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International Journal of Innovative Research in Advanced Engineering (IJIRAE) ISSN: 2349-2163
Volume 1 Issue 6 (July 2014) http://ijirae.com
__________________________________________________________________________________________________
© 2014, IJIRAE- All Rights Reserved Page - 83
Ground Water Quality Analysis for construction of Part of
Mumbai Metropolitan Region (MMR)
James S. Main Pushpam.K.V
Associate Professor, Civil & Environmental Engg, VJTI PG Student, M. Tech. Environmental Engg, VJTI
Abstract: Groundwater quality in the study area has been analysed in the present work. For this study, a part of Mumbai
Metropolitan Region were selected which covers almost the entire area. Fifteen water samples, from various bore wells
covering the study area during post monsoon season 2013 were collected to find out the values of different parameters in the
groundwater so as to check the suitability for construction. The tests for different parameters like, chloride, Sulphates,
suspended solids, Inorganic material, organic material, limits of acidity and, limits of alkalinity were performed by using
Standard procedures and the results were compared with IS456 guidelines. All samples, except two (In Virar and Vasai’ where
sulphate’ content was more than 1600 mg/l.) are suitable for construction. Samples from ‘Old Panvel’, ‘Virar’ and
‘Nalasapora’ were tested for the suitability for irrigation also, since the ground water is used for irrigation in those areas. The
important parameters affecting for irrigation purposes are: Electrical Conductivity (EC), Sodium adsorption ratio (SAR),
Sodium percentage (Na %) and Residual sodium carbonate (RSC). All the parameter values were within the permissible range,
hence the ground water from the said areas is suitable for irrigation.
Key words. Electrical Conductivity, Sodium adsorption ratio, Sodium percentage and Residual sodium carbonate.
I. INTRODUCTION
Of the available global water supply, 97.2% is saline water in oceans. This water is unsuitable for drinking or
agricultural uses. 2.14% is in ice caps and glaciers, 0.61% is groundwater. Much of this water is too deep for extraction.
0.009% is found in surface water. This is where most drinking water comes from.0.005% makes up soil moisture.0.001%
of water is found in the atmosphere (10).Rapid urbanization, growing population and speedy industrialization have led to
the pressure on demand for water. Ground water is used for domestic, industrial and irrigational purposes all over the
world. In the last few decades there has been a tremendous increase in the demand for fresh water due to rapid growth of
population and the accelerated pace of industrialization (7). The quality of ground water varies from place to place, with
the depth of water table, and from season to season and is primarily governed by the extent and composition of dissolved
solids present in it (5). The quality of ground water is of great importance in determining the suitability of particular
ground water for a certain use such as for public water supply, irrigation, toilet flushing, industrial applications,
constructional use etc. (2) The study area, i.e. Part of Mumbai Metropolitan Region (MMR), is highly urbanized, densely
populated and is industrialized, hence there is a high demand for water. Since the demand for water is not met through
other resources; the need for clean groundwater is very high and is an alternative solution.
II. STUDY AREA.
The study area is located on the western most periphery of the Maharashtra State. The coordinates of the study area
are Virar on the north, Kalyan on north east and Panvel on south east. Arabian Sea lies on the southern side of the area.
Fig 1.Sampling locations.
International Journal of Innovative Research in Advanced Engineering (IJIRAE) ISSN: 2349-2163
Volume 1 Issue 6 (July 2014) http://ijirae.com
__________________________________________________________________________________________________
© 2014, IJIRAE- All Rights Reserved Page - 84
III. SAMPLING.
Fifteen water samples, were collected in polyethylene bottles from various bore wells covering the study area during
post monsoon 2013 and pre monsoon 2014, which were cleaned with acid water, followed by rinsing twice with distilled
water. The water samples were chemically analyzed on the same day. At the sampling points, the boreholes were purged
the aquifer of stagnant water to acquire fresh samples for analysis, purging lasted for 5–10 minutes. The analysis of water
were done by using procedure of ‘standard method’. Utmost care was taken during the collection of samples to avoid any
kind of contamination.
IV. RESULTS AND DISCUSSIONS.
A. Suitability of ground water for construction
TABLE.1 VARIOUS PARAMETERS AND ITS VALUES TO CHECK THE SUITABILITY FOR CONSTRUCTION
The parameters to check the suitability of ground water for construction purposes are tested and compared with IS456
guidelines. Among the samples, except the two samples (In Virar and Vasai,’sulphate’ content is more than 1600 mg/l.),
all others are suitable for construction.
B. Groundwater for Irrigation Purpose:
The water quality used for irrigation is essential for the crop yield and quantity, maintenance of soil productivity and
protection of the environment. The quality of irrigation water is very much influenced by the land constituents of the
water source. The important parameters affecting the suitability of groundwater for irrigation purposes are: Electrical
Conductivity (EC), Sodium adsorption ratio (SAR), Sodium percentage (Na %) and Residual sodium carbonate (RSC).
The various cations like calcium, magnesium, sodium, potassium and anions like carbonate and bicarbonate were
tested and the values are given in the table 2and table3.Electrical conductivity in the entire study area is given in table4.
Sr.no
Placeoftube
well
Limitsof
Acidity(ml)
Limitsof
Alkalinity(ml)
Chloride(mg/l)
Sulphate(mg/l)
Inorganic
matter(mg/l)
Organic
matter(mg/l)
Suspended
Solids(mg/l)
1 MATUNGA i.8 22 107 <200 540 40 40
2 JOGESHWARI 2.3 5.9 105 <200 510 20 70
4 MULUND 0.9 15.7 55 <200 320 40 35
3 THANE 0.6 5.9 97 <200 710 80 60
5 MAHIM 1.0 12.4 42 <200 435 30 30
6 NEW PANVEL 0.7 24.6 61 <200 340 80 100
7 DOMBIVALI(west) 1.8 53 49 <200 360 100 15
8 CHEMBUR 0.9 23.8 241 <200 830 40 35
9 ANDHERI 5.6 24.1 112 <200 455 40 65
10 KALYAN 0.5 4.6 43 <200 535 200 25
11 VIRAR 0.2 6.8 386 >1600 1500 80 180
12 VASAI 1.2 20 47 >1600 725 130 140
13 NALASAPORA 1.8 22 266 <200 955 115 120
14 DOMBIVALI(east) 2.0 15.0 79 <200 380 30 110
15 OLD PANVEL 2.0 20 52 <200 350 50 60
LIMITSAS PER
IS:456:-2000
5.0ml 25ml
500mg/l
for RCC
mg/l
400 mg/l 3000mg/l
200
mg/l
2000
mg/l
International Journal of Innovative Research in Advanced Engineering (IJIRAE) ISSN: 2349-2163
Volume 1 Issue 6 (July 2014) http://ijirae.com
__________________________________________________________________________________________________
© 2014, IJIRAE- All Rights Reserved Page - 85
TABLE 2 CATIONS CONCENTRATION IN MEQ/L
Place Ca2+
Mg2+
Na+
K+
Ca2+
Mg2+
Na+
K+
mg/l mg/l mg/l mg/l meq/l meq/l meq/l meq/l
Panvel 56.1 173.9 29.64 0.92 2.800 14.310 1.289 0.024
Nalasapora 62.5 187.5 60.15 3.54 3.119 15.429 2.616 0.091
Virar 48 112 49.2 0.89 2.395 9.216 2.140 0.023
Sum 8.314 38.955 6.046 0.137
TABLE 3 ANIONS CONCENTRATION IN MEQ/L
Place CO3
2-
HCO3 -
CO3
2-
HCO3
-
mg/l mg/l meq/l meq/l
Panvel 0.493 199.49 0.016 3.269
Nalasapora 0.074 183.43 0.002 3.006
Virar 0.463 191.52 0.015 3.139
Sum 0.034 12.68
TABLE 4 ELECTRICAL CONDUCTIVITY
SR NO.
PLACE OF
TUBEWELL
EC µS/cm
1 MATUNGA 523.0
2 JOGESWARI 400.0
4 MULUND 400.0
3 THANE 1076.9
5 MAHIM 615.0
6 NEW PANVEL 384.0
7 DOMBIVALI(west) 646.0
8 CHEMBUR 1261.0
9 ANDHERI 646.0
10 KALYAN 1076.0
11 VIRAR 1723.0
12 VASAI 1061.0
13 NALASAPORA 1353.0
14 DOMBIVALI(east) 415.0
15 OLD PANVEL 492.0
1) Electrical conductivity (EC): The total soluble salt content of irrigation water generally is measured by
determining its electrical conductivity. Electrical conductivity in the study area, ranges from 384 to 1723 µmhos/cm.
(µS/cm) during post monsoon season 2013. Normally, irrigation water with an EC<700 µmhos/cm causes little or no
threat to most crops, while EC>3000 µmhos/cm maylimit their growth (9). Hence the ground water in this area is suitable
for irrigation.
International Journal of Innovative Research in Advanced Engineering (IJIRAE) ISSN: 2349-2163
Volume 1 Issue 6 (July 2014) http://ijirae.com
__________________________________________________________________________________________________
© 2014, IJIRAE- All Rights Reserved Page - 86
2) Sodium Adsorption Ratio (SAR): Sodium Adsorption Ratio (SAR) is a criterion for evaluating the sodium
hazard in irrigation waters, determined by measuring the ratio of sodium to magnesium and calcium. The formula
for calculating sodium adsorption ratio is:
. . . =	
1
2
( + )
Where calcium, and magnesium are in milliequivalents/litre. With the proper amount of calcium and magnesium in the
irrigation water, the irrigated soil will be granular in structure, easily worked, and permeable .With increasing proportions
of sodium, the soil will tend to become less permeable and water logging may occur. (12) The SAR values for three
representative water samples are shown below.
TABLE 5. SAR VALUES
PLACE SAR
PANVEL 0.441
NALASAPORA 0.859
VIRAR 0.888
As per Richards’s (6) classification, the SAR values of all samples fall in excellent category(<10). The calculated value of
SAR in the study area ranges from 0.441 to 0.888. In general, the higher the sodium adsorption ratio, the less suitable the
water is for irrigation.
3) Sodium %: Sodium is important cations which in excess deteriorates the soil structure and reduces crop yield. Sodium
causes an increase in the hardness of soil as well as reduction in its permeability. The sodium in irrigation water is also
expressed as percent sodium (%Na) and can be determined using the following equation . (9)
Na% = (Na+
+ K+
) *100/ (Ca2+
+ Mg2+
+ Na+
+ K+
).Where all ionic concentrations are expressed in meq/l. The values
from the percent sodium in the study area ranges from 7-15% which is less than 60%, hence suitable for irrigation.
4) Residual Sodium Carbonate (RSC): The excess sum of carbonate and bicarbonate in groundwater over the sum of
calcium and magnesium also influences the unsuitability of groundwater for irrigation. This is termed as residual sodium
carbonate (RSC) .If RSC<1.25 meq/l, the water is considered safe. If RSC lies between 1.25-2.5 meq/l, the water is of
marginal quality. If RSC>2.5 meq/l, the water is unsuitable for irrigation. Residual Sodium Carbonate (RSC) predicts the
accumulation of sodium in the soil based on the potential precipitation of calcium/magnesium carbonate. The RSC is
calculated using the formula given below: RSC = (CO3
2-
+ HCO3
-
) - (Ca2+
+ Mg2+
) Where the concentrations are
expressed in meq/l (6).It is found that RSC of Panvel, Nalasapora and Virar are-
13.83,-
15.54and -
8.5 respectively. A
negative RSC indicates water is unlikely to cause structural degradation. .Thus, based on RSC criteria, the tested
groundwater samples can be considered safe for irrigation purpose.
V. CONCLUSION:
In the study area, all the ground water samples except two (Virar and Vasai) are fit for construction as per IS: 456.
2000 and all the samples are suitable for irrigation.
REFERENCES
1) BIS, Indian standards specifications for drinking water, Bureau of Indian Standards, IS: 10500, (2012).
2) Central Zonal Office Central Pollution Control Board Bhopal. “Status of Ground Water Quality in Chhattisgarh, 2010”.
3) CPHEEO Manual on Water supply and treatment, 3rd
edition, Ministry of Urban |Development, New Delhi, May 1999..
4) I.S 456( Fourth Revision ICS 91.100.30 to IS-456-2000 clause: 5: 4)
5) Ravi Kumar., P. and Somashekar., R. K., Multivariate analysis to evaluate geochemistry of groundwater in Varahi river basin of
Udupi in Karnataka (India), The Ecoscan, 4 (2&3): 153-162, 2010
6) Richards L.A(1954): “Diagnosis and Improvement of Saline and Alkali Soils”,
Agriculture Handbook 60, US Department of Agriculture, Washington, DC, P. 160
7) Rijsberman, F. R. Agricultural Water Management, 2006, 80(1-3), 5.
8) Standard Methods for the Examination of Water and Wastewater, American Public Health Association/American Water Works
Association/Water Environment Federation, Washington DC, 19th edition, 1995
9) Tijani M.N., Hydrochemical assessment of groundwater in Moro area, Kwara State, Nigeria, Environ Geol, 24,194–202, (1994)
10) United Nation (2012). UN News Centre – 2012 World Water Day: Target 7.C of the Mdgs Met Before the 2015 Deadline;
Ensuring Access to Water for Agriculture Vital For Sustainable Future. Un Web Services Section | Department Of Public
Information, UnitedNations©2010.
11) WHO. Guidelines for drinking-water quality, health criteria and other supporting information, IV.th
edition2011, (World Health
Organization, Geneva). ]
12) James M.Montgomery consulting engineers, Inc., Water treatment principles and design 1985A Wiley Interscience
Publications,USA

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Ground Water Quality Analysis for construction of Part of Mumbai Metropolitan Region (MMR)

  • 1. International Journal of Innovative Research in Advanced Engineering (IJIRAE) ISSN: 2349-2163 Volume 1 Issue 6 (July 2014) http://ijirae.com __________________________________________________________________________________________________ © 2014, IJIRAE- All Rights Reserved Page - 83 Ground Water Quality Analysis for construction of Part of Mumbai Metropolitan Region (MMR) James S. Main Pushpam.K.V Associate Professor, Civil & Environmental Engg, VJTI PG Student, M. Tech. Environmental Engg, VJTI Abstract: Groundwater quality in the study area has been analysed in the present work. For this study, a part of Mumbai Metropolitan Region were selected which covers almost the entire area. Fifteen water samples, from various bore wells covering the study area during post monsoon season 2013 were collected to find out the values of different parameters in the groundwater so as to check the suitability for construction. The tests for different parameters like, chloride, Sulphates, suspended solids, Inorganic material, organic material, limits of acidity and, limits of alkalinity were performed by using Standard procedures and the results were compared with IS456 guidelines. All samples, except two (In Virar and Vasai’ where sulphate’ content was more than 1600 mg/l.) are suitable for construction. Samples from ‘Old Panvel’, ‘Virar’ and ‘Nalasapora’ were tested for the suitability for irrigation also, since the ground water is used for irrigation in those areas. The important parameters affecting for irrigation purposes are: Electrical Conductivity (EC), Sodium adsorption ratio (SAR), Sodium percentage (Na %) and Residual sodium carbonate (RSC). All the parameter values were within the permissible range, hence the ground water from the said areas is suitable for irrigation. Key words. Electrical Conductivity, Sodium adsorption ratio, Sodium percentage and Residual sodium carbonate. I. INTRODUCTION Of the available global water supply, 97.2% is saline water in oceans. This water is unsuitable for drinking or agricultural uses. 2.14% is in ice caps and glaciers, 0.61% is groundwater. Much of this water is too deep for extraction. 0.009% is found in surface water. This is where most drinking water comes from.0.005% makes up soil moisture.0.001% of water is found in the atmosphere (10).Rapid urbanization, growing population and speedy industrialization have led to the pressure on demand for water. Ground water is used for domestic, industrial and irrigational purposes all over the world. In the last few decades there has been a tremendous increase in the demand for fresh water due to rapid growth of population and the accelerated pace of industrialization (7). The quality of ground water varies from place to place, with the depth of water table, and from season to season and is primarily governed by the extent and composition of dissolved solids present in it (5). The quality of ground water is of great importance in determining the suitability of particular ground water for a certain use such as for public water supply, irrigation, toilet flushing, industrial applications, constructional use etc. (2) The study area, i.e. Part of Mumbai Metropolitan Region (MMR), is highly urbanized, densely populated and is industrialized, hence there is a high demand for water. Since the demand for water is not met through other resources; the need for clean groundwater is very high and is an alternative solution. II. STUDY AREA. The study area is located on the western most periphery of the Maharashtra State. The coordinates of the study area are Virar on the north, Kalyan on north east and Panvel on south east. Arabian Sea lies on the southern side of the area. Fig 1.Sampling locations.
  • 2. International Journal of Innovative Research in Advanced Engineering (IJIRAE) ISSN: 2349-2163 Volume 1 Issue 6 (July 2014) http://ijirae.com __________________________________________________________________________________________________ © 2014, IJIRAE- All Rights Reserved Page - 84 III. SAMPLING. Fifteen water samples, were collected in polyethylene bottles from various bore wells covering the study area during post monsoon 2013 and pre monsoon 2014, which were cleaned with acid water, followed by rinsing twice with distilled water. The water samples were chemically analyzed on the same day. At the sampling points, the boreholes were purged the aquifer of stagnant water to acquire fresh samples for analysis, purging lasted for 5–10 minutes. The analysis of water were done by using procedure of ‘standard method’. Utmost care was taken during the collection of samples to avoid any kind of contamination. IV. RESULTS AND DISCUSSIONS. A. Suitability of ground water for construction TABLE.1 VARIOUS PARAMETERS AND ITS VALUES TO CHECK THE SUITABILITY FOR CONSTRUCTION The parameters to check the suitability of ground water for construction purposes are tested and compared with IS456 guidelines. Among the samples, except the two samples (In Virar and Vasai,’sulphate’ content is more than 1600 mg/l.), all others are suitable for construction. B. Groundwater for Irrigation Purpose: The water quality used for irrigation is essential for the crop yield and quantity, maintenance of soil productivity and protection of the environment. The quality of irrigation water is very much influenced by the land constituents of the water source. The important parameters affecting the suitability of groundwater for irrigation purposes are: Electrical Conductivity (EC), Sodium adsorption ratio (SAR), Sodium percentage (Na %) and Residual sodium carbonate (RSC). The various cations like calcium, magnesium, sodium, potassium and anions like carbonate and bicarbonate were tested and the values are given in the table 2and table3.Electrical conductivity in the entire study area is given in table4. Sr.no Placeoftube well Limitsof Acidity(ml) Limitsof Alkalinity(ml) Chloride(mg/l) Sulphate(mg/l) Inorganic matter(mg/l) Organic matter(mg/l) Suspended Solids(mg/l) 1 MATUNGA i.8 22 107 <200 540 40 40 2 JOGESHWARI 2.3 5.9 105 <200 510 20 70 4 MULUND 0.9 15.7 55 <200 320 40 35 3 THANE 0.6 5.9 97 <200 710 80 60 5 MAHIM 1.0 12.4 42 <200 435 30 30 6 NEW PANVEL 0.7 24.6 61 <200 340 80 100 7 DOMBIVALI(west) 1.8 53 49 <200 360 100 15 8 CHEMBUR 0.9 23.8 241 <200 830 40 35 9 ANDHERI 5.6 24.1 112 <200 455 40 65 10 KALYAN 0.5 4.6 43 <200 535 200 25 11 VIRAR 0.2 6.8 386 >1600 1500 80 180 12 VASAI 1.2 20 47 >1600 725 130 140 13 NALASAPORA 1.8 22 266 <200 955 115 120 14 DOMBIVALI(east) 2.0 15.0 79 <200 380 30 110 15 OLD PANVEL 2.0 20 52 <200 350 50 60 LIMITSAS PER IS:456:-2000 5.0ml 25ml 500mg/l for RCC mg/l 400 mg/l 3000mg/l 200 mg/l 2000 mg/l
  • 3. International Journal of Innovative Research in Advanced Engineering (IJIRAE) ISSN: 2349-2163 Volume 1 Issue 6 (July 2014) http://ijirae.com __________________________________________________________________________________________________ © 2014, IJIRAE- All Rights Reserved Page - 85 TABLE 2 CATIONS CONCENTRATION IN MEQ/L Place Ca2+ Mg2+ Na+ K+ Ca2+ Mg2+ Na+ K+ mg/l mg/l mg/l mg/l meq/l meq/l meq/l meq/l Panvel 56.1 173.9 29.64 0.92 2.800 14.310 1.289 0.024 Nalasapora 62.5 187.5 60.15 3.54 3.119 15.429 2.616 0.091 Virar 48 112 49.2 0.89 2.395 9.216 2.140 0.023 Sum 8.314 38.955 6.046 0.137 TABLE 3 ANIONS CONCENTRATION IN MEQ/L Place CO3 2- HCO3 - CO3 2- HCO3 - mg/l mg/l meq/l meq/l Panvel 0.493 199.49 0.016 3.269 Nalasapora 0.074 183.43 0.002 3.006 Virar 0.463 191.52 0.015 3.139 Sum 0.034 12.68 TABLE 4 ELECTRICAL CONDUCTIVITY SR NO. PLACE OF TUBEWELL EC µS/cm 1 MATUNGA 523.0 2 JOGESWARI 400.0 4 MULUND 400.0 3 THANE 1076.9 5 MAHIM 615.0 6 NEW PANVEL 384.0 7 DOMBIVALI(west) 646.0 8 CHEMBUR 1261.0 9 ANDHERI 646.0 10 KALYAN 1076.0 11 VIRAR 1723.0 12 VASAI 1061.0 13 NALASAPORA 1353.0 14 DOMBIVALI(east) 415.0 15 OLD PANVEL 492.0 1) Electrical conductivity (EC): The total soluble salt content of irrigation water generally is measured by determining its electrical conductivity. Electrical conductivity in the study area, ranges from 384 to 1723 µmhos/cm. (µS/cm) during post monsoon season 2013. Normally, irrigation water with an EC<700 µmhos/cm causes little or no threat to most crops, while EC>3000 µmhos/cm maylimit their growth (9). Hence the ground water in this area is suitable for irrigation.
  • 4. International Journal of Innovative Research in Advanced Engineering (IJIRAE) ISSN: 2349-2163 Volume 1 Issue 6 (July 2014) http://ijirae.com __________________________________________________________________________________________________ © 2014, IJIRAE- All Rights Reserved Page - 86 2) Sodium Adsorption Ratio (SAR): Sodium Adsorption Ratio (SAR) is a criterion for evaluating the sodium hazard in irrigation waters, determined by measuring the ratio of sodium to magnesium and calcium. The formula for calculating sodium adsorption ratio is: . . . = 1 2 ( + ) Where calcium, and magnesium are in milliequivalents/litre. With the proper amount of calcium and magnesium in the irrigation water, the irrigated soil will be granular in structure, easily worked, and permeable .With increasing proportions of sodium, the soil will tend to become less permeable and water logging may occur. (12) The SAR values for three representative water samples are shown below. TABLE 5. SAR VALUES PLACE SAR PANVEL 0.441 NALASAPORA 0.859 VIRAR 0.888 As per Richards’s (6) classification, the SAR values of all samples fall in excellent category(<10). The calculated value of SAR in the study area ranges from 0.441 to 0.888. In general, the higher the sodium adsorption ratio, the less suitable the water is for irrigation. 3) Sodium %: Sodium is important cations which in excess deteriorates the soil structure and reduces crop yield. Sodium causes an increase in the hardness of soil as well as reduction in its permeability. The sodium in irrigation water is also expressed as percent sodium (%Na) and can be determined using the following equation . (9) Na% = (Na+ + K+ ) *100/ (Ca2+ + Mg2+ + Na+ + K+ ).Where all ionic concentrations are expressed in meq/l. The values from the percent sodium in the study area ranges from 7-15% which is less than 60%, hence suitable for irrigation. 4) Residual Sodium Carbonate (RSC): The excess sum of carbonate and bicarbonate in groundwater over the sum of calcium and magnesium also influences the unsuitability of groundwater for irrigation. This is termed as residual sodium carbonate (RSC) .If RSC<1.25 meq/l, the water is considered safe. If RSC lies between 1.25-2.5 meq/l, the water is of marginal quality. If RSC>2.5 meq/l, the water is unsuitable for irrigation. Residual Sodium Carbonate (RSC) predicts the accumulation of sodium in the soil based on the potential precipitation of calcium/magnesium carbonate. The RSC is calculated using the formula given below: RSC = (CO3 2- + HCO3 - ) - (Ca2+ + Mg2+ ) Where the concentrations are expressed in meq/l (6).It is found that RSC of Panvel, Nalasapora and Virar are- 13.83,- 15.54and - 8.5 respectively. A negative RSC indicates water is unlikely to cause structural degradation. .Thus, based on RSC criteria, the tested groundwater samples can be considered safe for irrigation purpose. V. CONCLUSION: In the study area, all the ground water samples except two (Virar and Vasai) are fit for construction as per IS: 456. 2000 and all the samples are suitable for irrigation. REFERENCES 1) BIS, Indian standards specifications for drinking water, Bureau of Indian Standards, IS: 10500, (2012). 2) Central Zonal Office Central Pollution Control Board Bhopal. “Status of Ground Water Quality in Chhattisgarh, 2010”. 3) CPHEEO Manual on Water supply and treatment, 3rd edition, Ministry of Urban |Development, New Delhi, May 1999.. 4) I.S 456( Fourth Revision ICS 91.100.30 to IS-456-2000 clause: 5: 4) 5) Ravi Kumar., P. and Somashekar., R. K., Multivariate analysis to evaluate geochemistry of groundwater in Varahi river basin of Udupi in Karnataka (India), The Ecoscan, 4 (2&3): 153-162, 2010 6) Richards L.A(1954): “Diagnosis and Improvement of Saline and Alkali Soils”, Agriculture Handbook 60, US Department of Agriculture, Washington, DC, P. 160 7) Rijsberman, F. R. Agricultural Water Management, 2006, 80(1-3), 5. 8) Standard Methods for the Examination of Water and Wastewater, American Public Health Association/American Water Works Association/Water Environment Federation, Washington DC, 19th edition, 1995 9) Tijani M.N., Hydrochemical assessment of groundwater in Moro area, Kwara State, Nigeria, Environ Geol, 24,194–202, (1994) 10) United Nation (2012). UN News Centre – 2012 World Water Day: Target 7.C of the Mdgs Met Before the 2015 Deadline; Ensuring Access to Water for Agriculture Vital For Sustainable Future. Un Web Services Section | Department Of Public Information, UnitedNations©2010. 11) WHO. Guidelines for drinking-water quality, health criteria and other supporting information, IV.th edition2011, (World Health Organization, Geneva). ] 12) James M.Montgomery consulting engineers, Inc., Water treatment principles and design 1985A Wiley Interscience Publications,USA