印度北部Bhima流域地下水水质适宜性评价:水文地球化学视角

Himanshu Gaikwad, H. Shaikh, B. Umrikar
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引用次数: 5

摘要

为了了解地下水资源质量及其对居民和灌溉的影响,对浅层无承压玄武岩含水层地下水中主要离子成分进行了研究。对Bhima流域上游30个地下水取样进行了分析,测定了主要阳离子和阴离子,建立了水质指数(WQI)和灌溉指标。分析了pH浓度、电导率、总硬度、总溶解固形物、主要阳离子和阴离子。使用Piper三线性图检测地下水类型为Ca2+-HCO3−、Ca2+-Na+-HCO3−、混合Ca2+-Mg2+-Cl−和Ca2+-Cl−基团。在该地区的一些地点发现了高浓度的硝酸盐(8至194毫克/升)。WQI显示66%的样本不适合饮用,因为硝酸盐含量高,主要是由于人为活动而引入的。采用钠吸附比(SAR)、渗透指数(PI)、凯利比(KR)、镁危害(MH)、钠(%)和残余碳酸钠(RSC)等指标确定了地下水的灌溉适宜性。该地区的地下水适合灌溉。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Evaluation of Groundwater Quality for Domestic and Irrigation Suitability from Upper Bhima Basin, Western India: A Hydro-geochemical Perspective
Major ion constituents present in groundwater are studied for shallow unconfined basaltic aquifer in order to understand the quality of groundwater resources and its impacts on inhabitants and irrigation. 30 groundwater samples collected from dug wells located in upper Bhima basin were analyzed to measure major cations and anions for establishing water quality index (WQI) and irrigation indices. The concentration of pH, electrical conductivity, total hardness, total dissolved solids and major cations and anions were analyzed. Groundwater types were detected using Piper’s trilinear diagram as Ca2+-HCO3−, Ca2+-Na+-HCO3−, mixed Ca2+-Mg2+-Cl− and Ca2+-Cl− groups. High concentration (8 to 194 mg/L) of nitrate was found at some locations in the region. WQI shows 66% of the samples to be unfit for drinking purposes due to high nitrate content mostly introduced because of the anthropogenic activities. Suitability of groundwater for irrigation purposes was determined using of Sodium Adsorption Ratio (SAR), Permeability Index (PI), Kelly Ratio (KR), Magnesium Hazard (MH), Sodium (%) and Residual Sodium Carbonate (RSC). Groundwater in the region is suitable for irrigation.
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