HYDROGEOCHEMICAL BEHAVIOUR AND GROUNDWATER SUITABILITY OF VISLON AREA, PART OF WRD WATERSHED, CHANDRAPUR DISTRICT, MAHARASHTRA, INDIA

Q4 Environmental Science

Pollution Research Pub Date : 2023-01-01 DOI:10.53550/pr.2023.v42i01.015

Y. Murkute

引用次数: 0

Abstract

An attempt has been done to understand the hydrogeochemical characteristics of groundwater from shallow aquifers of Vislon village, a part of WRD watershed (Lat. 20º06’30"N and Long. 79º 07' 00"E). The appropriateness of groundwater has also been checked for various purposes. The groundwater from study area is alkaline and slightly saline in nature. The Ca2+ > Mg2+ > Na+ > K+ and HCO3 - > SO4 2- > Cl- > NO3 - was the ascendancy of cations and anions. The earth metals (Ca + Mg) found to exceed the alkali metals (Na + K). The positive correlation interpreted from interrelationship of Na+ vs Cl- exhibited, silicate weathering process for liberation of ions in groundwater at rock-water interface. In addition the non-lithological source, anthropogenic inputs were also inferred indicating the agricultural fertilizers and domestic wastewaters. All the groundwater samples from the study area are suitable for drinking as well as domestic use. The groundwater from study area is also suitable for irrigation purpose with negligible exceptions

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印度马哈拉施特拉邦chandrapur地区部分WRD流域vislon地区的水文地球化学行为和地下水适宜性

本文对wwrd流域(北纬20º06′30”，东经79º07′00”)Vislon村浅层地下水的水文地球化学特征进行了研究。为了各种目的，地下水的适宜性也进行了检查。研究区地下水为碱性和微盐水。Ca2+ > Mg2+ > Na+ > K+和HCO3 - > SO4 2- > Cl- > NO3 -以阳离子和阴离子为主。土壤金属(Ca + Mg)大于碱金属(Na + K)，从Na+与Cl-的相互关系可以看出，在岩石-水界面处，地下水中离子的释放与硅酸盐风化作用有关。除了非岩性来源外，还推断了农业肥料和生活废水的人为输入。研究区所有地下水样本均适合饮用和生活用水。研究区地下水也适合灌溉，例外情况极少

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Pollution Research Environmental Science-Water Science and Technology

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