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Proceeding of National Conference on Environment and Development, 9th and 10th Sept. 2016 Conference Organised by, Dr. B. N. P. Arts, Smt. S. G. G. Com, & Sci. College, Lonavala
http://rutpp.com; 179 ISBN: 978-93-84663-10-0
An Evaluation of Seasonal Variation in Physico-chemical Parameters
of Borewell Water from Purandar Tehsil, Dist: Pune, (M.S.) India
B. L. Shinde1, B. U. Mane
1, K. S. Lohar
2
1. PDEA’s Waghire College, Saswad
2. Shrikrishna Mahavidyalaya, Gunjoti
ABTRACT:
The present study was carried on seasonal variation of physico-chemical parameters of
Bore-well Water from Purandar Tehsil, Dist: Pune, (M.S.) India. Overall, 20 samples were
collected during three seasons i) monsoon of 2013, ii) winter of 2013 and iii) summer of
2014 from the bore wells of various places of Purandhar Tehsil. The major water quality
parameters considered for the examination in this study are Temperature, pH, electrical
conductivity, total alkalinity, total dissolved salts, chlorine, dissolved oxygen, calcium
hardness, magnesium hardness and total hardness. The collected water samples were
analyzed and results obtained were compared with standards prescribed by WHO, and
Indian Standard Drinking Water specification IS: 10500-2012. It was found that the all
parameters were within permissible limit and bore well water is safe for drinking purpose.
Key Words: Bore Well water, Physico-chemical parameter, water quality.
INTRODUCTION
In different form water exists in nature such as cloud, rain, snow, ice and fog. Chemically pure water
does not be present for any appreciable duration in nature. It gets polluted as it reaches us. It cannot remain
pure during raining. It picks up small quantity of gases, ions, dust and particular matter from the atmosphere.
The quantity as well as the quality of water at given time and given space is very important in relation to the
life at that location at that time1. Groundwater is used for domestic and industrial water supply and also for
irrigation purposes in 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 industrialization2.
According to WHO organization, about 80% of all the diseases in human beings are caused by water. Water
quality becomes an important parameter for the assessment and management of groundwater. The greater
part of the soluble constituents in ground water comes from soluble minerals in soils and sedimentary rocks.
The more common soluble constituents include calcium, sodium, bicarbonate and sulphate ions. Water
sources available for drinking and other domestic purpose must possess high degree of purity, free from
chemical contamination and micro-organism. The potential and quality of bore-well water, is an economic
resource and essential component of our life, is getting deteriorated in major rural centers due to pollution
caused by population explosion, ruralization and industrialization3.
Studies on bore well water here we reported the seasonal variation in physicochemical parameters of
bore wells water from Purandhar Tehsil. Purandar is the rural and hilly area comes in shadow of rainfall.
Thus to complete needs of water number of bore-wells were constructed. Bore-wells are of different depths
ranging from 200 to 500 feet, thus Bore-well water contains number of salts along with hazardous heavy
metals.
MATERIALS AND METHODS
The study area, the Purandar Tehsil is situated in Pune district . Overall, 20 samples were collected
during three seasons i) monsoon of 2013, ii) winter of 2013 and iii) summer of 2014 from the bore wells of
various places of Purandhar Tehsil. The samples collected B-1 to B-20 from villages of Purandhar Tehsil
were Saswad, Kalewadi, Zendewadi, Dive, Khalad, Shivri, Jejuri, Nira, Veer, Parinche, Malshiras,
Waghapur, Shingapur, Vanpuri, Bhiwadi, Narayanpur, Chivewadi, Garade, Chambli and Bhivari
respectively. These samples were collected in clean and dry polyethylene bottle from bore wells after
Proceeding of National Conference on Environment and Development, 9th and 10th Sept. 2016 Conference Organised by, Dr. B. N. P. Arts, Smt. S. G. G. Com, & Sci. College, Lonavala
http://rutpp.com; 180 ISBN: 978-93-84663-10-0
running them from 5 minutes. All the collection of samples are processed for the different analysis within 6
to 12 hours after collection. In this present study various physical and chemical parameters of water samples
were determined and the result compared with standards prescribed by WHO, and Indian Standard Drinking
Water specification IS: 10500-2012.
All AR grade chemicals used for analysis of water. Double distilled water was used for the
preparation of reagents and solutions. The major water quality parameters considered for the examination in
this study are Temperature, pH, electrical conductivity, total alkalinity, total dissolved salts, chlorine,
dissolved oxygen, calcium hardness, magnesium hardness and total hardness.
Analysis of water samples carried out by using Standard Methods for examination of Water and
Waste Water by APHA 7. The temperature of the water samples was measured at sampling sites by 1/10
th
mercury thermometer of 0 to 1000C range. Elico digital pH meter was used for the measurement of pH
values. Standard buffer solutions of pH 4.0 and 9.2 were used for calibration. The total dissolved solids were
estimated by gravimetric method. The conductivity of water sample was measured with help of a digital
Elico conductivity meter. Dissolved oxygen was determined by modified Winkler’s method. Alkalinity is
measured by titration with standardized acid and is expressed commonly as milligrams per liter as calcium
carbonate (mg/l as CaCO3). Chloride was determined by titrimetric method. The calcium, magnesium and
total hardness was determined titrimetrically using EDTA method.
RESULTS AND DISCUSSION:
The seasonal variation in physico-chemical parameters i.e. Temperature, pH, electrical conductivity,
total alkalinity, total dissolved salts, chlorine, dissolved oxygen, calcium hardness, magnesium hardness and
total hardness of bore well water samples collected from villages of Purandhar Tehsil were analyzed.
The results of analysis of various physico – chemical parameters for the bore well water samples
collected are given in Table no. 1 (monsoon season-2013), Table no. 2 (winter season-2013) and Table no. 1
(summer season-2014). Samplings were done in three different seasons from June 2013 to April 2014.
Fig: 1 Seasonal Variation in Temperature of the Bore-well water samples
Proceeding of National Conference on Environment and Development, 9th and 10th Sept. 2016 Conference Organised by, Dr. B. N. P. Arts, Smt. S. G. G. Com, & Sci. College, Lonavala
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Table – 1: The physico- chemical analysis of the Bore-well water samples collected from different villages
of Purandhar Tehsil Dist: Pune during monsoon season of year 2013.
Sample
Temp
. 0C
Electrical
Conductanc
e
µmhos/cm
PH
Total
Alkalinity
mg/L
Total
Hardness
mg/L
Calcium
Hardness
mg/L
Magnesiu
m
Hardness
mg/L
Total
Dissolved
Solids
(TDS)
mg/L
Dissolved
Oxygen
(DO)
mg/L
Chlorid
e
mg/L
B-1 24 298.6 8.5 226.1 196.4 60.14 41.14 551.4 10.3 85.71
B-2 29 332.4 8.2 192.8 345.6 62.20 43.20 700.6 10.0 87.77
B-3 31 389.0 7.2 169.7 303.7 51.30 32.30 658.7 9.0 76.87
B-4 28 176.5 8.4 232.7 296.8 78.32 59.32 651.8 10.2 103.89
B-5 30 198.7 8.3 125.8 176.4 66.53 47.53 531.4 10.1 92.10
B-6 34 252.4 7.8 235.6 198.5 75.64 56.64 553.5 9.6 101.21
B-7 35 284.6 7.9 203.5 266.8 88.68 69.68 621.8 9.7 114.25
B-8 26 166.8 7.7 196.2 289.7 44.58 25.58 644.7 9.5 70.15
B-9 33 198.1 7.2 188.2 360.3 55.36 36.36 715.3 9.0 80.93
B-10 36 251.9 8 170.2 265.8 78.96 59.96 620.8 9.8 104.53
B-11 33 370.4 7.9 230.7 264.5 67.35 48.35 619.5 9.7 92.92
B-12 35 345.6 7.7 212.6 288.9 49.26 30.26 643.9 9.5 74.83
B-13 28 284.6 8.4 189.6 320.5 51.44 32.44 675.5 10.2 77.01
B-14 27 135.3 8.2 133.9 334.6 66.54 47.54 689.6 10.0 92.11
B-15 32 167.3 7.5 160.4 362.0 88.33 69.33 717.0 9.3 113.90
B-16 34 272.1 8.1 172.8 309.4 72.46 53.46 664.4 9.9 98.03
B-17 35 202.4 7.4 180.6 352.7 45.78 26.78 707.7 9.2 71.35
B-18 33 241.5 7.9 178.5 346.8 48.22 29.22 701.8 9.7 73.79
B-19 36 231.7 8 260.0 325.8 59.67 40.67 680.8 9.8 85.24
B-20 35 300.3 8.3 222.5 198.6 53.47 34.47 553.6 10.1 79.04
Table – 2: The physico- chemical analysis of the Bore-well water samples collected from different villages
of Purandhar Tehsil Dist: Pune during winter season of year 2013.
Sample
Temp
. 0C
Electrical
Conductanc
e
µmhos/cm
PH
Total
Alkalinity
mg/L
Total
Hardness
mg/L
Calcium
Hardness
mg/L
Magnesiu
m
Hardness
mg/L
Total
Dissolved
Solids
(TDS)
mg/L
Dissolved
Oxygen
(DO)
mg/L
Chlorid
e
mg/L
B-1 22 316.5 7.5 239.3 230.0 63.45 42.53 584.8 10.0 89.08
B-2 27 350.3 7.2 206.0 379.2 65.51 44.59 734.0 9.7 91.14
B-3 29 365.2 6.2 182.9 337.3 54.61 33.69 692.1 8.7 80.24
B-4 26 194.4 7.4 245.9 330.4 81.63 60.71 685.2 9.9 107.26
B-5 28 216.6 7.3 139.0 210.0 69.84 48.92 564.8 9.8 95.47
B-6 32 270.3 6.8 248.8 232.1 78.95 58.03 586.9 9.3 104.58
B-7 27 302.5 6.9 216.7 300.4 91.99 71.07 655.2 9.4 117.62
B-8 24 184.7 6.7 209.4 323.3 47.89 26.97 678.1 9.2 73.52
B-9 31 216.0 6.2 201.4 393.9 58.67 37.75 748.7 8.7 84.30
B-10 28 269.8 7 183.4 299.4 82.27 61.35 654.2 9.5 107.90
Proceeding of National Conference on Environment and Development, 9th and 10th Sept. 2016 Conference Organised by, Dr. B. N. P. Arts, Smt. S. G. G. Com, & Sci. College, Lonavala
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B-11 31 388.3 6.9 243.9 298.1 70.66 49.74 652.9 9.4 96.29
B-12 26 363.5 6.7 225.8 322.5 52.57 31.65 677.3 9.2 78.20
B-13 26 302.5 7.4 202.8 354.1 54.75 33.83 708.9 9.9 80.38
B-14 25 153.2 7.2 147.1 368.2 69.85 48.93 723.0 9.7 95.48
B-15 30 185.2 6.5 173.6 395.6 91.64 70.72 750.4 9.0 117.27
B-16 32 290.0 7.1 186.0 343.0 75.77 54.85 697.8 9.6 101.40
B-17 33 220.3 6.4 193.8 386.3 49.09 28.17 741.1 8.9 74.72
B-18 31 259.4 6.9 191.7 380.4 51.53 30.61 735.2 9.4 77.16
B-19 29 249.6 7 273.2 359.4 62.98 42.06 714.2 9.5 88.61
B-20 33 318.2 7.3 235.7 232.2 56.78 35.86 587.0 9.8 82.41
Table – 3: The physico- chemical analysis of the Bore-well water samples collected from different villages
of Purandhar Tehsil Dist: Pune during summer season of year 2014.
Sample
Temp
. 0C
Electrical
Conductanc
e
µmhos/cm
PH
Total
Alkalinity
mg/L
Total
Hardness
mg/L
Calcium
Hardness
mg/L
Magnesiu
m
Hardness
mg/L
Total
Dissolved
Solids
(TDS)
mg/L
Dissolved
Oxygen
(DO)
mg/L
Chlorid
e
mg/L
B-1 33 329.9 8.2 247.09 251.1 66.82 44.66 608.1 9.6 94.43
B-2 32 363.7 7.9 213.79 400.3 68.88 46.72 757.3 9.3 96.49
B-3 34 378.6 6.9 190.69 358.4 57.98 35.82 715.4 8.3 85.59
B-4 31 207.8 8.1 253.69 351.5 85.00 62.84 708.5 9.5 112.61
B-5 33 230.0 8 146.79 231.1 73.21 51.05 588.1 9.4 100.82
B-6 37 283.7 7.5 256.59 253.2 82.32 60.16 610.2 8.9 109.93
B-7 32 315.9 7.6 224.49 321.5 95.36 73.20 678.5 9.0 122.97
B-8 29 198.1 7.4 217.19 344.4 51.26 29.10 701.4 8.8 78.87
B-9 36 229.4 6.9 209.19 415.0 62.04 39.88 772.0 8.3 89.65
B-10 33 283.2 7.7 191.19 320.5 85.64 63.48 677.5 9.1 113.25
B-11 36 401.7 7.6 251.69 319.2 74.03 51.87 676.2 9.0 101.64
B-12 31 376.9 7.4 233.59 343.6 55.94 33.78 700.6 8.8 83.55
B-13 31 315.9 8.1 210.59 375.2 58.12 35.96 732.2 9.5 85.73
B-14 30 166.6 7.9 154.89 389.3 73.22 51.06 746.3 9.3 100.83
B-15 35 198.6 7.2 181.39 416.7 95.01 72.85 773.7 8.6 122.62
B-16 34 303.4 7.8 193.79 364.1 79.14 56.98 721.1 9.2 106.75
B-17 34 233.7 7.1 201.59 407.4 52.46 30.30 764.4 8.5 80.07
B-18 36 272.8 7.6 199.49 401.5 54.90 32.74 758.5 9.0 82.51
B-19 34 263.0 7.7 280.99 380.5 66.35 44.19 737.5 9.1 93.96
B-20 36 331.6 8 243.49 253.3 60.15 37.99 610.3 9.4 87.76
The graphical representation of seasonal variation in physico-chemical parameters i.e. Temperature, pH,
electrical conductivity, total alkalinity, total dissolved salts, chlorine, dissolved oxygen, calcium hardness,
magnesium hardness and total hardness of bore well water samples collected from villages of Purandhar
Tehsil were shown in fig No. 1 to fig No. 10.
Proceeding of National Conference on Environment and Development, 9th and 10th Sept. 2016 Conference Organised by, Dr. B. N. P. Arts, Smt. S. G. G. Com, & Sci. College, Lonavala
http://rutpp.com; 183 ISBN: 978-93-84663-10-0
Fig: 2 Seasonal Variation in Electrical Conductance of the Bore-well water samples
Fig: 3 Seasonal Variation in P
H of the Bore-well water samples
Proceeding of National Conference on Environment and Development, 9th and 10th Sept. 2016 Conference Organised by, Dr. B. N. P. Arts, Smt. S. G. G. Com, & Sci. College, Lonavala
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Fig: 4 Seasonal Variation in Total Alkalinity of the Bore-well water samples
Fig: 5 Seasonal Variation in Total Hardness of the Bore-well water samples
Proceeding of National Conference on Environment and Development, 9th and 10th Sept. 2016 Conference Organised by, Dr. B. N. P. Arts, Smt. S. G. G. Com, & Sci. College, Lonavala
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Fig: 6 Seasonal Variation in Calcium Hardness of the Bore-well water samples
Fig:7 Seasonal Variation in Magnesium Hardness of the Bore-well water samples
Proceeding of National Conference on Environment and Development, 9th and 10th Sept. 2016 Conference Organised by, Dr. B. N. P. Arts, Smt. S. G. G. Com, & Sci. College, Lonavala
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Fig: 8 Seasonal Variation in TDS of the Bore-well water samples
Fig: 9 Seasonal Variation in DO of the Bore-well water samples
Proceeding of National Conference on Environment and Development, 9th and 10th Sept. 2016 Conference Organised by, Dr. B. N. P. Arts, Smt. S. G. G. Com, & Sci. College, Lonavala
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Fig: 10 Seasonal Variation in Chloride of the Bore-well water samples
Temperature: Temperature of water is basically important because it effects bio-chemical reactions in
aquatic organisms. A rise in temperature of water leads to the increase in chemical reactions in water,
reduces the solubility of gases and amplifies the tastes and odours. The highest temperature observed during
summer season and the lowest during monsoon season. The average temperature of the present study ranged
from 24.00 – 36.00 0 C.
Total Alkalinity: The alkalinity in natural water is formed due to dissolution of carbon dioxide in water.
Carbonates, bicarbonates, thus formed are dissolved to yield hydroxyl ions. In the present investigation the
total alkalinity of the water samples is found in the Range 147.1 to 280.99 mg/lt.
pH: It is known that pH of water (6.5 to 8.5) does not has direct effect. But lower value below 5.0 produce
sore taste and has higher value above 8.5 and alkaline taste. The variation in pH ranged between 6.2 to 8.5.
pH was minimum in winter and maximum in monsoon season.
Electrical conductivity: Electrical conductivity is an important parameter for determining the water quality
for drinking and agricultural purposes. Many dissolved substances may produce colour, taste and odour. The
average values obtained are in the range 166.80 to 378.58 µmhos/cm.
Total Dissolve Solids: TDS values are useful to determine whether water is suitable for drinking purpose,
agriculture and industrial purposes. The TDS values in the present study ranged within 531.40 to 773.70
mg/lt. Generally TDS were observed maximum during the summer and minimum during winter.
Total Hardness: Water with Hardness above 200 mg / lit. may cause scale deposition in the distribution
system and results in excessive soap consumption and subsequent scur formation. Soft water with hardness
of less than 100 mg/ lit may have lower buffer capacity and more corrosive to water pipes. The hardness
values in the present investigation were found to range between 176.4 to 416.7 mg/lit. The highest value of
hardness observed was summer, while it was lowest in winter.
Calcium Hardness: Calcium is one of the most abundant metals which play an important role in biological
system. The calcium hardness values in the present investigation were found to range between 44.58 to
95.36 mg/lit.
Magnesium hardness: Magnesium though an essential and beneficial metal is toxic at higher
concentrations. Magnesium hardness particularly associated with sulphate ion has laxative effect on persons
un accustomed to it. In the present study calcium and magnesium contents are found in the range of 25.58 to
73.2 mg/lit.
Proceeding of National Conference on Environment and Development, 9th and 10th Sept. 2016 Conference Organised by, Dr. B. N. P. Arts, Smt. S. G. G. Com, & Sci. College, Lonavala
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Chloride: Chloride occurs in all types of natural waters. The high concentration of chloride is considered to
be an indication of pollution by sewage waste of animal origin. Industries are also important sources of
chloride in water. Chloride values obtained in the study are found in the range of 70.15 to 122.97 mg/lit.
Choride was minimum in monsoon and maximum in summer season.
Dissolved Oxygen (DO): DO is the parameters used to assess the pollution of water. DO values obtained in
the present study are within permissible levels.
IV: CONCLUSION
In this study various physical and chemical parameters of water samples were determined and the
result compared with standards prescribed by WHO, and Indian Standard Drinking Water specification IS:
10500-2012
In the present work the analyzed physico-chemical parameters are Temperature, pH, electrical
conductivity, total alkalinity, total dissolved salts, chlorine, dissolved oxygen, calcium hardness, magnesium
hardness and total hardness were within permissible limit.
ACKNOWLEDGEMENT
Authors are thankful to the University Grants Commission, Western Regional Office Pune, for funding
minor research project.
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