Evolution of groundwater chemistry in and around Vaniyambadi Industrial Area: Differentiating the natural and anthropogenic sources of contamination |
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Institution: | 1. British Geological Survey, Maclean Building, Wallingford, UK;2. National Institute of Hydrology, Roorkee, Uttarakhand, India;3. British Geological Survey, Lyell Centre, Edinburgh, UK;1. Dept. of Natural Resources, TERI University, New Delhi, India;2. Department of Environmental Sciences, Fiji National University, Fiji;3. Department of Environmental Science, Central University of Rajasthan, India;4. Institute for the Advanced Study of Sustainability (UNU-IAS), United Nations University, Japan;5. Faculty of Engineering, King Khalid University, Abha, Saudi Arabia |
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Abstract: | Groundwaters in the crystalline aquifers are the major source of drinking water in Vaniyambadi area of Vellore district. Geochemical methods in collaboration with statistical methods were applied in this industrial area to understand the natural and anthropogenic influences on groundwater quality. To accomplish this objective, groundwater samples were collected and analyzed for physicochemical parameters and the results showed a dominance in the order of Na+ > Mg2+ > Ca2+ > K+ and HCO3? > Cl? > SO42? > NO3? for anions and cations, respectively. In contrast to this anion dominance were changed to Cl? > HCO3? > SO42? > NO3? in samples collected near the tannery industries. Groundwater quality evaluation using TDS and TH suggested that 57% of the total samples are hard-brackish type, indicating its unsuitability for drinking purpose. Generally the water type is Na+Cl? to Ca2+Mg2+HCO3? type with an intermediate Ca2+Mg2+Cl?, suggesting the mixing of fresh groundwater with tannery effluent and cation exchange. Factor analysis and bivariate plots of major ions suggests that both natural and anthropogenic inputs are equally influencing the groundwater quality. Further investigations proved that silicate weathering is the dominant geogenic source of groundwater solute content, whereas tannery effluent is the anthropogenic source. Saline water mixing index (SWMI) and Cl? vs NO3? bivariate plot were employed to differentiate the tannery contamination from the other anthropogenic inputs such as agricultural fertilizers, municipal sewages, etc. This analysis shows that samples 2, 4, 8 and 9 (located within the tannery cluster) have a SWMI value greater than 1, representing the groundwater–tannery effluent mixing. This study infers that groundwater in the Vaniyambadi area is under serious threat from both natural and anthropogenic contamination. However, the controlling discharge of untreated tannery effluents must be regulated to reduce the further deterioration of this vital resource in this part of the country. |
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Keywords: | Hydrogeochemistry Factor analysis Natural and anthropogenic sources Saline water–groundwater mixing Vaniyambadi South India |
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