i   r

    A   c   c   e

   p   t   a    b    l   e

    W   a   t   e   r

    S   e    d    i   m   e   n   t

m   e

   v   o    l   u   m   e

    b   o   t   t   o   m

   s    i    d   e

   w   a   t   e   r

    l   e   v   e    l

   w   a   t   e   r

    l   e   n   g   t    h

    M    A    R

    M    A    R

   p   r   o    b

   a    b    i    l    i   t   y

    T    (    0    C    )

    d   e   n   s    i   t   y

m    )

    (    M   c   m    )

   w    i    d   t    h    (   m    )

   s    l   o   p   e

    l   e   v   e    l    (   m    )

    (   m    )

    l   e   v   e    l    (   m    )

    (   m    )

    (    M    C   m    )

    C   v

   o    f    f   a

    i    l   u   r   e

    (   t   o   n   s    /   m    3    )

    8 .    8

    7

    6    0    0

    0 .    0

    5

    1

    4    0

    1    1    5

    1    3    0 .    0

    1 ,    6

    0    0

    4    8 .    2

    0 .    8

    0

 .    0    1

    1    8

    1 .    2

    0

5

    1 ,    2

    5    3 .    4

    1 ,    0

    0    0

    0 .    2

    8

    8

    1    0

    7    1    0

    2    0

 ,    0    0    0

    1 ,    0

    5    0

    0 .    5

    8

    0

 .    0    1

    1    2

    1 .    2

    0

    4 .    9

    2    5    0

    0 .    2

    1

    1    9

    0 .    6

    5

    1    5    0

    1    5    2 .    5

    2

    1 ,    8

    0    0

    5    5

    0 .    5

    6

    0

 .    0    1

    1    2

    1 .    2

    0

    2    4    5

    5    0    0

    0 .    4

    1

    9

    6    6

    8    6    2

    8    9    0 .    0

    6 ,    0

    0    0

    2    8    8 .    5

    0 .    5

    0

 .    0    1

    1    0

    1 .    3

    5

    3    3 .    9

    4

    6    0    0

    0 .    0

    6

    4    8

    2    4

    2    7 .    5

    1    1

 ,    2    7    5

    5    2 .    3

    0 .    8

    1

    0

 .    0    1

    1    0

    1 .    2

    0

5

    3    6    2 .    5

    5

    2 ,    3

    0    0

    0 .    1

    5

    2

    1    8

    1    7    0

    1    7    9

    1    0

 ,    5    0    0

    7    5    0

    0 .    5

    1

    0

 .    0    1

    2    0

    1 .    2

    0

2

    1    5    9 .    3

    5

    1 ,    2

    0    0

    0 .    1

    4

    8    7    7 .    5

    7    9    5

    7    9    7

    3 ,    0

    0    0

    2    8    7

    0 .    5

    0

 .    0    1

    1    2

    1 .    2

    0

    7    7    3

    1 ,    5

    5    0

    0 .    1

    0

    6

    1 .    5

    1    3

    2    3 .    1

    7

    3    5

 ,    0    0    0

    8    0    9

    0 .    6

    7

    0

 .    0    1

    1    2

    1 .    2

    0

9

    2 .    7

    5    5

    5    0

    0 .    2

    3

    6    4    3 .    5

    6    1    5

    6    3    0 .    8

    4 ,    0

    0    0

    1    2    5

    0 .    7

    5

    0

 .    0    1

    2    0

    1 .    3

    5

    2 .    4

    1    0    0

    0 .    0

    5

    7    9    3 .    5

    7    8    0

    7    8    1 .    4

    7    0

    5 .    6

    0 .    5

    0

 .    0    1

    1    0

    1 .    1

    0

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Introduction

BackgroundSri Lanka is dependent on its water storage reser-

voirs to supply the country with water for irriga-

tion, urban and industrial use and hydropower. The

reliability of water and power supply during the dry

season, when rainfall and resulting runoff in the rivers

are low, is dependent on the storage capacity of the

reservoirs.

Reduced reservoir storage capacities caused bysedimentation result in less reliable water and power

supply. This is particularly true of the reservoirs in

the upper Mahaweli basin, which make significant

contributions to the economy of the country. These

reservoirs also play an important role in managing

floods. Management of sediment in existing reser-

voirs can potentially lead to more economical solu-

tions that may also result in sustainable use of both

the water resources and the water resource infrastruc-

ture of the country.

The Mahaweli River Cascade (Figure I.1) con-

sists of several major dams that were constructed

between 1976 and 1991. These include: Kothmale,

Polgolla, Victoria, Randenigala, Rantambe and a weir

on the main Mahaweli River. These facilities pro-

vide approximately 45 percent of the country’s power

requirements. A post-evaluation study of the VictoriaProject that was carried out in 1987 showed that

110 to 940 tons of sediment per square kilometer of 

river basin flows in Mahaweli River annually. Re-

l f h d h d

due to sediment deposition in th

studies also revealed that Polgo

reached a regime condition. At pinto this reservoir spill to Victoria

downstream and it was also fou

amount of suspended silt passed

tunnel and turbines. Removal o

the reservoir has not been done

high cost.

A hydraulic flushing exercise

the Rantambe Reservoir, with theout the deposited sediment duri

was observed that 10-15 percen

was removed.

The objective of the RESCO

investigate the technical and econ

managing sediments in the reservo

basin and to identify the optimal

egies for ensuring sustainable us

Study Phasing

The study has been undertaken i

first mission was in March 2002

assisted the Mahaweli Authority o

in identifying a portfolio of dam

cascade (Figure I.1) for further

ment studies. Preliminary data w

MASL and a survey plan was sesedimentation estimation

Phase II consisted of techni

analysis using the RESCON mode

ANNEX I: COUNTRY REPORT – SRI LANKA

T H E R E S C O N A P P R O A C H

Overall Objectives

The overall objectives of the project

were to:

MAHAWELI RIVER CASCADE

THE MAHA

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Quantify the storage depletion

trends at system level by inte-

grating current knowledge with

measurements in the surveyed

reservoirs

Determine the economic and

engineering feasibility of man-

aging sediment in the reservoirsin the Mahaweli river basin

Conduct an early identification

of the environmental and social

issues relevant to managing

sediment in the reservoirs, to

be used for the preparation of 

terms of reference for the fea-

sibility studies

Identify and prioritize the op-

timal management strategies for

ensuring sustainable use of the

reservoirs, should sustainable

use be feasible; if marginally

feasible, propose alternatives

Prioritize the reservoirs, consid-

ering their vulnerability to sedi-

mentation, for subsequentexecution of feasibility studies

including catchment manage-

ment measures

Train Sri Lankan engineers in the use of the

RESCON approach and software and in modern

hydrographic survey techniques.

Estimated Reservoir Storage Loss

The Mahaweli Authority of Sri Lanka (MASL) se-

lected reservoirs to be surveyed based on the rela-

ported by the Omnistar Satellites to

locations of the depth measurements (

latitude) throughout the surveys. A Ga

168 Sounder with a 200 kHz, 8o Transd

to determine the distance to the resethroughout the surveys. The depth so

correlated with tape measurements at

of survey sessions. The manual depth

and the echo-sounder depth sounding c

Regulating reservoir for irrigation water to systemof Mahaweli, other ID systems and power generati

Diverts 875 mcm

water to system H

Storage reservoir for irrigation water to system Hof Mahaweli other ID systems and power generatio

Storage reservoir for irrigation water to systems Bof Mahaweli other ID systems and power generatio

Kothmale(176 mcm)(703m-msl

Storage reservoir for irrigation water to systems Bof Mahaweli other IDsystems and power generatio

MAHAWELI RIVER CASCADE

Minipe Anicut(116m-msl)

Polgollla(4.2 mcm)(441m-msl)

Victoria(721mcm)(438m-msl)

Randenigala(860mcm)253m-msl)

Rantambe(32mcm)(152m-msl)

diverts irrigation than 50,000 Ha.

C O U N T R Y R E P O R T – S R I L A N K A

obtained from the MASL and the full supply level

was digitized from these maps for incorporation into

the survey database. This is a difficult and inaccu-

rate means of supplementing bathymetric data and

results in an underestimation of reservoir sedimen

sediment inflow into downstream

increase, thereby affecting their o

ful life. When considering reserv

text, it is therefore necessary to d

strategies that will optimize the e

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results in an underestimation of reservoir sedimen-tation due to the inability to estimate the volume of 

sediments deposited above the reservoir level at the

time.

Reservoir survey data collected in Sri Lanka re-

quired reduction to create contour maps of the new

reservoir topography for each surveyed reservoir. The

depth soundings were used to calculate bed eleva-

tions by subtracting them from the water surfaceelevations on the day the reservoir was surveyed.

The survey data were analyzed to develop existing

conditions, bathymetric maps and calculate exist-

ing reservoir capacity. Original reservoir capacity was

also calculated by digitizing reservoir topography data

from the time of dam completion provided by MASL.

The difference between the two values gives the to-

tal loss to sedimentation to date.

At the time of publishing, Rantambe is the only

reservoir for which the sedimentation analysis has

been completed. The analysis for other reservoirs is

awaiting further information.

Rantambe’s estimated sedimentation rate is

339,342 m3 /year. The existing capacity of Rantambe

is estimated to be 6,687,450 m3 at the retention level

of 152 m, which is a 38 percent reduction in capac-

ity since reservoir impoundment in 1990.Estimates of storage loss for Kotmale, Polgolla,

Victoria and Randenigala Reservoirs in the Mahaweli

Cascade used as input to the RESCON model were

obtained from MASL or historically published docu-

ments (HR Wallingford, 1995). Due to the lower level

of accuracy of older bathymetric survey methods,

these numbers should be viewed as preliminary.

RESCON Modeling

General

strategies that will optimize the esustainability of the system as a

In order to apply the RESC

project, the software was modifie

erating rules for the system as a

for a single reservoir. In particula

incorporated the effects of dischar

the river downstream of a dam b

ing or hydrosuction. In the case assumed that the sediment wou

removed from the river system a

downstream to lower lying reserv

model automatically runs all poss

of reservoir management schem

impact that management scheme

ervoirs have on each other and

set of sediment management tech

tem as a whole will produce the

benefit.

The drawback of the cascade

run time is approximately 18 hou

computer. For five reservoirs, the

model runs the original RESCON

and tabulates results.

Input DataData were collected by MASL for th

input for all five reservoirs in the M

See Table I.1. The mean annual s

Rantambe has been estimated fro

dertaken by this study. The value

ervoirs are based on data provided

studies.

RESCON Model Results

The original RESCON model fo

T H E R E S C O N A P P R O A C H

TABLE I.1

RESCON PARAMETERS

Parameter Units Kotmale Polgolla Victoria Randenigala

Initial Storage (106 m3) 176 8 4 681 722 0 835 0

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mary of the project life of the five reservoirs that

were analyzed, for current conditions and when fea-sible reservoir sedimentation management strategies

are implemented. Without implementing any sedi-

ment management techniques Rantambe is identi-

fied as the reservoir with the shortest project life

(24 years) and Victoria as the reservoir with the long-

est project life (1 197 years).

The project lives of each of these reservoirs can

be extended to a greater or lesser extent if feasiblesediment management techniques are implemented.

The most significant result is for Rantambe, which

can be extended from 24 years to perpetuity. See Table

I 2

Implementation of pro-active sedim

is not required at Victoria and Kotmbecause their project lives are several h

each.

Using the preliminary results of

modeling and using engineering ju

knowledge of the reservoirs and sedim

ment techniques, the sediment manag

gies for each reservoir were prioritize

are given in Table I.3.

Rantambe Reservoir

Rantambe Reservoir is expected to silt

years) if no action is taken This mak

Initial Storage (10  m ) 176.8 4.681 722.0 835.0

Capacity

Existing Storage (106  m3) 170.1 2.558 713.1 768.8

Capacity

Representative (m) 340 118 108 50

reservoir bottom width

Representative 2 2 2 3

reservoir side slope

Normal Pool Elevation (m) 703.0 440.7 438.0 232.0

River bed elevation (m) 638.0 434.3 340.0 148.5

Flushing water (m) 645.0 434.3 352.0 170.0

elevation

Reservoir length (m) 10450 7644 24800 12500

MAR (106  m3) 871 1,838 1,571 2,085

Cv for MAR 0.14 0.15 0.28 0.25

Average annualinflow of sediments (tonnes) 522,105 878,483 728,163 5,404,898

Sediment type: 650, fine grained sediments, density = 1.2 t/m3

C O U N T R Y R E P O R T – S R I L A N K A

TABLE I.2

APPROXIMATE RESERVOIR LIFE

Approximate Number of Years until Reservoi

Reservoir No Removal Option Partial R

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the original and that flushing every three years pro-

vides a long-term capacity of 45 percent of original.

It is recommended that dredging, HSRS and flush-

ing be studied in further detail.

Polgolla Reservoir

Currently, the expected life of Polgolla Reservoir is

36 years if no sediment management is undertaken.

Flushing is known to be successful at Polgolla, be-

cause it is currently flushed when the barrage gates

are lifted to allow flood flows to pass. With this site

experience confirming the RESCON results, flush-

ing is considered the first choice for sediment man-

agement at Polgolla.Sand mining is also presently executed in the main

body of Polgolla Reservoir with apparent success in

keeping this area free of sediment. This site knowl-

edge along with RESCON results suggests that dredg-

ing should be considered as a se

priority, particularly at intake tow

Although RESCON shows HSR

economical solution, it is unlikel

feasible due to the long reservoir

It is recommended that flush

ing continue as currently practice

mental dredging at intake towe

either using conventional dredgi

Randenigala Reservoir

Randenigala Reservoir had the la

ity of all the reservoirs in the c

according to the data assumed inhad the highest sediment inflow

time compared to the other

Randenigala is predicted to have

Reservoir No Removal Option Partial R

Kotmale 427

Polgolla 36

Randenigala 177

Rantambe 24

Victoria 1 197

TABLE I.3

PRIORITISED SEDIMENT MANAGEMENT OPTIONS

Sustainable reservoir volume

a Partial removal occurs via HSRS that is potential ly capable of sustainable removal for Rantambe Reservoir according to R

ing its life in perpetuity.

T H E R E S C O N A P P R O A C H

life of about 177 years without any pro-active sedi-

ment management.

Examining the RESCON model prioritization,

sustainable dredging was chosen to produce the high-

est economic benefit, but six dredges would be re-i d h i fl i di d d Th

moval alternatives. The NPV dec

proximately 50 percent by changing

from 5 percent to 10 percent. The va

by approximately another 33 perc

ing the discount rate from 10 perc

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est eco o c be e t, but s d edges wou d be equired to meet the inflowing sediment demand. Thus,

dredging is not a feasible option (from a practical

and technical point of view). The second choice of 

the RESCON model is HSRS partial removal. How-

ever, Table I.2 shows that the increased life provided

by partial removal HSRS is negligible. HSRS, too, is

disregarded as a possible solution.

Flushing is the third highest economic alterna-tive chosen by the RESCON model. The model pre-

dicts that flushing every 16 years provides the

optimum economic return and will keep Randenigala

operational at a long-term capacity of 477.5 Mm3

(57 percent of original capacity). This option will

require construction of new low-level service gates

because existing service gates have inadequate ca-

pacity. An initial estimate for total gate length re-

quired is at least 55 m. This is very wide consideringthe width of the entire dam.

It is recommended that Randenigala Reservoir be

studied further for flushing potential in a feasibility

level study. It must be verified that flushing is tech-

nically feasible for sustaining a reasonable capacity

and a reasonable economic return. Localized dredg-

ing can be used at critical structures but dredging is

not capable of producing a sustainable system alone.

Sensitivity to Discount Rate

The main runs of the model were undertaken using

a discount rate of 10 percent and the sensitivity of 

the results to altering the discount rate to 5 percent

and 15 percent tested. The results show that:

The predicted life of each reservoir did not change

for the different values of discount rate.

Economic benefit generally decreases with in-

g t e d scou t ate o 0 pe ccent.

Sensitivity to Cost of Dredging

The unit cost for dredging used in

US$5/m3. This is considered to be

pre-feasibility level assumption whichcost of dredging and some costs of sto

at an offsite location. The raw results

show that at this unit cost, dredging is

economic option for every reservoir. I

unit cost to US$15/m3, dredging be

less favorable, only being chosen at

as most economic and at one reserv

most economic. In other words if th

posal of the dredged sediments is likestantial then dredging is unlikely to be

feasible.

Environmental and Social Impacts

Table I.4 lists anticipated environmen

impacts of sediment management on Cascade using the RESCON methodolo

were considered in this application inc

management will:

Require the reservoir to be emptied

long?

Affect water quality downstream o

Require off-site disposal of sedime

“No Removal” of sediment, with ei

tainable or run-of-river assumptions, w

environmental or social impacts prio

C O U N T R Y R E P O R T – S R I L A N K A

tion and sustainable strategies that use

HSRS will produce environmental results

similar to one another. The reason for this

is that HSRS is used in each of these op-

tional sediment management strategies. Iti t d th t th t ti f di a   t   e

   g   o   r   y

o    i   m

   p   a   c   t

o    i   m

   p   a   c   t

o   r    i   m   p   a   c   t

o   r    i   m   p   a   c   t

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g gis expected that the concentration of sedi-

ment discharged downstream of the dam

via HSRS can be controlled to produce

positive conditions for fish downstream of 

the dam. This will create minor permanent

changes to the existing ecosystem. Because

of these minor ecosystem changes, fisher-

ies species ratios may be altered, affecting

human uses. Other social aspects should

not be affected, so HSRS options receive

a rating of 8 or minor overall impact in

Table I.4.

 When dredging sediments are removed

to the river downstream of the dam, the

concentration of the sediment discharge

will determine whether this is a positive

or negative environmental affect. Table I.4assumes that this concentration can be

controlled to produce positive conditions

for fish downstream of the dam. This will

create minor permanent changes to the

existing ecosystem. Because of these mi-

nor ecosystem changes, fisheries species

ratios may be altered, affecting human uses.

Other social aspects should not be affected,so dredging also receives a rating of 8 or

minor overall impact in Table I.4.

Flushing received the highest impact

rating in Table I.4 at a value of 10 with

one 3, so it is considered a moderate im-

pact. During initial stages of flushing, sedi-

ment concentrations can be quite high

downstream of the dam, which will causetemporary impacts to natural habitats.

Fisheries will see impacts during the im-

mediate aftermath of flushing, thus impact-

ing human uses Indigenous peoples will S    A    F    E    G    U    A    R    D    R    A    T    I    N    G    S

    E   n   v    i   r   o   n   m   e   n   t   a    l    S   a    f   e   g   u   a   r    d   s    R   a   t    i   n   g    (    V   a    l   u   e    1   t   o

    4    )

    C   u   m   u    l   a   t    i   v   e

    N   a   t   u   r   a    l

    H   u   m   a   n

    C   u    l   t   u   r   a    l    I   n    d    i   g   e   n   o   u   s

    T   r   a   n   s    b   o   u   n    d   a   r   y

    S   a    f   e   g   u   a   r    d

T   e   c    h   n    i   q   u   e

    H   a    b    i   t   a   t   s

    U   s   e   s

    R   e   s   e   t   t    l   e   m   e   n   t

    A   s   s   e   t   s

    P   e   o   p    l   e   s

    I   m   p   a   c   t   s

    R   a   t    i   n   g

    C   a

    N    /    A

    1

    1

    1

    1

    1

    1

    6

    N   o

    N    /    A

    1

    1

    1

    1

    1

    1

    6

    N   o

    H    S    R    S

    2

    2

    1

    1

    1

    1

    8

    M    i   n   

    H    S    R    S

    2

    2

    1

    1

    1

    1

    8

    M    i   n   

T H E R E S C O N A P P R O A C H

Trucking is not a first management choice for

any of the reservoirs in the Mahaweli Cascade. Nev-

ertheless, its safeguard rating would be a moderate

impact (value of 10) due to temporary impacts to

natural habitats (including permanent off-site dis-posal) and indigenous peoples and significant im

In summary, Victoria and Kotmale

an adverse environmental impact in th

future. If local dredging is later used t

towers minor impacts are expected. R

Randenigala are expected to have minenvironmental impacts due to the use o

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posal) and indigenous peoples and significant im-

pacts to human uses of power generation while the

reservoir is empty for trucking. Trucking requires

that a reservoir be empty far longer than flushing.

Because the reservoirs on the Mahaweli River are

existing, the impact of sediment management is

minimized in terms of social and environmental

considerations. The RESCON results are used to

provide environmental impact expectations.

environmental impacts due to the use o

ing or HSRS. Polgolla and the river d

it are expected to experience moderate e

and social impacts due to flushing and

tional impact due to localized dredgin

considerations should be addressed in

environmental impact assessment tha

ried out at the feasibility level.

ANNEX J: SENSITIVITY ANALYSES

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Introduction

This annex provides the details of the sensitivity testsundertaken on the model and which are summarized

in Chapter 6.

General Sensitivity Testing

By selecting pre-existing geometries, the number of 

variables that is arbitrarily varied within the expectedrange of possibilities is reduced because relationships

for the various geometric parameters to the capac-

ity are fixed. The geometric param

according to the relationships tak

etry data available for each site. senting the geometric relationship

 J.1.

Once the geometric paramete

capacity were set for each reserv

rameters were varied to test mod

parameter was varied within va

physical reality. The parameters t

shown in Table J.2.

TABLE J.1

GEOMETRIC PARAMETERS

ParameterParameter Description Symbol

Original (initial) storage capacity

  of the servoir. So

Existing storage capacity

  of the reservoir. Se

Reservoir length at the normal

  pool elevation. L

Representative bottom width

  for the reservoir. Wbot

Minimum bed elevation just

upstream of dam EL

TABLE J.2

PHYSICAL PARAMETERS VARIED IN AD

GEOMETRY CHANGES

P a

Parameter Description S

Mean annual sediment

  inflow mass

Multiplier for reservoir and

  its sediment (Tsinghua

  University method)

Representative discharge

  passing through reservoir

  during flushing

Frequency of flushing events

T H E R E S C O N A P P R O A C H

Parameters that were assumed con

termined with available data and judg

reservoir are listed in Table J.3.

A few parameters can be adjuste

variations in NPV; however, for simparameters were assumed constant as

TABLE J.3

CONSTANT PARAMETERS IN SENSITIVITY ANALYSIS

ParameterParameter Description Symbol

Density of in-situ reservoir sediment. rd

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parameters were assumed constant as

Table J.4.

The model outcomes from changes

cal input parameters generally followe

trends. For example, increasing width

for a constant value of flushing flow r

long-term capacity ratios and increas

ment load results in more sediment be

in the reservoir prior to removal. Insp

results leads to the conclusion that

model is consistent.

Gould’s Gamma Function Sensitiv

Yield calculated using Gould’s Gamma

tested for the following reservoirs: Ba(India); Sefid Rud (Iran); Abdel Karim

Bin El Ouidane, Ennakhla, Hassan I,

Mohammed V, Moulay Youssef, Oued

Sidi Driss and Timi N’Outine (Moro

(Pakistan); Polgolla and Victoria (Sri

Gebidem (Switzerland). Data used in

are in Table J.6.

The analysis of Gould’s Gamma yresulted in definite cases where the eq

plicable and where it is not. The reser

vided by mean annual runoff is the k

All reservoirs with Wt/MAR greater th

the trend that increasing probability o

creased reliability of resource) allows

be taken from the reservoir. However, w

is less than 0.2, the trend is less preincreasing probability of failure and

negative for 5 percent probability of f

is a physical impossibility. Wt/MAR p

ginally but acceptably in the range of 0

Density of in situ reservoir sediment. rd

Estimated reservoir water temperature. T

Sediment type category to be removed

  by hydrosuction dredging (medium Type

  sand/smaller or gravel).

Reservoir similar to Chinese reservoirs?

  “3”: if reservoir sediments are signi-

  ficantly larger than median grain size  (d50) = 0.1mm or if the reservoir has ANS

  been impounded for more than 10 years

  with out sediment removal. Use “1”: if

  otherwise. A value of “3” was used

  throughout the analysis.

Is reservoir yield ever used for

  hydroelectric power? HP

Sediment type for Brune Curve

  calculations. Brune curve

TABLE J.4

ASSUMED CONSTANT REMOVAL PARAMETERS

Parameter Assumed

Parameter Description Symbol Value

Acceptable probability of pr 0.01

  failure to provide reservoir

  yield in a given year

  (as decimal).

Maximum fraction of total yield YA 1

  that is allowed to be used in

  HSRS operations.

Maximum percent of capacity cl 75%

  loss allowable at any time in

  reservoir. Allowable loss must

be greater than the existing loss

S E N S I T I V I T Y A N A LY S E S

TABLE J.5

ECONOMIC PARAMETER ASSUMPTIONS.

Parameter Description Parameter Symbol Ass

If dam being considered is an existing dam enter 0. If the Edam is a new construction project, enter 1.

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  dam is a new construction project, enter 1.

Unit Cost of Construction. This cost is estimated using So c Defau

  specified in Reservoir Geometry.

Cost of Dam Construction. The default cost is estimated as C2 Defau

  unit cost of construction times initial reservoir storage

  volume (C2 = So*c*E).

Reservoir (Dam) Operation and Maintenance Coefficient omc

Dam Salvage Value Coefficient a

Discount Rate (decimal) r

Price of Net Reservoir Yield. P1

Unit Value of Water Used released downstream during actual

  flushing operations (water lost during drawdown is internally

  assigned a value of zero). PF

Unit value of water released downstream of dam in river by

  hydrosuction operations. PH

Unit value of water used in dredging operations. PD

Unit cost for hydrosuction operations expressed as $/m3  of

  sediment removed. CH

Unit cost of traditional dredging CD Defau

TABLE J.6

INPUT FOR GOULD’S GAMMA FUNCTION TESTING.

Existing Average Annual StandardReservoir Capacity (106 m3) Inflow (106  m3) of Average A

Polgolla, Sri Lanka 2.6 1,838.0 27

Victoria, Sri Lanka 713.1 1,571.0 43

Abdel Karim El Khattabi, Morocco 8.9 48.2 3

Bin El Quidine, Morocco 1253.0 1,050.0 60

Ennakhla, Morocco 4.9 55.0 3

Hassan I, Morocco 245.0 288.5 14

Ibn Battouta, Morocco 33.9 52.3 4

Mohammed V, Morocco 362.6 750.0 38

Moulay Youssef, Morocco 159.4 287.0 14

T H E R E S C O N A P P R O A C H

TABLE J.7

SENSITIVITY TO VALUE OF UNIT RESERVOIR YIELD

(P1=$0.1/M3 TO P1=$0.2/ M3)

Change in NPV

Possible Strategies Technique ($ 1000 million)

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Sensitivity to Economic Parameters

Changes in economic parameters may alter not only

the ranking of desirable sediment management strat-egies, but could also affect the amount of sediment

removed with each strategy and magnitude of vari-

ables such as the timing of decommissioning and

any retirement fund contributions. Sensitivity analysis

was performed on key economic parameters of the

Tarbela Dam case study to investigate these effects

and test the model for consistency with economic

intuition. The following parameters were varied: priceof net reservoir yield (P1), rate of discount (r), mar-

ket rate of interest (m), cost of operations and main-

tenance coefficient (omc) and costs of sediment

removal for different techniques The results of this

sustainable solutions is somewhat hig

for non-sustainable solutions. Also, t

capacity ratio (LTCR) increases by 31

percent respectively for dredging andfollows that the higher water prices ge

tives to keep more storage capacity. I

flushing, changes in economic param

affect LTCR because the latter is deter

gineering features rather than econom

tion.

r: Discount Rate

The discount rate determines the we

benefit and cost relative to the prese

Non-sustainable (Decommissioning)-with No Removal N/A 138.4

Non-sustainable (Decommissioning)-with Partial Removal HSRS 138.4

Non-sustainable (Run-of-River)-with No Removal N/A 138.7

Non-sustainable (Run-of-River)-with Partial Removal HSRS 138.7

Sustainable Flushing 139.2

Sustainable HSRS N/A

Sustainable Dredging 142.3Sustainable Trucking 138.8

Change in LTC (million m 3) Chang

Long term reservoir capacity for Flushing 0

Long term reservoir capacity for HSRS N/A

Long term reservoir capacity for Dredging +1,890

Long term reservoir capacity for Trucking +405

S E N S I T I V I T Y A N A LY S E S

TABLE J.8

SENSITIVITY TO DISCOUNT RATE

(r reduced from 5% to 3%)

Change in NPV

Possible Strategies Technique ($ 1000 million

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m: Market Rate of Interest

The annual retirement fund is calculated using the

market interest rate (i.e., the rate of return on in-vesting the fund). The value of this annual contri-

bution is reported only when decommissioning cost

exceeds any benefit of dam removal. For the Tarbela

case study simulation, it is assumed that US$2.5

billion is the net cost of decommissioning the dam.

The corresponding annual retirement fund is US$2

million with 5 percent market interest rate. If the

interest rate increases from 5 percent to 8 percent,the annual retirement fund contribution decreases

to US$0.29 million. Thus, the annual retirement fund

contribution is highly sensitive to the market inter-

est rate One should also expect that the annual re-

Non sustainable (Decommissioning)-with No Removal N/A 70.2

Non sustainable (Decommissioning)-with Partial Removal HSRS 70.2

Non sustainable (Run-of-River)-with No Removal N/A 72.2

Non sustainable (Run-of-River)-with Partial Removal HSRS 72.2

Sustainable Flushing 81.7

Sustainable HSRS N/A

Sustainable Dredging 89.1Sustainable Trucking 37.9

Change in LTC (million m3)

Long term reservoir capacity for Flushing 0

Long term reservoir capacity for HSRS N/A

Long term reservoir capacity for Dredging 2,025

Long term reservoir capacity for Trucking 270,056

nance cost to initial construction

value of 0.01 means that annu

maintenance cost is 1 percent of i

cost. The results of change in th0.01 to 0.05 are summarized in T

nual operations and maintenanc

dent of sediment management str

in omc reduces the NPVs for al

same amount except for non-sus

decommissioning. As no annual op

tenance cost is incurred after d

change in NPV for non-sustainabing) strategies is slightly lower. L

frequency of sediment removal a

sediment removal are all indepen

in annual operations and mainte

T H E R E S C O N A P P R O A C H

TABLE J.9

SENSITIVITY TO OPERATION & MAINTENANCE COEFFICIENT

(omc = 0.01 to omc = 0.05)

Change in NPV

Possible Strategies Technique ($ 1000 million) Chan

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rameter changes decrease the cost of sediment re-

TABLE J.10

SENSITIVITY TO COST OF SEDIMENT REMOVAL PARAMETERS

 (S2, PH, CD, CT)

Change in NPVPossible Strategies Technique ($ 1000 million) Chang

Non sustainable (Decommissioning)-with No Removal N/A 0

Non sustainable (Decommissioning)-with Partial Removal HSRS 0.2

Non sustainable (Run-of-River)-with No Removal N/A 0

Non sustainable (Run-of-River)-with Partial Removal HSRS 0.2

Sustainable Flushing 1,367.2

Sustainable HSRS N/A

Sustainable Dredging 264.6Sustainable Trucking 3,310.16

Change in LTC (million m3) Change

Long term reservoir capacity for Flushing 0

Long term reservoir capacity for HSRS N/A N

Long term reservoir capacity for Dredging 810

Long term reservoir capacity for Trucking 135

Dredging: CD (unit cost of dredgin

Non sustainable (Decommissioning)-with No Removal N/A –1.801

Non sustainable (Decommissioning)-with Partial Removal HSRS –1.801

Non sustainable (Run-of-River)-with No Removal N/A –1.830

Non sustainable (Run-of-River)-with Partial Removal HSRS –1.830

Sustainable Flushing –1.830

Sustainable HSRS N/A

Sustainable Dredging –1.830

Sustainable Trucking –1.830

S E N S I T I V I T Y A N A LY S E S

sediment removal costs increases the difference be-

tween NPV with sediment removal and that with no

removal. More importantly, the magnitudes involved

suggest the need for technological innovation in

sediment removal because a mar

unit cost of removal has the pot

lion of dollars over the long term

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World Bank 

1818 H Street, NW

Washington, DC 20433

Tel. 1 202 473-1000

www.worldbank.org

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 Among the many sessions of the Third World Water Forum, held in Japan, March 2003, there was

one titled “Sedimentation Management Challenges for Reservoir Sustainability”. Two main messages

emerged from that session:

• Whereas the 20th century focused on reservoir development, the 21st century will necessarily

focus on sediment management; the objective will be to covert today’s inventory of non-

sustainable reservoirs into sustainable infrastructures for future generations.

• The scientific community at large should endeavor to devise solutions for conserving existing

water storage facilities in order to enable their functions to be delivered for as long as possible,

possibly in perpetuity.

These important messages are very much in line with the World Bank’s Water Resources Sector

Strategy that calls the Institution to address management of existing infrastructure, as well as to

develop much needed priority water infrastructure.

In fact, many poor countries facing similar climate variability as rich countries, have as little as

1/100th as much water infrastructure capacity. The result is great vulnerability to the vicissitudes of 

climate variability, a vulnerability which is exacerbated by climate change. There is much that can

and must be done by managing watersheds better, and managing demand.

The present book can assist in making existing reservoirs sustainable, as well as in the sustainable

design of new surface storage facilities. The book addresses the issue of reservoir sustainability

from an economic angle, a perspective hardly explored so far.

 We hope that this initial step will encourage others to follow, both in additional research, and in

actions aimed at conserving water storage assets for future generations.

Ian Johnson

Vice President, Sustainable DevelopmentWorld Bank