Characterization of ground water quality of Siwani and Tosham blocks of Bhiwani district of Haryana

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Date
2009
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CCSHAU
Abstract
The Present investigation for characterization of ground water quality and its effect on soil properties in respective blocks, was undertaken. Two hundred and five (205) and one hundred seventy three (173) ground water samples were collected from randomly selected tube-wells of Siwani and Tosham blocks, respectively. The Soil samples were collected from sites of different quality ground water used of Siwani and Tosham blocks and were analyzed for their physico-chemical properties. The pH, EC, SAR and RSC in ground waters varied from 7.8-9.1, 0.26-17.62 dS m-1, 0.06-28.45 (mM L-1)1/2 and nil-11.43 me L-1, respectively in Siwani Block and from 7.50-9.10, 0.29-17.53 dS m-1, 0.32-45.74(mM L-1)1/2 and nil-5.56 me L-1 respectively in Tosham Block. Dominant cation was sodium followed by magnesium and calcium. Likewise, in the case of anions, chloride was the dominant anion followed by sulphate, bicarbonate and carbonate upto EC 3 dSm-1 and after EC class 3-6 dS m-1 and above the trend was Cl- > SO4-2 >HCO3- >CO3-2 type water in Siwani block. In Tosham block dominant cation was sodium followed by magnesium and calcium. Likewise, in the case of anions, chloride was the dominant anion followed by sulphate, bicarbonate and carbonate.As per Manchanda (1976) classification 17, 21, 21, 10, and 31 percent waters of Siwani block were classified under good, marginal, saline, sodic, and saline-sodic categories respectively. As per AICRP (1989) classification 17%, water samples were found under good category, 21% marginally saline, 21% saline, 31% high SAR saline, 1.0% marginally alkali, 1%, alkali and 8% water samples were classified as highly alkali waters. Similarly, in Tosham block 26%, 22%, 13%, 8% and 31% waters of Tosham block were classified under good, marginal, saline, sodic, and saline-sodic categories respectively. As per AICRP (1989) classification 27%, water samples were found under good category, 23% marginally saline, 13% saline, 31% high SAR saline, 3% marginally alkali, 1%, alkali and 2% water samples were classified as highly alkali waters. The marginal water could be used without appreciable harmful effect on crop and soil. But its long term use depends on type of soil, rainfall and crops to be grown. The problematic water required special management practices depending upon the soil type, crop and climatic factors. The use of poor quality water resulted salt accumulation both in surface (0-15 cm) and sub surface (15-30 cm) layers. Mostly highest ECe and SARe were observed in the surface layer (0-15 cm) of soil.
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Area, Productivity, Crops, Irrigation, Biological development, Land resources, Economics, Agricultural development, Livestock, Agricultural products
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