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首页> 外文期刊>Journal of water resource and protection >Hydrogeochemistry of Groundwater from Different Aquifer in Dimbhe Command Area of Ghod River, Maharashtra India
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Hydrogeochemistry of Groundwater from Different Aquifer in Dimbhe Command Area of Ghod River, Maharashtra India

机译：来自Ghod River，Maharashtra India的Dimbhe指挥区不同含水层的地下水化学化学

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摘要

The groundwater geochemistry of Dimbhe command area of Ghod River basin was evaluated based on major ions characteristic to decide its suitability for drinking, domestic use, and irrigation. Groundwater samples from different depth (shallow and deep) aquifer were collected and investigated for pH, electrical conductivity (EC), total dissolved solid (TDS), Ca, Mg, Na, K, Cl, SO_4, CO_3, HCO_3, NO_3, Fe, and Mn. The results show that the shallow groundwater is dominated by Ca-HCO_3 and Na-HCO_3 and deep aquifer by Na-HCO_3 water facies. The sodium adsorption ratio (SAR) and salinity hazard indicate that the groundwater from the shallow and deep aquifer is suitable for irrigation purposes, and part of the intermediate aquifer is not suitable for crop irrigation. Groundwater from the shallow and deep aquifer is regarded as fresh water and suitable for drinking, domestic and agricultural irrigation use.
机译：基于主要离子特性评估了Ghod River盆地Dimbhe指挥区的地球化学地球化学，以决定其适合饮用，家庭使用和灌溉。收集来自不同深度（浅层和深层）含水层的地下水样品，并研究了pH，导电性（EC），总溶解固体（TDS），Ca，Mg，Na，K，Cl，SO_4，CO_3，HCO_3，NO_3，FE和mn。结果表明，浅层地下水由Ca-HCO_3和Na-HCO_3和Na-HCO_3水相的深含水层主导。钠吸附比（SAR）和盐度危害表明，来自浅层和深含水层的地下水适合灌溉目的，部分中间含水层不适合作物灌溉。来自浅层和深含水层的地下水被认为是淡水，适合饮酒，国内和农业灌溉用途。

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