4.5 Article

Physicochemical quality evaluation of groundwater and development of drinking water quality index for Araniar River Basin, Tamil Nadu, India

期刊

ENVIRONMENTAL MONITORING AND ASSESSMENT
卷 186, 期 2, 页码 935-948

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SPRINGER
DOI: 10.1007/s10661-013-3425-7

关键词

Groundwater quality; Piper trilinear diagram; Drinking water quality index; Araniar River Basin

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  1. Council of Scientific and Industrial Research, New Delhi, India

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Groundwater is the most important natural resource which cannot be optimally used and sustained unless its quality is properly assessed. In the present study, the spatial and temporal variations in physicochemical quality parameters of groundwater of Araniar River Basin, India were analyzed to determine its suitability for drinking purpose through development of drinking water quality index (DWQI) maps of the post- and pre-monsoon periods. The suitability for drinking purpose was evaluated by comparing the physicochemical parameters of groundwater in the study area with drinking water standards prescribed by the World Health Organization (WHO) and Bureau of Indian Standards (BIS). Interpretation of physicochemical data revealed that groundwater in the basin was slightly alkaline. The cations such as sodium (Na+) and potassium (K+) and anions such as bicarbonate (HCO3 (-)) and chloride (Cl-) exceeded the permissible limits of drinking water standards (WHO and BIS) in certain pockets in the northeastern part of the basin during the pre-monsoon period. The higher total dissolved solids (TDS) concentration was observed in the northeastern part of the basin, and the parameters such as calcium (Ca2+), magnesium (Mg2+), sulfate (SO4 (2-)), nitrate (NO3 (-)), and fluoride (F-) were within the limits in both the seasons. The hydrogeochemical evaluation of groundwater of the basin demonstrated with the Piper trilinear diagram indicated that the groundwater samples of the area were of Ca2+-Mg2+-Cl--SO4 (2-), Ca2+-Mg2+-HCO3 (-) and Na+-K+-Cl--SO4 (2-) types during the post-monsoon period and Ca2+-Mg2+-Cl--SO4 (2-), Na+-K+-Cl--SO4 (2-) and Ca2+-Mg2+-HCO3 (-) types during the pre-monsoon period. The DWQI maps for the basin revealed that 90.24 and 73.46 % of the basin area possess good quality drinking water during the post- and pre-monsoon seasons, respectively.

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