i
IMPACT OF URBANISATION ON
GROUNDWATER IN KARAPAKKAM VILLAGE
A THESIS
Submitted by
R. SUBALAKSHMI
in partial fulfillment for the award of the degree of
MASTER OF ENGINEERING IN INTEGRATED WATER RESOURCES MANAGEMENT
CENTRE FOR WATER RESOURCES DEPARTMENT OF CIVIL ENGINEERING
ANNA UNIVERSITY: CHENNAI 600 025
MAY 2011
ii
ANNA UNIVERSITY:: CHENNAI 600 025
BONAFIDE CERTIFICATE
Certified that this report titled “IMPACT OF URBANISATION ON
GROUND WATER IN KARAPAKKAM VILLAGE” is the bonafide work of
Ms. R. SUBALAKSHMI (Roll No. 2009262018) who carried out the work
under my supervision. Certified further, that to the best of my knowledge the
work reported herein does not form part of any other thesis or dissertation on the
basis of which a degree or award was conferred on an earlier occasion on this or
any other candidate.
Dr. K. ILAMPARUTHI Mr.V.LENIN KALYANA SUNDARAM
Professor and Head Assistant Professor
Department of Civil Engineering Centre for Water Resources
Anna University Anna University
Chennai - 600 025. Chennai - 600 025.
iii
ABSTRACT
Urbanisation in India has resulted in population increase and
infrastructure development which in turn have led to a large demand for water.
The demand for water and population growth has increased exponentially in
Karapakkam, whereas water availability (surface and ground water potential) has
decreased. Most of the agricultural lands have rapidly converted in to hotels and
IT sectors. During the last 8 years, over exploitation of groundwater for
industrial, domestic and irrigation purpose has occurred in a large scale.
An attempt has been made to study and delineate the land use changes
for the selected years and to study the impact of urbanisation on groundwater
quality and quantity using Remote Sensing and GIS. Land use and land cover
classification is applied to delineate entire study area with the help of ground
truth verification. Groundwater potential is calculated using long term trend
analysis method. Ground water quality assessment is an important factor to
ensure safe and sustainable use of water. Groundwater quality of the surrounding
area is analysed for physical and chemical parameters. Water quality index is
calculated based on the water quality parameters. Based on these index values,
groundwater quality index map was generated. Land use changes, groundwater
quality and groundwater potential are used to assess the environmental changes
which affect the livelihood of people. Focus group discussions and questionnaire
survey are used to evaluate the livelihood changes.
iv
The results indicate that the effects of urbanisation has affected
agriculture, groundwater condition and livelihood changes. In 2002, 38% of the
land was used for agricultural purpose whereas now, there are no agricultural
activities in the village. This is because of scarce water sources, agricultural
labour and demand of agricultural land for urban uses. Urbanisation has greatly
affected the groundwater condition. Okkium Maduvu and Renganathan Street
wells were unfit for drinking purpose, because these two wells are located
nearby Okkium Maduvu River, which is very near to Pallikaranai swamp. The
contaminant from the Pallikaranai swamp passes through this river and drains at
Buckingham canal. In 2002, the well water condition was very good. Now, 78%
of the well water is not fit for drinking purpose. 51% of people are using
portable water and other’s use panchayat water and water from nearby villages.
On the other hand, urbanisation has created many employment opportunities.
66% of people are now earning more than Rs. 7000 and 21% of people earn
more than Rs. 10000
From the results, urbanisation has led to a great economic growth and
growth of commercial actives but unplanned urbanisation has led too many
problems and pathetic situations such as flooding, traffic, unhygienic and poor
environment. The groundwater resource has also witnessed a rapid decrease in
quantity and quality. Management measures have to be adopted in order to
conserve this resource. Also, opportunities should be created within rural areas
to prevent migration to cities and minimize the urbanisation effects and increase
the benefits.
v
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vii
ACKNOWLEDGEMENT
First and foremost I am grateful to GOD ALMIGHTY for having given
me a wonderful life and infinite blessings. My sincere and heartfelt gratitude to
Mr. V. LENIN KALYANA SUNDARAM, Assistant Professor, Centre for
Water Resources, Anna University for his expert guidance, valuable suggestions,
continued help and constant encouragement.
I express my sincere thanks to Dr. K. ILAMPARUTHI, Head,
Department of Civil Engineering, Dr. N. K. AMBUJAM, Professor and
Director, Centre for Water Resources for their keen and continued interest
during my project work.
I would like to express my special thanks to, Dr. S. RAVICHANDRAN,
Professor in-charge, Integrated Water Resources Management,
Dr. N. G. ANUTHAMAN, Associate Professor, Mr. M. BALAMURUGAN
Assistant Professor, Dr. R. SARAVANAN Assistant Professor and
Dr. PRAKASH NELLIYAT, Research Co-ordinator, Centre for Water
Resources, for their illuminating suggestions and constructive criticisms.
I express my heartfelt and deep sense of gratitude to all our Department
staff members, also I extend my thanks to The Government of Netherlands
and SaciWATERS for the fellowship provided. And I would like to thank
Karapakkam Village People for their supports.
Finally I express my gratitude to my FAMILY MEMBERS and
FRIENDS for their valuable support and encouragement during this project
work.
SUBALAKSHMI R
viii
TABLE OF CONTENTS
CHAPTER NO TITLE PAGE NO
ABSTRACT (ENGLISH) iii
ABSTRACT (TAMIL) v
ACKNOWLEDGEMENT vii
LIST OF TABLES xi
LIST OF FIGURES xii
LIST OF ABBREVIATIONS xiv
1 INTRODUCTION 1
1.1 GENERAL 1
1.1.1 Groundwater 1
1.1.2 Characteristic of Groundwater 1
1.1.3 Urbanisation 2
1.1.4 Urbanisation in India 2
1.1.5 Urbanisation in Tamil Nadu 3
1.1.6 Effects of Urbanisation 5
1.2 NEED FOR THE STUDY 6
1.3 OBJECTIVES 7
1.4 ORGANIZATION OF THE THESIS 7
2 REVIEW OF LITERATURE 9
2.1 GENERAL 9
2.1.1 Urbanisation 9
2.1.2 Groundwater 9
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CHAPTER NO TITLE PAGE NO
2.1.3 Water Quality 9
2.1.4 Livelihood 10
2.2 LAND USE CHANGES 10
2.3 GROUNDWATER QUALITY 11
2.4 GROUNDWATER POTENTIAL 14
2.5 LIVELIHOOD ASSESSMENT 16
2.6 SUMMARY 18
3 STUDY AREA AND METHODOLOGY 19
3.1 GENERAL 19
3.2 STUDY AREA 19
3.2.1 Climate and Rainfall 19
3.2.2 Description of the Study Area 20
3.3 METHODOLOGY 22
3.3.1 Reconnaissance Survey 23
3.3.2 Data Collection 24
3.3.3 Data Analysis 25
3.3.4 Land Use Changes 25
3.3.5 Groundwater Quality 26
3.3.6 Groundwater Potential 28
3.3.7 Livelihood Assessment 30
4 RESULTS AND DISCUSSION 31
4.1 GENERAL 31
4.2 CHANGES IN LAND USE PATTERN 31
4.3 GROUNDWATER QUALITY 36
4.3.1 Temporal Variation of Groundwater
Quality Parameters 36
x
CHAPTER NO TITLE PAGE NO
4.3.2 Water Quality Index (WQI) 36
4.3.3 Generation of Water Quality Index Map 39
4.4 GROUNDWATER POTENTIAL 42
4.4.1 Analysis of Water Level 42
4.4.2 Groundwater Quantity 44
4.5 LIVELIHOOD ASSESSMENT 47
4.5.1 Source of Drinking Water 47
4.5.2 Analysis of Groundwater Quality 48
4.5.3 Agricultural Status 51
4.5.4 Economic Status 51
4.5.5 Sanitation and Health Status 52
4.5.6 Impact of Urbanisation 53
5 SUMMARY AND CONCLUSION 55
5.1 SUMMARY 55
5.2 CONCLUSION 56
REFERENCES 58
ANNEXURE
xi
LIST OF TABLES
TABLE NO TITLE PAGE NO
Table 1.1 Urban Population of Tamil Nadu 4
Table 3.1 Categories of Water Quality Index 28
Table 4.1 Land use Pattern for the Years 2002, 2004,
2006, 2008 and 2010 32
Table 4.2 Water Quality Parameters, BIS Standards and
Weighting factor 37
Table 4.3 Water Quality Classification based on WQI of
September 2010, January, February and
March 2011 38
Table 4.4 Water Level Data for the Years 2002 and 2006 42
Table 4.5 Groundwater Quantity for January and
February 2011 46
xii
LIST OF FIGURES
FIGURE NO TITLE PAGE NO
Figure 1.1 Effect of Urbanisation 6
Figure 3.1 Index Map of Karapakkam Village 21
Figure 3.2 Details of Study Area 22
Figure 3.3 Flowchart for Methodology 23
Figure 3.4 Flowchart for Land Use Changes 26
Figure 3.5 Well Location Map of Karapakkam Village 27
Figure 4.1 Land use Map of Karapakkam Village -2002 33
Figure 4.2 Land use Map of Karapakkam Village -2004 33
Figure 4.3 Land use Map of Karapakkam Village -2006 34
Figure 4.4 Land use Map of Karapakkam Village -2008 34
Figure 4.5 Land use Map of Karapakkam Village -2010 35
Figure 4.6 Water Quality Index Map-September 2010 40
Figure 4.7 Water Quality Index Map-January 2011 40
Figure 4.8 Water Quality Index Map-February 2011 41
Figure 4.9 Water Quality Index Map-March 2011 41
Figure 4.10 Water Level Fluctutation 42
Figure 4.11 Water level Contour-January 2011 43
Figure 4.12 Water level Contour-February 2011 43
Figure 4.13 Water level Contour-March 2011 44
Figure 4.14 Theissen Polygon Map 45
Figure 4 15 Groundwater Quantity 45
Figure 4.16 Sources of Drinking Water 48
Figure 4.17 Amounts Spend for Drinking Water 48
Figure 4.18 Reasons for Water Quality Deterioration 49
Figure 4.19 Water Quality Map- 2002 49
xiii
FIGURE NO TITLE PAGE NO
Figure 4.20 Water Quality Map- 2005 50
Figure 4.21 Water Quality Map- 2010 50
Figure 4.22 Agricultural Status 52
Figure 4.23 Economic Status 52
Figure 4.24 Sanitation Facility Status 52
Figure 4.25 Health Impact 52
Figure 4.26 Major Health Problem 53
xiv
LIST OF ABBREVIATION
BGL Below ground level
GIS Geographic Information System
GWQI Groundwater Quality Index
MCM Million Cubic Meter
MoHA Ministry of Home Affairs
MRC Master Recession Curve
OIF Optimum Index Factor
SOI Survey of India
WQI Water Quality Index
WTF Water Table Fluctuation
HCO3 Bicarbonate
Ca Calcium
CO3 Carbonate
ERDAS Earth Resources Data Analysis System
E East
EC Electrical conductivity
ha Hectare
Km Kilometer
Mg Magnesium
µs/cm Micro-siemens/cm
mg/l Milligram per litre
N North
% Percent
pH Potential of hydrogen ions
Na Sodium
TDS Total Dissolved Solids
TH Total Hardness
1
CHAPTER 1
INTRODUCTION
1.1 GENERAL
1.1.1 Groundwater
In India, groundwater plays a crucial role in increasing food and
productions, providing drinking water and facilitating industrial development.
Groundwater is a major source of water which meets agricultural, industrial and
drinking water requirements. Groundwater forms one of the important sources of
water supplies in many areas, as it is believed to be safe and free from
pathogenic bacteria and from suspended matter. The pace of groundwater
withdrawal in many fertile regions is increasing phenomenally due to the fast
pace of population growth accompanied by agricultural and industrial
development.
1.1.2 Characteristic of Groundwater
i) It is almost universally available, with variation in levels, quality
and quantity.
ii) It is common property resource as no single person or organisation
can own it.
iii) It is dynamic equilibrium between rain water, surface water bodies
including ponds, lakes, wetlands, rivers, tanks and groundwater.
2
Forest and trees are part of this system as both forests and trees
play crucial role in groundwater recharge.
iv) Many aquifers are to offer natural protection from contamination,
so untreated groundwater is usually cleaner and safer than its
untreated surface water equivalent.
v) Groundwater is relatively easy and cheap to use. It can be brought
on stream progressively with little capital outlay and boreholes can
often be drilled close to where the water supply is needed.
vi) It is a resource that is organisationally easy to develop.
1.1.3 Urbanisation
Urbanisation refers to a process in which an increasing proportion of an
entire population lives in cities and change in land use from agriculture to
human settlements, commercial sectors and industries. In developing country
urbanisation and population pressure are two main challenges to water resource
management especially in cities of developing countries. The interaction
between urban development and demand to water are affecting the quantity and
quality of groundwater. Generally the change in groundwater quantity and
quality are caused by increase in groundwater abstraction and the existing new
sources of recharge.
1.1.4 Urbanisation in India
India is the most populous country in the world after China. Population
of India is 1.14 billion (MoHA, India 2008). All developmental sectors are in
growing state, villages which once did not have the basic amenities for water
and electricity even after several years of independence are being provided with
these facilities in recent years through several government-sponsored programs.
Despite these efforts to improve rural facilities, there is a rapid migration of rural
3
population to urban areas possibly for better work opportunities and living
conditions. The urban areas are fast getting densely populated and are expanding
rapidly to adjoining areas putting unwanted stress on the natural resources.
Agricultural lands around the urban areas are rapidly decreases and converted to
hotels and tall buildings. Value of these lands is also increasing and the
environmental health around these areas is on the decrease.
The improvement in infrastructural facilities and increase in trained
manpower, several small to large-sized industries are being rapidly established
with no proper disposal facilities for their effluents. It creates an environmental
chaos especially in the rapidly expanding towns and cities across the country.
Groundwater quality is soon getting deteriorated due to seepages from unlined
sewerage lines and effluent channels. The impact of urbanisation on the
groundwater in an urban area depends on geographical location and the
economic status of the city or even the country (Naik et al. 2005).
1.1.5 Urbanisation in Tamil Nadu
Tamil Nadu is the first urbanisation state among the fifteen major states
in the country. Urbanisation has been increasing since 1961. Tamil Nadu has
emerged as the state with the highest level of urbanisation (43.86 percent) in the
country. The total population of Tamil Nadu is 6.21 cores according to 2001
census. Out of the total population 2.72 core people are living in urban areas.
Urban population of Tamil Nadu require a wide range of urban services
including water supply, sewerage, solid waste management and streets as well as
social infrastructure like schools, hospitals, markets and so on. Urban population
of Tamil Nadu listed in Table 1.1.
Tamil Nadu has a much dispersed pattern of urbanisation with
municipalities in virtually every district (excluding Ariyalur and Perambalur).
The boundaries of Chennai District are contiguous with the Chennai Municipal
Corporation. However, the Chennai Metropolitan area is a larger area which
4
includes several municipalities and town panchayats in Tiruvallur and
Kancheepuram Districts.
Table 1.1 Urban Population of Tamil Nadu
Year No.of
towns
Urban
population
Urban
population (%)
Decadal
growth (%)
Annual growth
rate (%)
1981 434 159.5 32.95 27.98 2.47
1991 469 190.77 34.15 19.59 1.79
2001 832 272.42 43.86 42.79 3.56
Source: (Census of India, 2001)
The spatial distribution (by district) of the six corporations, 104
municipalities and 611 town panchayats, clearly illustrates that urbanisation is
not limited to anyone part of the State. However the urban population is
concentrated along certain urban corridors. Poor persons are estimated during
1999-2000 as 49.97 lakhs in the urban areas according to census of India.
i) Water supply
An increasing urban population has been creating a huge gap between
demand and supply of water every year. According to 2001 census, 30 percent
of urban towns have not access to safe drinking water. The minimum per capita
supply of water required in urban areas varies from 70 lit/day to 130 lit/day and
this requirement of water supply varies according to the land use classification
of the towns. The government spends 141.69 cores to urban water supply on
2003 -2004 (TWAD, 2005).
ii) Pollutants
Due to high influx of population in urban areas the consumption
patterns, unplanned urban and industrial development has led to the problem of
5
air and water pollution. Many urban centres and industrial units are located in
densely populated areas. The large industries have very high aggregate pollution
potential. Due to these aspects the large numbers of people are affected.
Due to increase in urbanisation the density of motor vehicles per km2
has increased from 22 to 52 percent in 1996 to 2004. This has led to traffic
congestion and release of many toxic air pollutants into the atmosphere.
Particularly, the growth of two wheelers is increasing in a steep manner and
contributing to 50.6 percent of the pollution load. Results of poor maintenance
of vehicles are spewing out of noxious fumes into the atmosphere. Apart from
the concentration of vehicles in urban areas and the other reasons for increasing
vehicular pollution are the types of engines used, age of vehicles, congested
traffic, poor road conditions and outdated automotive technologies and traffic
management systems. Vehicles are a major source of pollutants in major cities.
1.1.6 Effects of Urbanisation
Due to urbanisation flood can be occurred and create more pollution.
The pollutions are air pollution, water pollution, solid pollution and congestion.
Air pollution is particularly noticeable in rapidly urbanising villages, where
industry tends to be located within or adjacent to the settlements. In the absence
of industrial electricity, low-grade coal is used to fire the furnaces, which causes
many factories to emit black smoke. Traffic is considered the most important
source of air pollution.
Water pollution is caused by industry and households. Main problem
was lacking of good sewage system. Some villages still have open sewage
drains, even though the population densities are becoming very high. Solid
pollution is including households and industries waste. Household wastes are
mostly organic and contain few toxic substances; industrial wastes are more
dangerous. Hence more drainage facilities have to be constructed with proper
6
planning. The extraction of water in urban areas is more compared to rural areas.
Figure 1.1 shows that the effect of urbanisation.
Figure 1.1 Effect of Urbanisation
1.2 NEED FOR THE STUDY
Water resources are vital inputs to livelihood production activities in a
wide variety of ways. Urbanisation and population pressure are two main
challenges to water resource management, especially in cities of developing
countries. Urbanisation reduces infiltration of groundwater due to the
impermeable nature of the catchments by paved areas, buildings and roads.
The runoff from the increased pavement goes into storm sewers, which
then goes into streams. Usually this runoff is used to soak into the ground. But
now due to urbanisation it goes to the streams and causing flood. Changing a
stream channel can cause flooding and erosion along the stream banks. Also
more sewage is discharged into the streams.
The groundwater recharge may be decreased as a result of urbanisation.
Groundwater recharge is often linked with dry-season flows and groundwater
contributes as much of the river discharge during the dry season. Also the
groundwater is recharged from waste water, sewage mixed water and septic
More water use
Compare to rural
More drainage
More pollution
Less recharge
More floods
Urbanisation
7
tank, so groundwater gets polluted. People cannot access that water for drinking
purpose.
Chennai and urban villages have faced continuous drought leading to a
serious decline in the water table and water yields. Urbanisation has created
serious livelihood problems in the villages.
As far as groundwater is concerned it is mentioned that urbanisation
affects both the quantity and quality of groundwater systems and livelihood
impact of the people in the village. Remote sensing and geographical
information system have been used for a long time to study land use patterns,
groundwater quantity and quality and collecting spatial information.
1.3 OBJECTIVES
Due to increasing population most of the lands are converted to
infrastructure for urbanisation. Unplanned urbanisation creates the problem in
groundwater quality, quantity and livelihood. Objectives are framed in order to
study these problems.
The objectives of the study are:
i) To delineate the land use changes for different periods using
satellite imagery;
ii) To study the impact of urbanisation on groundwater quality and
quantity; and
iii) To assess the environmental changes which affect the livelihood of
people through questionnaire survey.
1.4 ORGANIZATION OF THE THESIS
i) Chapter 1 includes introduction, need for the study and the
objectives framed for the present study.
8
ii) Chapter 2 describes the previous work done by various
researchers in the relevant field that come within the scope of the
present study and the earlier studies carried out in the study area
are also considered.
iii) Chapter 3 deals with the methodology adopted in the present
study for attaining the objectives which was based on the literature
survey. Also the location and background information about the
study area are also included.
iv) Chapter 4 covers the results of the analysis done and the
discussions carried out in this regard.
v) Chapter 5 gives the summary and conclusions for this study.
9
CHAPTER 2
REVIEW OF LITERATURE
2.1 GENERAL
This chapter describes the previous work done by various researchers in
relevant field that comes within the scope of the present study and the earlier
studies carried out in the area under consideration. Review of literature helps to
frame the methodology to be adopted towards the attainment of objectives which
is discussed in this chapter. The basic definitions of few important terms are
given below.
2.1.1 Urbanisation
According to the United States Postal Service, Urbanisation is an area,
sector or development within a geographic area. Urbanisation is the name for the
movement of people from rural to urban areas, and the resulting growth of cities.
Urbanisation is a process that has occurred, or is occurring, in nearly every part
of the world that humans have inhabited.
2.1.2 Groundwater
Groundwater is one of the most valuable natural resources, which
supports human health, socio - economic development and functioning of
ecosystems (Zektser 2000).
2.1.3 Water Quality
The quality of water is defined in terms of its physical, chemical and
biological parameters, and ascertaining its quality is important before use for
10
various intended purposes such as potable, agricultural, recreational and
industrial water usages, etc ., (Sargaonkar 2003)
2.1.4 Livelihood
A livelihood comprises the capabilities, assets (including both material
and social resources) and activities required for a means of living. A livelihood
is sustainable when it can cope with and recover from stresses and shocks and
maintain or enhance its capabilities and assets both now and in the future, while
not undermining the natural resource base. (Scoones 1998).
2.2 LAND USE CHANGE
Generally population growth is increase and the availability of land
resources is limited. So land use planning is essential. Aim of land use planning
is achieve a systematic assessment of land and water potential, alternatives for
land use, and the economic and social conditions required to select and adopt the
best land use options. Effective land use planning often involves local
communities, scientific information on land resources, appropriate technologies,
and integrated evaluation of resource use Following papers are describes the
various land use planning done various places
Palaniyandi et. al, (1997) had detected the change in land use in
Chengai MGR district, Tamil Nadu, using IRS- 1A-LISS II digital data of 1990,
Landsat 5 TM digital data of 1986 and SOI toposheet and other secondary data.
He observed build-up area and agricultural land use, forest and waste land has
delineated each category using Remote Sensing and GIS technique. Using
digital planimeter each category area has been calculated.
Jaiswal et. al, (1999) had detected the change in land use mid-western
part of Gohparu Block, Shahdol district, Madhya Pradesh using IRS- 1C-LISS
III digital data of 1996 and Survey of India (SOI) toposheet 1967 and other
11
secondary data. From visual analysis of satellite imagery and reconnaissance
survey, major vegetation types and land cover classes were mapped. He had
analysed post-classification comparison techniques.
Brahmabhatt et. al, (2000) used Remote Sensing and GIS technique to
analyze the land use pattern in Mahi Right Bank Canal (MRBC) command area
in Kheda district of Gujarat using Survey of India (SOI) toposheet. Pre-
interpretation field visits and reconnaissance survey, crop types, crop condition,
extent of salinity, water logging, and land cover classes were mapped. Area of
various land cover classes was measured using electronic planimeter.
Jayakumar et. al, (2003) had detected the change in land use in Kolli
Hill, Tamil Nadu, using IRS- 1C-LISS III digital data of 1999, Landsat TM
digital data of 1990 and SOI toposheet and other secondary data. He had
analysed the changes in the cropping pattern and causes for the changes. Matrix
technique was used to interpret the maps in GIS Interpreting module in ERDAS
Imagine Software.
Raturi et. al, (2004) had used Remote Sensing and GIS technique in
Rudraprayag district of Uttaranchal to analyze the vegetation pattern over a
period of time. IRS-1C-LISS III was overlaid on the survey of India (SOI)
toposheet. From visual analysis of satellite imagery and reconnaissance survey,
major vegetation types and land cover classes were mapped. Interpretation was
made based on the tonal variation and textural pattern. The areas sensitive to
landslides, the degraded forest zones that needed special attention during the
developmental activities were identified.
2.3 GROUNDWATER QUALITY
Groundwater is very important natural resources. Due to urbanisation
the groundwater quality is rapidly changed. Various methods are used to
12
evaluate the groundwater quality. Some of the papers are described below about
groundwater quality.
Landwehr et. al, (1974) studied an objective of water quality index. He
described, it is an interesting application of Kendall’s nonparametric
classification procedure for the development of a water quality index. The
authors are completely analysing of results from a survey taken in the fall of
1973. That work shows old and new experts rate water quality was same. Again
ratings were given by experts from different regions. It should be noted that the
form of water quality index as it was published by Brown et al, and the author
has been changed. That form of an index was an excellent estimator of the mean
opinion of the panal.
Graniel et. al, (1999) studied the groundwater quality in the city of
Merida, Yucatan, Mexico, where dependence on groundwater supply is 100%, is
affected by urbanisation. In this study, sampling was carried out in 1991 of 39
samples and recorded the water level. Groundwater samples were analysed by
laboratory techniques. Analytical results provide a baseline to compare with the
earliest available chemical data for 1970. After comparison he suggests, that the
most affected areas coincide with urbanisation.
Anbazhagan et. al, (2004) assess the groundwater quality of Panvel
Basin, Raigarh district, Maharashtra, India using the Geographic Information
System (GIS). GIS based groundwater quality mapping has been carried out in
the region with the help of data generated from chemical analysis of water
samples collected from the basin. In this area the groundwater samples show
quality of groundwater was exceedence in terms of chloride, hardness, TDS and
salinity. These parameters indicate the level of quality of groundwater for
drinking and irrigation purposes. Piper diagram is used to understand the
problems concerning the geochemical of groundwater. Idrisi 32 GIS software
was used for generation of various thematic maps and for spatial analysis and
13
integration to produce the final groundwater quality map. In this study, the
concentration of chloride for post monsoon (390 mg/l) exceeds the desirable
limits (250 mg/l). He suggested groundwater quality is desirable and undesirable
for drinking and irrigation purposes.
Sarkar et. al, (2006) assessed the water quality of a groundwater basin
in Bangladesh for irrigation use. The objectives of the study were to determine
different water quality constituents in groundwater in the study area and to
assess in Pabna district which belongs to the Ganges river floodplain. Common
problems for quality irrigation water were cited and the water quality parameters
indices determined were precisely evaluated and interpreted. From the analytical
result it was observed that the compositions of the groundwater samples were
within the permissible range of irrigation use, except increased chloride values
responsible for toxicity problem. Standard water quality parameter indices like
pH, EC, SAR, SSP, RSBC, TH were found within the acceptable range of crop
production. RSC values were higher (3.26 to 4.16 meq/l) than the permissible
limit (>2.5 meq/l) due to HCO3 – content in the irrigation water that may induce
some permeability problem. Arsenic was traced and at one location it was found
(0.2 to 0.3 mg / l) above the danger limit (> 0.05 mg/l). However, except these
minor discrepancies the groundwater of the study locations was categorized as
excellent to good quality and seemed to be suitable for crop production.
Hameed et. al, (2010) has assessed Evaluating Raw and Treated Water
Quality of Tigris River within Baghdad by Index Analysis. Water quality index
(WQI) is a single value indicator of the water quality determined through
summarizing multiple parameters of water test results into simple terms for
management and decision makers. In this paper, thirteen parameters were
considered. On the basis of these data, raw and treated drinking water from
Tigris River within Baghdad were analysed. Cluster analysis conducted on the
WQI data in this area was applied to detect the fluctuation of water quality. This
paper describes, WQI showed that Tigris water never reached “Excellent” levels
14
nor fallen to “Unsuitable” condition, except in occasional untreated water
samples. Effects of various sources of pollution were evident and the needs for
intensive studies on WQI became evident.
Machiwal et.al, (2010) has focused on a GIS-based assessment and
characterisation of groundwater quality in a semi-arid hard-rock terrain of
Rajasthan, western India using long-term and multi-site post-monsoon
groundwater quality data. Spatio-temporal variations of water quality parameters
were analysed by GIS techniques. Groundwater quality was evaluated based on
a GIS-based Groundwater Quality Index (GWQI). A Potential GWQI map was
also generated by Optimum Index Factor concept. Optimum Index Factor (OIF)
was developed to select an optimum combination of three bands in a satellite
image in order to create a color composite. The Potential Groundwater Quality
Index was then computed by using rank maps of three parameters obtained from
the best Optimum Index Factor (OIF) combination. The groundwater quality
parameter group of Ca, Cl and pH were found to have the maximum value (6.6)
of Optimum Index Factor (OIF). The most influential water quality parameters
were identified by performing a map removal sensitivity analysis among the
groundwater quality parameters. GIS analysis revealed that sulfate and nitrate
ions exhibit the highest (CV > 30%) temporal variation, but groundwater pH is
stable. He suggested the groundwater quality of the study area is generally
suitable for drinking and irrigation (median GWQI > 74).
2.4 GROUNDWATER POTENTIAL
Due to urbanisation groundwater potential is varying place to place.
Some places have more water table and some places have low water table. Some
methods are used to estimate the groundwater potential. Following papers are
described some of the methods are used to estimate the groundwater potential.
Lenters (2001) studied the Long – term Trends in the Seasonal Cycle of
each of the Great Lakes (Lakes Superior, Michigan-Huron, Erie and Ontario)
15
water levels from 1860 -1998. objectives of the study is to find out monthly
changes in water level (∆L), to find the monthly changes in the Great Lakes
water level varied over the period since 1860, to find the variations imply
regarding the seasonal cycle of Great Lakes water levels and find out the differs
from one lake to another. The monthly changes in water level ∆L were
calculated for all the months from the year 1860 -1998 and for all the four
locations and plotted against time. Few plots of ∆L as a function of time over the
139 year period exhibited significant striking trends. It was found that significant
positive trends in one month were nearly balanced by significant negative trends
in another month. This indicated important changes in seasonality of ∆L over
time, but with little or no change in the annual mean ∆L
The author mentioned that there were a number of times where monthly
lake level changes exhibited considerable decadal scale variability but with no
significant linear trend over the 139 year period. Therefore the linear trend
presented in the study are only meant to approximate the real long term changes
and more extensive time series analysis for precise inter annual to decadal
variations are left for future study.
Delin et. al, (2007) he describes the Ground-water recharge was
estimated across Minnesota using a water-table fluctuation method as part of a
recent U.S. Geological Survey (USGS) Groundwater Resources Program
recharge study (Delin and others, 2006). Water-level data used in the water
table fluctuation (WTF) method. Data were collected from various sites across
Minnesota. The USGS has conducted intensive, long-term research at five sites
that yielded 1 to 10 years of continuous water-level data were obtained from the
Minnesota Department of Resources (MDNR) observation well network. Thirty-
four MDNR wells at 31 sites met these criteria, with most of the data collected
before 1980. Where data were available only in analog form, one value from
every fifth day was entered manually into a database.
16
The Master Recession Curve (MRC) approach used in the WTF method
is an automated or semi-automated procedure for calculating DH (tj) from water-
level data. MRC can be used to predict the slope of the hydrograph in the
absence of recharge. Once the MRC is established, positive deviations of the
hydrograph from the MRC are attributed to recharge, allowing recharge to be
quantified even during periods of falling groundwater levels.
Naik et. al, (2008) assess Impact of urbanisation on the groundwater
regime in a fast growing city,solapur,in central India. Objective of this paper is
find out the groundwater quantity and quality. Groundwater recharge is
estimated from four basis.
i) Recharge due to rainfall infiltration,
ii) Recharge due to transmission losses,
iii) Recharge due to irrigation from wastewater and
iv) Recharge due to percolation from surface water tanks
Hill piper diagram (piper 1944) is used to estimate the groundwater
quality. He suggested Urbanisation has thus increased the groundwater recharge
in Solapur city. The groundwater recharge estimated in 1980 was 5.33 MCM
(Million Cubic Meter), while in 1994, it is estimated at 5.60 MCM and he
estimated future demand on water. Solapur is expected to have a groundwater
recharge of 41 MCM during 2020 as estimated previously.
2.5 LIVELIHOOD ASSESSMENT
A livelihood comprises the capabilities, assets and activities required for
a means of living. Livelihood depends upon access to many different types of
assets. The assets are human, physical, financial, social and natural. To
understand this well, assess the livelihood and all the diverse assets it depends
upon skills, access to transport, equipment, telecommunications and the social
networks. Following papers are described about the livelihood assessment.
17
Quang et.al, (2005) describes impact of urbanisation on agricultural in
Hanoi. He conducted interviews with district and municipal officials to analyse
the impacts of urbanisation on agricultural livelihood, used timeline analysis to
identify the changes that took place over the period of urbanisation. And he used
seasonal calendar to know about the cultivation of crops in a year by the people
who still continue to be in farming activity. During group discussions, tools such
as mapping timelines, pie chart, free listing, ranking, transect walking and Venn
diagram were used for analysing the impacts of urbanisation. This paper
describes urbanisation brings about better living conditions for those living
nearby newly urbanised areas by giving opportunities to higher cash income jobs
compared to work in agriculture.
Anantha et al, (2010) had described the impact and potential opportunities
of groundwater irrigation on rural farm households. He focused on the size and
pattern of the groundwater economy in selected villages located in the hard rock
areas of Karnataka, India. He consists of 225 farmers selected from different
categories based on their degree of dependency on groundwater based
agriculture. Using participatory rural appraisal (PRA), wells (both functional and
non-functional), well depth, distance between wells, farm size and farmers’
names were mapped in each village. The information gathered includes, among
other things, a socio-economic profile, details of irrigation wells, information on
access to groundwater irrigation and information about agricultural inputs and
outputs. He suggested that the groundwater scarcity affects the livelihoods of
rural communities based groundwater economy and agricultural economy.
Mandere et. al, (2010) assess the livelihood change and household
income in Nyahururu, Kenya. Objective of this paper is to assess the impact of
the peri-urban development dynamics to household income. The data for this
study was collected through questionnaires and interviews with individual
households in the peri-urban Nyahururu and local government officers to get
details about that village. From the study peri-urban development to accomplish
18
a reduction in poverty for the households not only depends on the infrastructural
developments but rather the socio-economic opportunities that arise from the
developments, which will be dependent on the developers involved and the
government policy.
2.6 SUMMARY
The literature review provided guidelines as to what methods are
available for performing analysis related to this study and also give an idea of
the various data required for the same. Also it could be seen that groundwater
problems quantity, quality and livelihood changes due to urbanisation are seen
throughout the world.
Review of the above literatures helped in framing the methodology of
this study. The land use pattern was delineated using superimposing method and
the water quality index map was generated through GIS contouring method.
Long term trend analysis method and water level fluctuation method was used to
calculate groundwater potential. Finally questionnaire survey and focus group
discussion were used to evaluate the livelihood changes.
19
CHAPTER 3
STUDY AREA AND METHODOLOGY
3.1 GENERAL
This chapter discusses with the description of the study area, its
location, climate and rainfall and the methodology adopted for this study. The
methodology shows the input information, analysis method and output.
3.2 STUDY AREA
Kancheepuram is in the northeast coast of Tamil Nadu and located
adjacent to the Bay of Bengal. It is bounded in the west of Vellore and
Thiruvannamalai districts, north by Thiruvallur and Chennai districts and in the
south by Villupuram district. The district has a total geographical area 439,337
ha with a coastal line of 57 km. For administrative reasons, it has been divided
into 4 revenue divisions comprising of 10 taluks with 1137 revenue villages. For
developmental activities, the district has been divided into 648 village
panchayats. Level of urbanisation in Kancheepuram is 53.48% according to
2001 census.
3.2.1 Climate and Rainfall
Kancheeepuram has a tropical climate with a uniform temperature
round the year. The maximum temperature during summer is 36.6oC and
minimum is 21.1oC respectively and the same are 23.7oC and 19.8oC during
winter respectively. The pre monsoon rainfall is almost uniform throughout the
district. The coastal taluks get more rainfalls rather than the interior regions.
This district mainly depends on seasonal rainfalls. Distress conditions prevail in
20
the event of the failure of rains. Northeast and southwest monsoons are the
major sources of rainfall with 54% and 36% contributions each to the annual
rainfall.
3.2.2 Description of the Study Area
The study area selected for the study is Karapakkam village.
Karapakkam village is located on Sholinganallur taluk, of St.Thomas mount
block of the Kancheepuram district in Tamil Nadu at 12°54'51.01"N latitude and
80°13'45.77"E longitude. The village has Injampakkam, Pallikaranai, Okkiam
Thoraipakkam and Sholinganallur as its boundaries in the East, West, North and
South respectively. There are three wards which hold three members and all are
female. The total village extent is 244.48 ha with 1500 households. The total
population of this village as per 2009 census is 7565 comprising of 4265 most
backward classes, 2479 backward classes, 593 scheduled caste and 56 scheduled
tribes. It is about 10 km away from Thiruvanmiyur. Karapakkam have one
Government well, which is under the control of Public Work Department and it
has nine panchayat well under the control panchayat. Buckingham canal flows
on eastern side of the village. There are few private engineering colleges located
nearby village.
In this area agricultural activities was done before 8 years where paddy
was cultivated in this area. Land owners are sold the agricultural lands to IT
sector due to inadequate water for irrigation purpose. So the people are not
intersested to make agricultural activities. Karapakkam has a secular religious
mix. Hindus, Muslims and Christians live side by side. Like all other Indian
regions Hindus are more in number than Muslims who are slightly more than
Christians. Figure 3.1 depicts the location of Karapakkam village at India level.
Figure 3.2 depicts the location of Karapakkam village.
21
Figure 3.1 Index Map of Karapakkam Village
22
Figure 3.2 Details of Study Area
3.3 METHODOLOGY
The objectives of the study as mentioned earlier in Section 1.3. The
methodology has been framed and showed in flow chart as indicated in
Figure 3.3. The stepwise procedure followed to achieve each objective of this
study is explained in this section.
23
Figure 3.3 Flowchart for methodology
3.3.1 Reconnaissance Survey
As an initial step, a reconnaissance survey was carried out to ascertain a pre-
hand knowledge of the study village. From the walk through survey, the land use
patterns and the agricultural lands, where the impact of urbanisation on
groundwater were identified through physical observation and also from people
through informal interviews.
Study area visit
Survey of India toposheet No: 66D/1 and D/5
Study area delineation Village map
Water level
fluctuation method
Groundwater
Quality Map Groundwater
Quantity
Collection of well
water Samples
Questionnaire survey
Analyses of Water
Quality Parameters
Focus Group Discussion
Land use changes
Groundwater
Quality index Map
Image
Measures for
livelihood changes
24
3.3.2 Data Collection
The data required for this study has been collected under two
subdivisions, namely primary data and secondary data. The field data collection,
questionnaire survey and GPS survey are conducted through survey. Some of the
water level, water quality data, maps and other information are collected from
government and NGO which presented in detail the following sections.
i) Primary Data Collection
a) Fieldworks
As a first step, observation wells were selected randomly. Fieldworks
were carried. Fieldworks included water level measurement, collection of water
sample and measure elevation of the well. Water samples were analyse physical
and chemical parameters in the laboratory.
b) Questionnaire survey
Second primary data was collected through questionnaire survey. The
questionnaire is attached in the Annexure. The information collected based on
the people occupation, changes in land use pattern, drinking water source,
groundwater quality and quantity, agricultural status and health aspects their
opinion regarding the changes in groundwater condition and livelihood due to
urbanisation. The information like occupation status, its income with respect to
change in land use pattern was gathered from village people.
c) GPS survey
The GPS was used to survey the Karapakkam village. During the
survey, the readings were taken at all observation wells and temples in different
places. It is necessary to know about the geographical location and elevation of
the well to calculate groundwater quantity.
25
ii) Secondary Data Collection
Survey of India toposheet number: 66D/1 and D/5 were obtained and
Village map was obtained from Karapakkam Panchayat office. Images were
downloaded from Google earth for 2002, 2004, 2006, 2008 and 2010 with the
help of time line tool. Water level and water quality data for the period 2000 -
2009 were collected from Public Work Department and Central Groundwater
Board at the respective offices.
3.3.3 Data Analysis
The primary data thus obtained from the questionnaire were analysed
using the Microsoft excel. It was used to encode and analyse the quantitative
data and qualitative data information converted to numerical data. Data and
information are presented in appropriate charts to answer clearly the research
questions.
3.3.4 Land Use Changes
Images were downloaded from Google earth for 2002, 2004, 2006,
2008 and 2010 with the help of Google Earth Timeline option. Village map was
obtained from Karapakkam Panchayat office. ArcGIS was used for the analysis
and display of land use map. Geo referencing was done the five images using
GIS tool. The process of geo referencing was done using Survey of India (SOI)
topo map by giving the coordinates, create base map. Land use/ land cover status
was visually interpreted for current year and delineate the land use changes, but
the current year map will be finalized after ground truth verification. The base
map and delineate land use maps was superimposed to delineate present study
area map. Finally the land use/ land cover map of 2002, 2004, 2006, 2008 and
2010 were digitized and incorporated into GIS domain for change analysis. The
methodology for delineation of land use was framed and showed in flow chart as
indicated in Figure 3.4.
26
Figure 3.4 Flowchart for Land use Changes
3.3.5 Groundwater Quality
The groundwater quality parameters of Karapakkam village such as pH,
EC, TDS, Turbidity, CO3, HCO3, TH, Ca, Mg, Cl, Na, K, SO4 and NO3 for the
years 2000, 2009 were collected from the respective departments. For the year
2010 and 2011, eleven groundwater samples were collected in the domestic
wells from the Karapakkam village during the month of September 2010,
January 2011, February 2011 and March 2011. The well location map is
presented in Figure 3.5. The groundwater quality parameters was analysed in the
laboratory following the standard procedure (APHA 1997) for pH, EC, TDS,
Turbidity, CO3, HCO3, TH, Ca, Mg, Cl, Na, K, SO4 and NO3. The pH, EC and
TDS were measured by using pH meter and conductivity meter, respectively.
Total hardness and calcium hardness were determined by titration with EDTA.
Magnesium hardness obtained from subtraction of total hardness and calcium
hardness. Estimation of alkalinity and chlorides were determined by titrimetric
method. Sulphate and nitrate were estimated by spectrophotometer. Sodium and
Geo referencing and
create Base map
Land use map change
for different periods
Geo referencing
Delineate the land use
changes
Superimposing Map
Village
Map
Image Field visit
and mark
control
points for
the current
year
Survey of India
toposheet No: 66
27
potassium were estimated by flame photo meter and turbidity was measured by
turbid meter.
Figure 3.5 Well Location Map of Karapakkam Village
i) Analysis of water quality index for drinking purposes
The procedure adopted by Landwehr (1974) by developing Water
Quality Index (WQI) to determine the suitability of groundwater. WQI is a very
useful tool for communicating the information on overall quality of water.
The WQI is computed by adopting the following formula,
WQI =
)(1
ii
n
ii pTa (3.1)
Where,
ia - the weight of the ith parameter,
iT - a function that transforms the measured value of ith
parameter into a quality rating,
ip - the measured value of the ith parameter,
28
Based on the WQI values, the groundwater quality are rated as
excellent, good, poor, very poor and unfit for human consumption as presented
in Table 3.1. Based on the above procedure, WQI is calculated for the study
village and checked for its usefulness.
Table 3.1 Categories of Water Quality Indices
Water Quality Index Description
0-25 Excellent
26-50 Good
51-75 Poor
76-100 Very Poor
>100 Unfit for drinking
ii) Generation of water quality index map
The various thematic layers were generated using GIS contouring
methods. The natural neighbourhood interpolation method was used for
generating the contour needed for creation of thematic layer. WQI values for
each sample was calculated using equation 3.1. Based on the WQI values WQI
map was derived in GIS environment.
3.3.6 Groundwater Potential
The groundwater potential was calculated in Karapakkam village.
Water level was monitored from each well. To study the changes in the water
level the procedure followed by Lenters (2001) is also adopted to study the long
term trend of water fluctuation and change in storage. The period taken for the
study is from 2002 to 2010.
29
For determining the temporal variation, the monthly changes in the
water level, ∆L was calculating using equation 3.2.
∆L = Lt+1 – Lt, (3.2)
Where, Lt - Monthly water level of the current month (m)
Lt+1- Monthly water level of the following month (m)
For a particular location, the ∆L will be calculated for all the months of
the year
i) Then the net (annual) ∆L is calculated by summing up the ∆L of
the individual months.
ii) The same procedure is then carried out on the data of the
remaining years i.e. 2002-2010.
iii) Then the ∆L obtain for each month and the net (annual) ∆L is
plotted against month (January, February, and March 2011) from
which a number of striking trends were noticed.
The steps described above to calculate ∆L will be performed using the
Excel spread sheet. Graphs are drawn between the ∆L obtained for each month
and time.
Theissen polygon was created to find out the area corresponding to each
well. Well elevation found out from the GPS survey. Based on the well
elevation, calculate groundwater level. The monthly changes in the water level
∆L were calculating using equation 3.2. Groundwater quantity was calculated
using water level fluctuation method.
30
Groundwater quantity is calculated by water level fluctuation method
adopting the following formula,
Q = A*∆L* Sy (3.3)
Where,
Q = Volume of water (m3)
A = Influence area of well (m2)
∆L= Water level fluctuation (m)
Sy = Specific yield of the well (6% for clayey soil according
to Report of the Groundwater Resource Estimation Committee, 2009).
3.3.7 Livelihood Assessment
Livelihood assessment was analysed based on land use changes,
groundwater quality and groundwater potential. Focus Group Discussion and
questionnaire survey was used to analyse the livelihood changes. Questionnaire
survey is an essential tool, which can give details of actual situation of the study
area. The survey was conduct to study the socio economic impact of
groundwater quality and quantity due to urbanisation and also to understand the
status of groundwater quality and quantity changes. The questionnaire format
has been prepared mainly aiming for a comparison of change of groundwater
quality and quantity in pre and post monsoon over a period of time.
The questionnaire addresses the following aspects:
i) Sources of domestic water including drinking water.
ii) Socio and economic status of the people.
iii) About the groundwater quality and quantity conditions in the
wells.
iv) Uses of well water at different places.
v) Health problem in the area due to urbanisation, land use changes,
deterioration of water quality, drainage facilities, etc.,
31
CHAPTER 4
RESULTS AND DISCUSSION
4.1 GENERAL
This Chapter discusses the results of the analysis carried out on i)
changes in the land use pattern between 2002 and 2010 ii) changes in
groundwater quantity and quality variation over the years and (iii) assess the
livelihood changes due to land use pattern, groundwater quantity and quality
through the focus group discussion and questionnaire survey.
4.2 CHANGES IN LAND USE PATTERN
The static land use / land cover distribution for each study year as
derived from the maps are presented in the Table 4.1. Figure 4.1 to Figure 4.5
shows the land use map 2002, 2004, 2006, 2008 and 2010 respectively.
From this Table 4.1, it is clear that the Residential area was increased
from 4.51% in 2002 and also increased a little to 6.31%, in 2010 it was about
10.4%. The reason was that increase in land value, due to proximity to the city,
induced the conversion of cultivated land as residential plots. In past years,
Karapakkam village is an agriculture oriented village, in 2002, the agricultural
land was 38.1% at that time the area of cultivation was more when comparing
this in 2006 to that of 2008 it was reduced to 30.4% and 7.81%. The reason for
the decline in agriculture was labour scarcity; the landless agricultural labourers
went to the nearby city for want of employment and the land value was raised.
Fallow land was increased from 4.97% in 2002 and also increased a little to
6.78%, in 2010 it was about 36%.
32
Table 4.1 Land use Pattern for the Years 2002, 2004, 2006, 2008 and 2010
Land use categories
2002 2004 2006 2008 2010
Area
(ha)
Area
(%)
Area
(ha)
Area
(%)
Area
(ha)
Area
(%)
Area
(ha)
Area
(%)
Area
(ha)
Area
(%)
Agricultural land 93.24 38.14 80.47 32.92 74.39 30.43 19.10 7.81 0.00 0.00
Aquifer recharge zone 24.59 10.06 24.59 10.06 24.59 10.06 24.59 10.06 24.59 10.06
Fallow Land 12.15 4.97 13.64 5.58 16.56 6.78 70.24 28.73 87.99 35.99
Buckingham canal 10.24 4.19 6.86 2.81 6.86 2.81 5.40 2.21 5.10 2.09
Cemetery 1.85 0.76 1.85 0.76 1.85 0.76 1.85 0.76 1.85 0.76
Collage 1.26 0.52 1.41 0.58 1.41 0.58 1.41 0.58 2.01 0.82
Grass land 7.01 2.87 4.32 1.77 3.29 1.35 2.65 1.08 2.10 0.86
Industries 11.72 4.80 14.22 5.82 14.46 5.91 20.50 8.38 25.22 10.31
Pond 1.17 0.48 1.18 0.48 1.62 0.66 2.43 0.99 1.84 0.75
Residential Area 11.03 4.51 12.82 5.24 15.42 6.31 18.58 7.60 25.52 10.44
School 0.71 0.29 0.71 0.29 0.71 0.29 4.03 1.65 4.03 1.65
Small industries 0.26 0.11 0.35 0.14 0.44 0.18 0.50 0.20 0.55 0.23
Temple 0.74 0.30 0.77 0.31 0.82 0.33 0.86 0.35 0.92 0.38
Total Area 244.48 244.48 244.48 244.48 244.48
32
33
Figure 4.1 Land use Map of Karapakkam village -2002 Figure 4.2 Land use Map of Karapakkam village -2004
33
34
Figure 4.3 Land use Map of Karapakkam village -2006 Figure 4.4 Land use Map of Karapakkam village -2008
34
35
Figure 4.5 Land use Map of Karapakkam village-2010
There is no change in the Aquifer recharge zone and Cemetery.
Regarding the water bodies the Buckingham canal area was reduced from 4.19%
to 2.09%. In 2002, the Industrial area was increased from 4.8% and also
increased 5.91% in 2010 it was about 10.3%. Colleges, schools, and temples
36
were slightly increased. Small industries also slightly increased. Grass land was
slightly reduced.
4.3 GROUNDWATER QUALITY
4.3.1 Temporal Variation of Groundwater Quality Parameters
Groundwater quality parameters were analysed in the laboratory for
four month. Groundwater quality parameters are pH, EC, TDS, Turbidity, CO3,
HCO3, TH, Ca, Mg, Cl, Na, K, SO4 and NO3 for which WHO has prescribed
maximum desirable limits for drinking purpose were analysed. The pH of the
water samples in the study area ranged between 6.0 to 8.0. The desirable limit of
Electrical conductivity was 2000µs/cm. The water quality in Kalaimagal nagar is
within the desirable limit. The concentration of total dissolved solids in most of
the areas exceeds the permissible limits except at Kalaimagal nagar, which has
found to be below 1000 mg/l at all the months.TDS in groundwater also
originate from natural sources, dense residential area, sewage, urban run-off and
industrial wastes. The concentration of Chloride in most of the areas is within
the permissible limits except at Near Okkium Maduvu, Mahatma Gandhi Street,
and Sadagopan Street. High concentration of Total Hardness is found in
Rangasamy street, Indragandhi street and Near Okkium Maduvu. The other
samples showed a moderate range of hardness values which is of common
contamination from dense residential human activities and weathering and
leaching of salts into the groundwater. In all the month, samples shows moderate
range of Sodium and Potassium values which is due to natural geology. The
other parameters like Bicarbonates, Nitrates Sulphates and Turbidity were found
to be within the permissible limits.
4.3.2 Water Quality Index (WQI)
To analyse the groundwater quality changes in the study area, water
quality index was developed. WQI was computed by weighted index method to
37
determine the suitability of groundwater for drinking purpose. The estimated
quantitative values of water quality parameters and their standards are used to
calculate water quality index using equation 3.1. The WQI calculated by
Landwehr (1974) was used for assessing the suitability of groundwater for
drinking purposes, which is found to be more appropriate for the current study.
Based on the procedure as explained earlier, indices were calculated for the
month of September 2010, January 2011, February 2011 and March 2011. The
calculated Weighting factors (ai) are shown below in Table 4.2.
Table 4.2 Water Quality Parameters, BIS Standards and Weighting
factor (ai)
Parameters BIS Standards Weighting factor (ai) pH 8.5 0.24
TDS (mg/l) 500 0.0041 Turbidity (NTU) 50 0.41
HCO3 (mg/l) 500 0.0041 Ca (mg/l) 75 0.027 Mg (mg/l) 30 0.0681 Cl (mg/l) 250 0.0082 Na (mg/l) 200 0.0102 K (mg/l) 20 0.102
SO4 (mg/l) 250 0.0082 NO3 (mg/l) 45 0.045
It is inferred that, during the month of January 2011 in most of the
places the quality of water seems to be good compared to other months. During
September 2010, February 2011 and March 2011 few places of poor quality
water are identified. The Water quality classification is done based on the WQI
of September 2010, January 2011, February 2011 and March 2011 and presented
in Table 4.3.
38
Table 4.3 Water Quality Classification based on WQI of September 2010, January, February and March 2011
ID Name Latitude and Longitude
WQI (Sep)
WQ Rating
WQI (Jan)
WQ Rating
WQI (Feb)
WQ (Rating)
WQI (Mar)
WQ Rating
Well 1 Renganathan street
12° 55' 14.74"N, 80° 13' 51.09"E 95.8 Very
poor 61.84 Poor 113 Unfit for drinking purposes
125 Unfit for drinking purposes
Well 2 Near Okkium Maduvu
12° 55' 7.07"N, 80° 14' 2.33"E 141
Unfit for drinking purposes
77.31 Very poor 112
Unfit for drinking purposes
121 Unfit for drinking purposes
Well 3 Indragandhi street
12° 55' 1.01"N, 80° 13' 55.37"E 63.6 Poor 42.73 Poor 93.3 Very Poor 99.8 Very
Poor
Well 4 Kupusamy street
12° 54' 54.04"N, 80° 14' 2.15"E 62.9 Poor 56.3 Poor 66.8 Poor 69.6 Poor
Well 5 Kalaimagal nagar
12° 54' 48.69"N, 80° 14' 4.60"E 54.7 Poor 42.4 Good 49.4 Good 56.8 Poor
Well 6 Government well
12° 54' 50.47"N, 80° 13' 55.19"E 52.3 Poor 49.3 Good 58.8 Poor 62.3 Poor
Well 7 Muthamil nagar
12° 54' 54.05"N, 80° 13' 42.17"E 100 Very
poor 82.7 Very poor 93.78 Very Poor 101
Unfit for drinking purposes
Well 8 Mahatma Gandhi street
12° 54' 43.34"N, 80° 13' 48.06"E 45.3 Good 32.4 Good 42.9 Good 56.2 Poor
Well 9 Vendraai amman kovil steet
12° 54' 42.43"N, 80° 13' 56.11"E 87.6 Very
Poor 64.3 Poor 91.46 Very Poor 99.3 Very Poor
Well 10 Rangasamy street
12° 54' 41.55"N, 80° 14' 2.15"E 73.5 Very
Poor 62.6 Poor 71.8 Poor 76.8 Very Poor
Well 11 Sadagopan street
12° 54' 37.63"N, 80° 13' 58.22"E 49.8 Good 39.34 Good 43.1 Good 49.6 Good
38
39
Hence the quality of water samples in the study area was found to vary
from good to very poor in the January 2011 and good to unfit for drinking
purposes in the September 2010, February 2011 and March 2011. In January
2011, it was found that water quality in general, related to quantum of rainfall
received, in good. The improvement in groundwater quality, during this month
may be due to the rainfall in the previous month. This may have an impact on
the dilution of salts.
4.3.3 Generation of Water Quality Index Map
Water quality index values revealed that the groundwater at two wells
were good quality with the WQI ranging in between 0-50 and therefore can be
used for human consumption. Four samples were having poor quality with WQI
ranging between 50-75 and three samples were having very poor quality and
cannot be used for domestic purposes. The WQI was found to be above 100 in
areas like Near Okkium Maduvu and Renganathan Street. These two well has
heavy contamination. The municipal solid waste were dumping in pallikaranai
area. The leachats from this area have seeped though the soil and contaminated
the nearby wells. Okkium Maduvu well is locate from the nearby Pallikaranai
swamp water was passed through the Okkium Maduvu to reach the Buckingham
canal. The WQI map is shown in Figure 4.6, Figure 4.7, Figure 4.8 and Figure
4.9.
40
Figure 4.6 Water Quality Index Map-September 2010
Figure 4.7 Water Quality Index Map-January 2011
41
Figure 4.8 Water Quality Index Map-February 2011
Figure 4.9 Water Quality Index Map-March 2011
42
4.4 GROUNDWATER POTENTIAL
4.4.1 Analysis of Water Level
Table 4.4 shows that the water level in government well has a maximum
depletion of 0.87 m below ground level (BGL) in the pre-monsoon of 2002 and
0.15 m, (BGL) in post-monsoon. In 2006, the depth to water level was 2.15 m,
(BGL) in the pre-monsoon and in the post-monsoon it was 1.25 m, (BGL). In the
month of March 2011 the water level has a maximum depletion of 3.8 m, (BGL)
and in the February 2011, the water level has decreased to 10.5 m, (BGL). The
reason for the lower levels in a well may be due to the indiscriminate pumping
over extraction of groundwater. The change in storage was calculated based on
the water level fluctuation method using GEC norms (eqn. 3.2). Figure 4.10
shows that the water level fluctuation during January 2011 to March 2011 in the
study area. Figures 4.11 to 4.13 show the spatial distribution map of water level
variation.
Table 4.4 Water Level Data for the Years 2002 and 2006
Period Pre monsoon in ( m ) Post monsoon in ( m ) 2002 0.87 0.15 2006 2.15 1.25
Figure 4.10 Water Level Fluctutation (m)
43
Figure 4.11 Water level Contour-January 2011
Figure 4.12 Water level Contour-February 2011
44
Figure 4.13 Water level Contour-March 2011
From the water level contour map, the groundwater flows were
identified. The groundwater movement was northwest dirction to southeast
direction. Because Renganathan street, Okkium Maduvu, Indragandhi Street has
higher level and Rengasamy street lower level. Mahatma Gandhi street and
Muthamil nagar has higher level than Kupusamy street, Sadagopan Street,
Government well and Kalaimagal nagar.
4.4.2 Groundwater Quantity
Groundwater quantity was estimated by adopting the water level
fluctuation method using equation 3.3. Area of influence was calculated by using
Theissen polygon method and shown in Figure 4.14. Figure 4.15 shows the
groundwater quantity for the month of February and March 2011. The change in
groundwater storage for January 2011 to February 2011 was shown in Table 4.5.
45
Figure 4.14 Theissen polygon map
Figure 4 .15 Groundwater Quantity(m3)
46
Table 4.5 Groundwater quantity for January and February 2011
Well No Name Latitude and Longitude Area (m2) Change in Water Level (∆L) (m) Groundwater Potential (m3)
Jan Feb Jan-Feb Feb-Mar
Well 1 Renganathan street
12° 55' 14.74"N, 80° 13' 51.09"E 290200 -0.75 -1.25 -13059 -21765
Well 2 Near Okkium Maduvu
12° 55' 7.07"N, 80° 14' 2.33"E 512100 -0.7 -1.05 -21508 -32262
Well 3 Indragandhi street
12° 55' 1.01"N, 80° 13' 55.37"E 128700 -0.6 -0.75 -4633.2 -5792
Well 4 Kupusamy street 12° 54' 54.04"N, 80° 14' 2.15"E 126600 -0.7 -1.15 -5317.2 -8735
Well 5 Kalaimagal nagar
12° 54' 48.69"N, 80° 14' 4.60"E 589300 -1.1 -1.35 -38894 -47733
Well 6 Government well
12° 54' 50.47"N, 80° 13' 55.19"E 81570 -1.2 -1.6 -5873 -7831
Well 7 Muthamil nagar 12° 54' 54.05"N, 80° 13' 42.17"E 213100 -1.1 -1.45 -14065 -18540
Well 8 Mahatma Gandhi street
12° 54' 43.34"N, 80° 13' 48.06"E 125700 -0.9 -1.05 -6787.8 -7919
Well 9 Vendraai amman kovil steet
12° 54' 42.43"N, 80° 13' 56.11"E 48840 -0.8 -1.2 -2344.3 -3516
Well 10 Rangasamy street
12° 54' 41.55"N, 80° 14' 2.15"E 275900 -1.3 -1.9 -21520 -31453
Well 11 Sadagopan street
12° 54' 37.63"N, 80° 13' 58.22"E 43930 -0.9 -1.3 -2372.2 -3427
Note: -ve sign indicate the water level depletion
46
47
Analyzing the reasons for the fluctuation in the water level, it was found
that urbanization in the recent years is one of the reasons for the decline. Due to
the increase in impervious layers, paved areas and induced changes in land use
causing compaction of the top sub-soil, the natural rainfall recharge has very
much reduced.
Thus, it could be inferred that in the recent years, in spite of the good
amount of rainfall, the water level position has not increased substantially
indicating that the surplus rainfall would have gone as waste in the form of
runoff. The rapid increase in urban development, the demand for water has
increased in many told. Hence the groundwater potential is under a great threat,
and it has to be protected. The construction of rainwater harvesting structure will
increase the water level and also controlling the over extraction of water, may
improve the water level.
4.5 LIVELIHOOD ASSESSMENT
The questionnaire survey and Focus Group Discussion was conducted
with the people living in the Karapakkam village. It was conducted to determine
the reasons for water quality variation in the village. The data were obtained in
terms of employment, income, age group, housing type, year of living on the
village, source of drinking water and health impact. The obtained data were
analysed with the help of Microsoft excel. From the analysis, statistical data
results were obtained which are given below. Sample size of the study is 53 in
which 42% of people were living in rented house and 58% of people living in
own house.
4.5.1 Source of Drinking Water
Figure 4.16 shows the sources of drinking water in present status. In
2002, the sources of drinking water were well water and pond water. In 2010,
the sources are well water, Panchayat water, portable water and collecting water
48
from Sholinganallur and Nellur villages. There is a drastic change in the group
of people using well water for drinking from 2002 and now. 76% of the
respondents were used well water for drinking purpose in 2002 and it is reduced
to 4% in 2010 because of the groundwater quality deterioration. The septic tanks
are constructed near to their wells, so the groundwater gets polluted and unfit for
use. In 2002, portable water is not used for drinking purpose, but now 51% of
the respondents used portable water. Presently, almost 13% of the respondents
are using the Panchayat water for drinking and they are boiling the water only
during the monsoon season. Figure 4.17 Shows that the amounts spend for
drinking water.
Figure 4.16 Sources of Drinking Water Figure 4.17 Amounts spend for
Drinking Water
4.5.2 Analysis of Groundwater Quality
From the questionnaire survey, the groundwater quality data were
collected on four different categories namely Excellent, Good, Moderate Poor
and Very Poor. The data were analysed in GIS software at specially for all the
observation well during 2002, 2005, 2010. From the people observation, before
2005, mostly the well water was excellent and good. After 2005, the quality of
the water gets too deteriorated.
49
The reason for the quality deterioration was extraction of more water,
lack of improper drainage system and natural geology. Figure 4.18 shows the
reason for water quality deterioration. Figures 4.19 to 4.21 show the water
quality map for the years 2002, 2005 and 2010 respectively.
Figure 4.18 Reasons for Water Quality Deterioration
Figure 4.19 Water Quality Map for 2002
50
Figure 4.20 Water Quality Map for 2005
Figure 4.21 Water Quality Map for 2010
51
From the rating of water quality map, it is inferred for that Renganathan
street, Near Okkium Maduvu and Muthamil nagar wells, the water quality was
very poor. The trend of change in water quality for both calculated water quality
index map and from people’s response map on water quality are similar. Hence
this study has given very good opinion about the people’s understanding of
groundwater in this area.
4.5.3 Agricultural Status
In the past, 42% of respondents had own agricultural land and involved
in agricultural activities, but 34% of respondents work as a agricultural
labourers. In present year no agricultural practise were done. But urbanisation
has turned these agricultural lands into built-up area and fallow land thus
affecting the livelihood of the people who were dependent on agriculture. The
reason is that the agricultural labourers moved to other places for jobs, as they
are getting more income on non-agricultural jobs which resulted in labour
scarcity and wage rise. The land and house owners have rented out their
properties to the employers of IT companies, making huge income, which in turn
is improving their living standards. Figure 4.22 shows the agricultural status of
the study area.
4.5.4 Economic Status
As seen in Figure 4.23, among people of different income groups, 13%
of the people, who earn low income (< Rs.5000) are mostly affected by
urbanisation. Earlier they were working as an agricultural labourer. In this study
it is found that 21% of the people earned high income due to IT companies, petty
shops and hotels.
52
Figure 4.22 Agricultural Status Figure 4.23 Economic Status
4.5.5 Sanitation and Health Status
Based on the response, in the year 2010, arround 69% of residents have
sanitation facility. Figure 4.24 shows the sanitation facility status and Figure 4.25
shows the health impact of people’s in Karapakkam. Figure 4.26 shows the
major problems faced by the people due to water stagnation such as health
disease. In this 64% of people are highly affected by health problem and 36% of
people are not affected. Out this 64%, 54% of residents are affected by cold,
33% of residents were affected by fever and 13% of residents were affected by
skin disease such as allergy, psoriaris etc.,
Figure 4.24 Sanitation Facility Status Figure 4.25 Health Impact
53
Figure 4.26 Major Health Problem
4.5.6 Impact of Urbanisation
i) Positive Impacts
The positive impacts from many people are,
a) Some of them joined in good jobs.
b) Few have their own petty shops and hotels.
Due to IT companies most of the people was benefited. Some of the
people were working in Housekeeping, construction labourer, Bottle Company,
Lathe works and catering etc., People has a sense of awareness towards
education, due to IT companies. Also land value is increased in recent years,
because of the demand for land. The land and house owners have rented out their
properties to the employers of the IT companies and making huge income, which
in turn is improving their living standards.
The land owners sold out the land completely and welcome urbanisation
because the faith in agriculture is decreased and they feel that it might bring
benefits to the next generation. During the discussions with women from the
54
land owning families, it was noticed that they were tempted towards urbanisation
and wanted to move out of agricultural, considering it as inferior job. Increasing
land price and urban style make them comfortable with increase in urbanisation.
ii) Negative Impacts
Most of the agricultural land was sold to IT company and some of the
lands were converted to fallow land. Previously the landless agricultural
labourers dependent only agriculture. Now they shifted to other jobs in the
industries, construction works etc., 13% of the people were unemployed with
comparatively lower living standard. In groundwater condition, Groundwater
level gets decrease due to over extraction of groundwater. Groundwater quality
also varied due to over extraction and improper drainage. During rainy reasons
stagnation of water is more prevalent and causes among the people health
problems.
55
CHAPTER 5
SUMMARY AND CONCLUSION
5.1 SUMMARY
The impact of urbanisation on groundwater in Karapakkam village is
carried out in many aspects to finding the changes in land use pattern,
groundwater condition due to urbanisation and to assessing the livelihood
changes. Actually livelihood is comprises of capabilities, assets (including both
material and social resources) and activities required for a meaning of living.
The livelihood of people is often disturbed / changed due to the developments in
the environment.
The urbanisation status of village was found by considering the changes
in the land use pattern, between the years 2002, 2004, 2006, 2008 and 2010. By
using the water quality indices the spatial variation of drinking water quality was
found. Water level data were collected for January, February and March 2011 to
analyse the changes in the water level. Also the questionnaire survey was
conducted to the villager’s to assess the livelihood changes in occupational
characteristics, agriculture, water level and water quality before and after
urbanisation. These primary data were analysed using Microsoft Excel and GIS
software. The livelihood changes were discussed in various aspects to quantity
the effects.
56
5.2 CONCLUSION
The present study gives an overall view of the status of urbanisation and
water resources in Karapakkam village and also it gives various details about the
impacts of urbanisation on livelihood option. Due to urbanisation, the land use
pattern was changed over the decades. In 2002, 38% of land was used to
agricultural purposes. January 2010 most of the land was sold to corporate and
Real estate companies, which have been converted in to IT company and
residential areas. Due to this rapid development the demand for land has
increased and all the agricultural lands are converted into urban development.
Also the land value has increased alarmingly to many told in the last two
decades. Some lands were converted to fallow land due to shortage of irrigation
water source. As of now (2010) agricultural land was no move in Karapakkam
village. Industrial area and residential area was increased from 4.8% to 10.3%
and 4.51% to 10.4% in 2002 and 2010 respectively. But in other way, due to
urbanisation, 21% of people’s are earning more than Rs.10000.
Regarding the water quality and water level, it could be inferred that
earlier the village had appreciable groundwater potential and the quality of
groundwater was good for domestic purposes. But the water resources are
declining day by day in terms of water level and also deteriorating in quality.
Water Quality Index, questionnaire survey and focus group discussion was used
to classify the well. From the classification Okkium Maduvu and Renganathan
street well was unfit for drinking purposes, where the water quality index was
found to be more than 100. The reasons attributed for the quality deterioration
were over extraction and lack of proper drainage system. The decreasing
availability of water coupled with pollution will result in acute scarcity of good
quality water in the area.
Due to the groundwater quality deterioration, 51% of people are using
portable water for drinking purpose and 18% of people spend more than
57
200 rupees per month for buying portable water. Groundwater stagnation was a
major problem due to improper drainage and impervious layer, which causes
health problem. It is arrived from the questionnaire that 66% of people’s are
affected health disease such as fever, cold and skin disease. From the economic
status 66% and 21% of people’s are living under good and moderate status.
There are 13% of the people, who are mainly depends and work as an
agricultural labourer in this area. Their livelihood was affected by urbanisation
and no agricultural activities. The monthly income they earn is below Rs.5000.
This study has been carried out and analysed on detail about the rapid
urbanisation and techno economical aspects. Few important points raised by the
people during the questionnaire survey and considered in the management of
reasons effectively in an urban environment are given below.
i) Urbanisation is a major challenge for water resources. Planned
urbanisation gives positive impacts, but unplanned urbanisation
creates more problems and complicates the situation, which in fact
give more negative impacts.
ii) Awareness must be created among the people about the
urbanisation, over extraction of water and sanitation to conserve
the water resources.
iii) It is learned that most of people doesn’t have enough knowledge
about septic tank, disposal of sewage in water bodies and their
advantages.
iv) The people depends on agricultural labour are asking for some
other water source to encourage agriculture, but it seems to be
impractical for the present scenario.
58
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61
ANNEXURE
QUESTIONNAIRE FOR MEASURING THE LIVELIHOOD
CHANGES DUE TO URBANISATION
General information
1. Person identification:
i) Name:
ii) Address:
2. Respondent profile:
i) Sex: Male Female
ii) Age -
3. Monthly income detail:
a) <5000 b) 5000-10000 c) 10000-15000 d) >15000
4. Family education and occupation status
Family members Education Occupation
Name Relation
5. Ownership of house:
a) Owned b) Rented c) Living with relative
62
6. How long are you living in this house?
Groundwater Condition
7. Did you find any changes in ground water condition early and now?
(Yes/No)
i) If yes, what are the change occurred? (specify year and reason also)
1. Ground water level __________________________________
_________________________________________________
2. Ground water quality ________________________________
_________________________________________________
8. Is there any remarkable change in quality of ground water during peak
summer? (Yes/No)
i) If yes, what are the changes? ______________________________
9. Domestic water sources
Purpose Source
Own well Panchayat water Cane water
Drinking
Cooking
Bathing
Washing
Gardening
Cleaning
10. Do you have own well? (Yes/No)
i) If yes, when did you construct the well?
1. What is the depth of well?
2. Well water condition and usage of well
63
Periods
Well water condition
(Very good, Good, Moderate, Bad,
Very Bad)
Well water
usage
Early ( )
Now ( )
3. If well water is not sufficient, what is the alternate source?
ii) If No, what is the source of domestic water?
11. What is the source of Panchayat water supply?
12. Availability of Panchayat water
i) Frequency _____________
ii) Quality _______________
13. How you are getting the Panchayat water?
a) Own connection b) Public connection
i) If the tap is public, how far from your house? (specify in metres or
kilometres)
14. How much time you are spending for collecting the water?
15. How much money do you spend to purchase can water (monthly)?
Sanitation Facility
16. Do you have toilet facility? (Yes/No)
i) If yes, whether you are using owned/public toilet?
a) Own toilet b) Public toilet
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1. If you have own toilet, what type toilet facility
a. Pit toilet b. Flush toilet
ii) If no, what is your defecation practice?
17. How frequently you are cleaning the toilet?
18. What type of sewage collection system do you have?
a) Lined septic tank b) Unlined septic tank
19. How far the septic tank is located from your well? (specify in metres)
20. Is there any solid waste collecting system in your area? (Yes/No)
i) If yes, how will collect? (specify frequency)
ii) If no, how do you dispose the solid waste?
Health Problem
21. Is there any health problem due to ground water? (Yes/No)
i) If yes, what are the problems? ________________________________
22. Is there any disease frequently affect your family? (Yes/No)
i) If yes, specify type of disease ________________________________
23. Are you getting any health support through Primary Health Centre?
(Yes/No)
i) If yes, what are the supports?
Economic Status
24. Any changes occurred in your occupation? (Yes/No)
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i) If yes, what are the changes?
1. Early__________________
2. Now __________________
25. Did you modify your house? (Yes/No)
i) If yes, what type of modification?
_______________________________________________________
Agricultural Status
26. Did you involved in agricultural activates? (Yes/No)
i) Early ___________________
ii) Now ___________________
27. What are the types of crops cultivated?
i) Early___________________
ii) Now __________________
iii) What type of fertilizer you used/using? (Organic/Inorganic)
28. If you are not involved in agricultural activities? (specify the
constraints)__________________________________________________
__________________________________________________________
29. Is the land value increases in this village?
i) If yes, how much? (Sq.ft)
1. Early__________________
2. Now __________________