Delineation and Evaluation of Subsurface Water …•The standard reasoning is that even after...
Transcript of Delineation and Evaluation of Subsurface Water …•The standard reasoning is that even after...
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DirectorCentre for Water Management & Research University of Rajasthan,
Jaipur-302004, India Email: sinha_1415@ hotmail.com, [email protected]
Delineation and Evaluation of Subsurface Water Storage to Cope up with the Climatic Variability and Change : Case Studies From Arid to Semi Arid Region Of Western India.
Professor A. K. Sinha
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Evolution of World Water Shortage in 100 Years
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Indus
River Basins- River Basins- Water stress and water scarcityWater stress and water scarcity
GangaSub-basin
Brahmaputra Sub-basin
Inland Drainagein Rajasthan
MahiWest Flowingrivers of Kachch and Katiawar
Stress <1700 m3 / per/yrScarce <1000 m3/per/yr
NarmadaTapti
Sabarmati Godavari
Mahanadi SubernarekhaBrahmani-Baitarani
West-flowingrivers from Tapi to Tadri
West-flowingrivers from Tadri to Kanyakumari
East-flowingrivers between Pennar &Kanyakumari
Cauvery
Eest-flowingrivers between Mahanadi & Pennar
Krishna
Pennar
Occasional water problem
Water stress
Water scarcityAbsolute scarcity
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1986 1988 2000 2003
Floods in India and its impacts
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100 300 500 700
Precipitation in mm
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Recharge in mm
Western India- Hydrological extremes
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…… …… ContdContd
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Rainfall- Water level-Draft trend
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Climate Change-Challenges & Opportunities in Arid zone
Climate change is now a reality .
Arid zone must recognise and react to the reality
Need to Adapt to the consequences of Climate Change or to Mitigate the causes of it
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Floods in Western India
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1984
1986
1997
2000
2001
2002
Temporal-spatial spread of drought &
impacts
Drought is occurring in some or the other part of the country
Primary impacts: water availability, agriculture production, hydropower generation
Secondary Impact: Agricultural GDP dips, increase in commodity prices, livelihood of people dependent on rainfed farming (marginal farmers & farm laborers surviving) affected
Rainfed areas (61%) – most affected
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Needs for Enhanced Storage •Need of sufficient storage capacity under growing water demands and increasing climate variability …….Tuinhof A, Olsthoorn T, Heederik JP, de Vries J . : 2005: Groundwater storage and water security: making better use of our largest reservoir , Water Sci Technol. 2005;51(5):141-8.
•A key feature of some aquifers and ground-water systems is the large volume of ground water in storage, which allows the possibility of using aquifers for temporary storage, that is, managing inflow and outflow of ground water in storage in a manner similar to surface-water reservoirs .Even if 8 percent of the 33,000 km3 (Postel 1999) floodwater that runs off to the oceans annually recharge the groundwater, we have a renewable supply of over 2,500 km3 of groundwater annually—which seems several times more than the world uses today. Postel, Sandra. 1999. The pillars of sand: Can the irrigation miracle last? Washington: The Worldwatch Institute 1999)http://www.isnar.org/iwmi/pubs/WWVisn/GrWater.htm - _ftn3
•The standard reasoning is that even after 800,000 big and small dams around the world, the reservoirs can capture and store no more than a fifth of the rainwater, the bulk of the remainder still running off to the seas. India has built more than its share of the world’s dams but 1,150 km3 of its rainwater precipitation still run off to the seas annually in the form of "rejected recharge" (INCID 1999) INCID (Indian National Committee on Irrigation and Drainage). 1999. Water for food and rural development 2025. Paper presented at the PODIUM workshop,
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Major Objective
Understanding Subsurface Storage Potentialities in Palaeochannel and Ephemeral River basin –Semiarid to Arid region of Western India
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Sustainable management of groundwater resources
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Rann
Mohenjo-daro
Jaisalmer
Jodhpur
GanweriwalaBanawali
Dholavira Surkota
da Source:RRSC,Jodhpur
Palaeodrainage –Excellent Storage for Groundwater
(Sinha & Raghav 2003)
Palaeodrainage in Indian Desert Region- IRS P3 WiFS Image
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HYDROGEOLOGY
Aquifer Area (sq. km)
Percentage of total area
Younger alluvium
121.18 11.10
Older alluvium
877.92 80.38
Quartzite 89.97 8.24
Depth to water level 13.55 – 61.10 m
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Number of boreholes :12
Depth of drilling :60 – 125 m.
Thickness of alluvium :78 – 102 m.
BasamentMalani granite
Depth to water level35 – 55 m.
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GROUND WATER LEVEL BEHAVIOUR
Depth to water level :13.55 – 61.10 m.
In major part between 30 and 50 m
Southern and southeastern partshallow i.e. < 35 m
Central partdeeper i.e. 35 – 60 m
Northern part45 – 55 m
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Alluvium : 1.04 m/year
Quartzite : 0.34 m/year
Decline in water level (1997-2006)
Decline in water level (1987-2006)
Alluvium : 0.66 m/year
Quartzite : 0.21 m/year
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CHEMICAL QUALITY
The ground water is fresh and
potable in major part of the area.
EC: 500 – 1500 micromhos/cm at
25° in major part of the area.
EC:1500 –5091 micromhos/cm at
25° in north western part.
Chloride: 35 – 1118 ppm.
Concentration of salts increases
in the direction of flow of Kantli
river from south to north direction.
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Ground elevation - 370 – 290 m amsl.
Thickness of alluvium - 69 – 102 m.
Basement - Malani granite
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Ground elevation - 319 - 325 m amsl.
Thickness of alluvium - 85 - 100 m.
Basement - Malani granite
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Aquifer Storage Space
Pot. Pot. ZoneZone
Pot.Zone Pot.Zone area area
(sq.km.)(sq.km.)
Average Average depth to depth to
water water level level
below below 3m 3m
(Post (Post 06)06)
Aquifer Aquifer thicknethickness (m)ss (m)
Sp Sp Yield Yield (%)(%)
Storage Storage space in space in aquifer aquifer (MCM)(MCM)
Non Non aquifer aquifer saturatesaturate
d d thicknesthicknes
s (m)s (m)
Sp Sp Yield Yield of non of non aquifeaquifer (%)r (%)
Storage Storage space in space in
non non aquifer aquifer (MCM)(MCM)
Total Total storage storage space space
available available (MCM)(MCM)
AA 121.18121.18 31.8331.83 7.967.96 0.120.12 115.75115.75 23.8723.87 0.0120.012 34.7134.71 150.46150.46
AoAo 877.92877.92 50.2250.22 12.5512.55 0.10.1 1101.781101.78 37.6737.67 0.010.01 330.71330.71 1432.501432.50
QQ 89.9789.97 16.316.3 16.316.3 0.0150.015 21.9921.99 -- -- -- 21.9921.99
1089.071089.07 36.8136.81 1239.531239.53 61.5461.54 365.42365.42 1604.961604.96
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Artificial Recharge To Ground Water
To augment the depleted ground water resources, rain water harvesting
and artificial recharge to ground is very effective in supply side
management of ground water resources.
Average annual rainfall : 465.5 mm.
Rain water run off planned for artificial recharge (5%) : 21.9219 MCM
AquiferAquifer Area Area (sq.km)(sq.km)
Volume Volume of water of water (MCM)(MCM)
Efficiency Efficiency (%)(%)
Water to Water to be be
recharged recharged (MCM)(MCM)
Percolation Percolation TankTank
Dug well Dug well rechargerecharge
Recharge Recharge Pit/RTRHSPit/RTRHS
Volume Volume (MCM)(MCM)
NoNo Volume Volume (MCM)(MCM)
NoNo Volume Volume (MCM)(MCM)
No.No.
AA 121.18121.18 2.43432.4343 0.90.9 2.19092.1909 1.31451.3145 44 0.65730.6573 329329 0.21910.2191 577577
AoAo 877.92877.92 17.657717.6577 0.90.9 15.891915.8919 9.53529.5352 3232 4.76764.7676 23842384 1.58921.5892 41824182
QQ 89.9789.97 1.82991.8299 0.90.9 1.64691.6469 0.98810.9881 33 0.49410.4941 247247 0.16470.1647 433433
TotalTotal 1089.11089.1 21.921921.9219 2.72.7 19.729719.7297 11.837811.8378 3939 5.91895.9189 29602960 1.97301.9730 51925192
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Major Objective Interfacing Fresh-Saline Groundwater Zone & Recharge Estimation
Groundwater & Saline Area Management
Case Studies - II
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• About 23% of formation water available in Rajasthan is saline in nature.
• Generally in saline areas, a thin cushion of potable water floating on the saline water is withdrawn for drinking and other use.
• Rajasthan accounts of 49% of villages facing groundwater salinity and 56% of villages with Fluoride contaminated groundwater in India.
Origin of Problem
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Need For Saline Pockets Investigation
The saline zones in this dry state of India are quite prominent but so small that they are not reflected even on district level hydrogeological maps.
The occurrence of well-defined saline pockets within fresh water region warranted the need to take up systematic micro level hydrogeological investigations to understand the precise hydrogeoloical set up of the saline aquifer and its development
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Water Resources Potable water Poor quality water
Potential zone area (km2) 220169.06 97673.13
Net annual groundwater availability (mcm) 10382.5781 3104.0937
Existing gross groundwater draft for irrigation
(mcm)
11599.0104 487.6452
Existing gross groundwater draft for domestic
and industrial use (mcm)
139.1914 13.29
Existing gross groundwater draft for all uses
(mcm)
12991.2018 500.9352
Allocation for domestic and Industrial
requirement as on year 2025 (mcm)
2719.7713 -
Net groundwater availability for future irrigation
development (mcm)
-3936.2036 -
Present groundwater balance (mcm) -2608.6237 2603.1586
Stage of groundwater development (%) 125.13 16.14
The Dynamic Potable and Saline Water Resources of Rajasthan
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Study area
parallels 27015’ – 27030’ and meridians 7505’ – 75020’
Study AreaStudy Area
720 km2( SOI Topo-sheet nos.
45M/3 & 45M/7)
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Physiography & Drainage
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83 VES of Schlumberger array were interpreted: Q’, ‘H’, ‘HK’, ‘HKH’ and ‘KH’ type curves are
encountered in the area. ‘A’ type curve is not represented in the area. ‘Q’ type curves are noticed in saline formation water
areas. ‘H’ type curves are noticed in hard rock areas.
The potential areas are represented by ‘HKH’ and ‘KH’ type curves.
‘HK’ type curves indicate presence of finer clastics and deterioration of groundwater quality with depth.
Geo Electrical Resistivity SoundingGeo Electrical Resistivity Sounding
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Representatives Schlumberger VES Type Curves of Study Area
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An approximate estimate of groundwater recharge on construction of the contour trench can be made as follows:
Mean annual rainfall (1974-2006) : 488.8 mm Catchment area of ridges and hillocks : 120 km2
Rainfall run-off co-efficient of rocky terrain : 0.5 Groundwater Recharge component : 0.5
Monsoon run-off available for groundwater recharge:Area* Mean annual rainfall* Run-off co-efficient* Recharge
component
120* 1000* 1000* 0.488* 0.5* 0.5 = 14640000 cubic meter/yea or 14.64 million cubic meter/year
Estimate of Groundwater Recharge
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MAR MAY HELP IN REDUCING THE GLOBAL WARMING
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Potential of MAR for Energy savings , reduction of Green house gases & resultant Carbon credits….
Dominant contribution to energy production in Western India is from Thermal Power Plants
The enormous quantum of power saved will reduce the Green house Gas (GhG) emissions
Reduction in GhG to contribute towards reducing the global warming.
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Potential of MAR for Energy savings , reduction of Green house gases & resultant Carbon credits
Gross Ground water draft :2415MCM/annum Wells with electric connections :1,31,414 Dynamic head : 25-100 m Lifting 1 m3 of water by one meter : 0.01 kWh Lifting 2415 MCM needs nearly 1550 Million
kWh of electricity under present situation Energy cost Rs.5347.5 Million (considering
the cost of power delivered @ Rs 3.45 /kWh)
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Potential of MAR for Energy savings , reduction of Green house gases & resultant Carbon credits..
MAR on full scale implementation would reduce average dynamic head
Reduction by 10m :Saving 258 Million kWh of power valued at Rs 888 Million
Reduction by 20m :Saving 515 Million kWh of power valued at Rs 1775 Million
Reduction by 30m :Saving 775 Million kWh of power valued at Rs 2670 Million
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Potential of MAR for Energy savings , reduction of Green house gases & resultant Carbon credits….
The potential for carbon credits due to reduction in power consumption has been computed by considering the Average coefficients as followed in the USA.
Carbon dioxide = 1.34 lb/kWh
Methane = 0.0111 lb/kWh
Nitrous oxide = 0.0192 lb/kWh
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Potential of MAR for Energy savings , reduction of Green house gases & resultant Carbon credits….
The saving of 775 Million kWh of power implies saved emissions of GhG as follows:
Carbon dioxide = 1038.5 Million lb or 4,71,188 Metric tons ( 1 metric ton =2204 lb)
Methane = 8.6 Million lb or 3902 Metric tons Nitrous oxide = 14.9 Million lb or 6760 Metric tons At the @ US $ 10/metric tonne of carbon dioxide ,
the carbon saving would be worth US $ 4.7 Million or Rs 211 Million/year.( considering 1US $= Rs 45)
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In conclusion …
“If society continues to use precious groundwater resources without recompense or replenishment, the water (management) crisis will only deepen”
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The Water Which Came Down From Heaven ..Those Spring Up Their Own.The Bright And Pure Water That Finally Reaches The Sea .May These Divine Water May Protect Me
• Rigveda ( Vii-49-2)
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Thank you