Evaluation of Geochemical Characteristics of Groundwater in Parts of Ghataprabha Sub-basin Using DRASTIC Indices

Abstract

Ghataprabha is an auxiliary of river Krishna and flows over Chandgad taluk of Kolhapur district, Maharashtra. Bauxite mining was one of the major issues in this part of the sub-basin, in the early ’90s due to which there was a strong public protest about the quality of water. Accordingly, a survey was conducted to get the public perception on water pollution in the headwater catchment of Ghataprabha sub-basin. During the survey, a broad opinion was expressed with regard to water quality contamination of Ghataprabha river by a section of the society living in the riparian zones of the river basin. Therefore, in this paper, an effort has been done to understand the in variation in water quality with special reference to groundwater. Thirty-eight groundwater samples (nineteen each from before and after rainy season) were assembled and analysed for EC, TDS, pH, chlorine ion HCO3, SO4, PO4, Ca, Mg, Na and K. The values have shown that the density of all measured factors is broadly within the permissible limits (as per BIS Standards), before and after-monsoon. The present observations do compared with the earlier reported parameters of the year 2000. The results show that there is a betterment of water quality in the mining field as compared to previous data. This clearly demonstrates that the mining area can be reclaimed over the years by taking appropriate conservation measures. However, ionic ratios such as SAR, KR and SSP showed considerable variations indicating that there is localised impact on water quality resulting in the groundwater pollution. DRASTIC indices were computed based on hydrogeological characteristics and found that more than 30% of the observatory wells are contaminated where the nitrates are very high (more than 45mg/L) which clearly demonstrated that groundwater is getting polluted in high intense agriculture areas and also in areas close to settlements.

Water induced surface erosion risk assessment in Jumar agricultural watershed, Jharkhand, India using multivariate statistics and GIS

“…The high intensity rainfall for a prolonged period causes weathering of surface soil and dilution of ions in surface water (Fu et al, 2020;Ghaemi & Noshadi, 2022). The precipitation water percolates and reacts with carbon dioxide generated in microbial processes and air trapped in pores in summers to form carbonic acid (Mali et al, 2020;Rao et al, 2021). Later, the carbonic acid form dissociates to release hydrogen ions lowering the pH (Marghade et al, 2021).…”

Evaluation of Groundwater Vulnerability of Yishu River Basin Based on DRASTIC-GIS Model

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