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SIXTH INTERNATIONAL CONFERENCE ON GEOMORFOLOGY September 7-11, 2005 ZARAGOZA Consequences of river regulation Consequences of river regulation works: works: altered fluvial processes + altered fluvial processes + increasing flood hazard increasing flood hazard Dr. Dr. Tí mea mea Kiss Kiss assistant professor assistant professor Department Department of of Physical Physical Geography Geography and and Geoinformatics Geoinformatics, , University University of of Szeged, Hungary Szeged, Hungary 200 2006. WVU, Morgantown WVU, Morgantown Map of Hungary
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  • SIXTH INTERNATIONAL CONFERENCE ON GEOMORFOLOGY

    September 7-11, 2005 ZARAGOZA

    Consequences of river regulation Consequences of river regulation works: works:

    altered fluvial processes + altered fluvial processes + increasing flood hazardincreasing flood hazard

    Dr. Dr. TTíímeamea Kiss Kiss assistant professor assistant professor

    DepartmentDepartment ofof PhysicalPhysical GeographyGeography andand GeoinformaticsGeoinformatics, , UniversityUniversity ofof Szeged, HungarySzeged, Hungary

    20020066.. WVU, MorgantownWVU, Morgantown

    Map of Hungary

  • SIXTH INTERNATIONAL CONFERENCE ON GEOMORFOLOGY

    September 7-11, 2005 ZARAGOZA

    What is the problem?What is the problem?

    2001

    2001

    2006

    2006

    Problem: Problem: IncreasingIncreasing floodflood levellevel →→ hazardhazard

    Yearly highest water levels on the fluviometer at Mindszent

    Increase in flood levelsbetween 1901 and 2006

  • SIXTH INTERNATIONAL CONFERENCE ON GEOMORFOLOGY

    September 7-11, 2005 ZARAGOZA

    What can be the possible cWhat can be the possible causesauses ofof thetheincreasingincreasing floodflood levelslevels? ?

    Climate (storminess)

    Land-use (canopy)

    Horizontal (migration)

    Vertical (narrowing)

    Roughness (vegetation)

    Aggradation

    Buildings, new constructions

    Increasing height and frequency

    of floods

    Changes on the catchment

    Changes on the floodplain Changes on the

    channel

    Artificial vs. natural

    1. Natural and economic conditions before regulation works 1. Natural and economic conditions before regulation works (mid(mid--1919thth c.)c.)

    2. Engineering works 2. Engineering works (late 19(late 19thth c., early 20c., early 20thth c.)c.)3. Consequences3. Consequences4. Present4. Present--day situationday situation

    ContentContent

  • SIXTH INTERNATIONAL CONFERENCE ON GEOMORFOLOGY

    September 7-11, 2005 ZARAGOZA

    1. Conditions before regulations1. Conditions before regulationsNatural:

    -Huge floodplain

    (swamps)

    -Long-lasting floods

    Social-economic:

    -increasing population

    -Opened W-Eu market

    -Eneneering

    -Financial background

    + PEACE!

    2. 2. HistoryHistory ofof riverriver managementmanagement

    The The „„ggreatreat”” (19(19thth c.) river regulationsc.) river regulationsFrom 1846 until From 1846 until thethe 18901890’’s s Uniform ideas on the whole Uniform ideas on the whole catchmentcatchment

  • SIXTH INTERNATIONAL CONFERENCE ON GEOMORFOLOGY

    September 7-11, 2005 ZARAGOZA

    1.1. CutCut--offs offs (T(Tiszaisza:: 102 places)102 places)→→ decreased length (1214decreased length (1214 →→761 km)761 km)→→ increased gradient (3,7increased gradient (3,7→→7cm/km)7cm/km)→→ SemiSemi--natural natural channelchannel developmentdevelopment

    22. . Levee constructionLevee construction→→ flood protected area 26,500 kmflood protected area 26,500 km22

    →→ length: 2940 kmlength: 2940 km→→ Semi natural Semi natural floodplainfloodplain

    developmentdevelopment3. 3. Drainage systemDrainage system (40,000 km)(40,000 km)

    2. 2. HistoryHistory ofof riverriver managementmanagementThe The „„ggreatreat”” (19th c.) river regulations(19th c.) river regulations

    2. 2. HistoryHistory ofof riverriver managementmanagementRiver management in the 20River management in the 20thth centurycentury

    Floodplain:Floodplain:hardly mahardly maiintainedntained

    (dense vegetation, aggradation, (dense vegetation, aggradation, ((il)legalil)legal constructions)constructions)

    Levees:Levees:continuous heightening continuous heightening

    ((locallocal, not enough), not enough)Channel:Channel:

    bank bank stabilisationstabilisationfollowing following locallocal ideas and designideas and design

    1. Revetment1. Revetmentss260 km on the 590 km long section260 km on the 590 km long section

    2. 2. GroyneGroyness189 189

  • SIXTH INTERNATIONAL CONFERENCE ON GEOMORFOLOGY

    September 7-11, 2005 ZARAGOZA

    3. Consequences3. ConsequencesCCutut--offsoffs

    INCISION

    Lowering the water table

    Land slidesFast, GREAT floods

    Fish population

    Land-use changesClimate change

    Shortened

    Extra sediment load

    Increased gradient

    Pattern change

    widening

    Floodplain aggradation

    Present slope conditions

    3. Consequences:3. Consequences:CCutut--offsoffsCChannelhannel

    slope changesslope changes

  • SIXTH INTERNATIONAL CONFERENCE ON GEOMORFOLOGY

    September 7-11, 2005 ZARAGOZA

    3. Consequences:3. Consequences:CCutut--offsoffsincisionincision

    3. Consequences:3. Consequences:CCutut--offsoffsincisionincision

    width depth

    Max (m) mean (m) max (m) mean (m) shape index

    Area (m2)

  • SIXTH INTERNATIONAL CONFERENCE ON GEOMORFOLOGY

    September 7-11, 2005 ZARAGOZA

    3. Consequences:3. Consequences:CCutut--offsoffs

    pattern changepattern change

    3. Consequences3. Consequenceslevee constructionslevee constructions

    Lowered

    water table

    Micro-climate change (dryer,

    warmer)

    Soil alterations

    (salinization, dry-land solis)

    Decreased area of wetlands

    Need of irrigation

    Artificial (active) floodplain Protected (inactive) floodplain

    Inland water problems(active subsidence, no accumulation)

    narrow

    Large sediment

    imput Intensive aggradation

    Altered land-use, Invasive species

    High floods

    (5 m water-depth)

    GREAT, large floods

    High friction

  • SIXTH INTERNATIONAL CONFERENCE ON GEOMORFOLOGY

    September 7-11, 2005 ZARAGOZA

    3. Consequences3. Consequenceslevee constructionlevee construction

    Intensive accumulationIntensive accumulation

    3. Consequences3. Consequenceslevee constructionlevee construction

    Intensive accumulationIntensive accumulation

  • SIXTH INTERNATIONAL CONFERENCE ON GEOMORFOLOGY

    September 7-11, 2005 ZARAGOZA

    0,0

    0,5

    1,0

    1,5

    2,0

    2,5

    3,0

    1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24

    szelvények

    (m)

    hullámtéri akkumuláció mértéke

    3. Consequences3. Consequenceslevee constructionlevee construction

    Intensive accumulationIntensive accumulation

    Amount of aggradation (m)

    3. Consequences3. Consequenceslevee constructionlevee construction

    WetWet--land reductionsland reductions

    I. Military survey (late 18th c.)

    II. Military survey (late 19th c.)

  • SIXTH INTERNATIONAL CONFERENCE ON GEOMORFOLOGY

    September 7-11, 2005 ZARAGOZA

    I. Military survey (late 18th c.)

    Topographical map (1980)

    3. Consequences3. Consequenceslevee constructionlevee construction

    WetWet--land reductionsland reductions

    3. Consequences3. Consequenceslevee constructionlevee constructionSalinizationSalinization

  • SIXTH INTERNATIONAL CONFERENCE ON GEOMORFOLOGY

    September 7-11, 2005 ZARAGOZA

    3. Consequences3. Consequencesrevetment constructionsrevetment constructions

    Narrowing due to dense riparian vegetation

    Large sediment

    imput

    No lateral erosion

    Smaller cross-section

    GREATer, large floods

    Slight incision

    Active point-bar formation

    Smaller flood conductivity

    Sharper bends

    Slope decrease

    Tisza, Szolnok

    Same discharge – increasing flood height

    Something wrong!!Something wrong!!

    DDischargeischarge –– Stage (water level) Stage (water level)

    Rising

    stage

    Falling stage

  • SIXTH INTERNATIONAL CONFERENCE ON GEOMORFOLOGY

    September 7-11, 2005 ZARAGOZA

    In case of freely developing meanders

    3. Consequences3. Consequencesrevetment constructionrevetment construction

    Revetment construction (1940), upper section straightened (1886)

    3. Consequences3. Consequencesrevetment constructionrevetment construction

  • SIXTH INTERNATIONAL CONFERENCE ON GEOMORFOLOGY

    September 7-11, 2005 ZARAGOZA

    CrossCross--sectionalsectional changeschanges

    at inflexion point

    in axis of meander

    at revetment

    Decrease of cross-s. area 2-3%

    Decrease of cross-s. area 4-6 %

    Decrease of cross-s. area 6-19 %

    Flood conductivity ??

    FloodFlood conductivityconductivity chageschages duedue toto alteredaltered crosscross--sectionalsectional parametersparameters

  • SIXTH INTERNATIONAL CONFERENCE ON GEOMORFOLOGY

    September 7-11, 2005 ZARAGOZA

    decliningdeclining-- 66--13 %13 %

    ((worseworse thanthan ininnaturalnatural statestate))

    narrowernarrower, , deepdeepchannelchannel

    areaarea decreasedecrease

    lowlow sinuositysinuositynarrowingnarrowing bendsbends

    2020thth c. c. regulationsregulations((sincesince 19301930’’s)s)

    revetmentsrevetments

    higherhigher+2+2--3 %3 %

    widewide, , deeperdeeperchannelchannel

    areaarea increaseincrease

    lowerlower sinuositysinuositylargelarge bendsbends

    1919thth c. c. regulationsregulations(1890(1890-- 1929)1929)

    cutcut--offsoffs

    normalnormalwidewide channelchannellargelarge areaarea

    highhigh sinuositysinuositynarrownarrow bendsbends

    NaturalNatural statestate

    FloodFloodconductivityconductivity

    CrossCross--sectionssectionsPlanimetryPlanimetry

    ConclusionsConclusionsRiver management vs. channel development

    What to do now? What to do now?

    To do nothing = heroic work, spending money during flood (on nothing)

  • SIXTH INTERNATIONAL CONFERENCE ON GEOMORFOLOGY

    September 7-11, 2005 ZARAGOZA

    What to do now? What to do now?

    Climate (storminess)

    Land-use (canopy)

    Horizontal (migration)

    Vertical (narrowing)

    Roughness (vegetation)

    Aggradation

    Buildings, new constructions

    Changes on the catchment

    Changes on the floodplain

    Changes on the channel

    River restoration? New ways of river and watershed management?

    Decrease run-off:Stream restoration?

    Land-use optimalization?Storage lakes?

    Decrease roughness:Floodplain restoration?

    Land-use optimalization??

    Increase flood conductivity:Channel restoration?Removal of levees?

    Land-use optimalization??

    Learn from our mistakes!Learn from our mistakes!

    -Long river regulation history

    -To monitor changes:

    long hydrological data set: water level data (since the 1860’s)

    precise Q data (since 1960’s)

    spatial data: map series (first survey 1790”s)

    cross sections (since 1890)

    -Easy to start the devil’s circle

    (continuous maintenance should be needed)

  • SIXTH INTERNATIONAL CONFERENCE ON GEOMORFOLOGY

    September 7-11, 2005 ZARAGOZA

    ThankThank youyou forfor youryour attentionattention!!


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