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Investigation of hydrogeochemical processes and groundwater quality in Upper Vellar sub-basin Tamilnadu, India

机译:印度泰米尔纳德邦上上层盆地的水文地球化学过程和地下水质量调查

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An attempt has been made in the Upper Vellar sub-basin to assess the hydrogeochemical processes influencing the water chemistry along with suitability of water for domestic and agricultural utilities. A total of 35 groundwater samples were collected for two different seasons, premonsoon (PRM) and post monsoon (POM), and analyzed for major cations, anions, and trace elements. The obtained results indicate that the dominance of silicate weathering, ion exchange process, and anthropogenic and microbial activities alter the chemistry of groundwater. The Piper plot suggests the facies evolution from Ca-HCO3, Ca-Mg-Cl and mixed Ca-Na-HCO3 and NaCl fluxes influencing the water chemistry. The ionic ratio plots suggest the predominance of Na+, Ca2+, HCO3- and Cl- indicating the silicate minerals dissolution and anthropogenic activities. All the trace elements are within the scale; however, Zn exceeds the WHO standard. The stability plot suggests samples representing kaolinite field during PRM and evolves towards montmorillonite and chloride field during POMinfers the dissolution of silicates minerals and ions from host rocks. According to the WHO standard, 23% of PRM and 6% of POM water samples exceed the maximum permissible limits for drinking purposes.
机译:已尝试在上韦拉尔次流域中评估影响水化学的水文地球化学过程以及水对家庭和农业公用事业的适用性。在两个不同季节(季风前(PRM)和季风后(POM))总共收集了35个地下水样品,并分析了其中的主要阳离子,阴离子和微量元素。获得的结果表明,硅酸盐风化作用,离子交换过程以及人为和微生物活动的优势改变了地下水的化学性质。 Piper图表明,Ca-HCO3,Ca-Mg-Cl以及Ca-Na-HCO3和NaCl混合通量的相演化会影响水的化学反应。离子比图表明,Na +,Ca2 +,HCO3-和Cl-占优势,表明硅酸盐矿物的溶解和人为活动。所有的痕量元素都在比例之内。但是,锌超过了世界卫生组织的标准。稳定性图表明,样品代表PRM期间的高岭土场,并在POMin期间向蒙脱石和氯化物场演变,从而溶解了硅酸盐矿物和离子从宿主岩石中的溶解。根据WHO标准,PRM中的23%和POM水样品中的6%超出了饮用目的的最大允许限值。

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