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Hydrogeochemistry and multivariate statistical analysis of groundwater quality of hard rock aquifers from Deccan trap basalt in Western India

机译:德克斯特印度德克兰陷阱玄武岩地下水质量的水文地球化学及多元统计分析

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In the present investigation, hydrogeochemistry and multivariate statistical analysis of groundwater quality were assessed from hard rock aquifers of the Deccan trap basalt in the Jalna district of Maharashtra. Groundwater samples (n = 105) were collected from the study area in a systematic grid pattern to avoid biasing in sampling. Water quality parameters of all these groundwater samples were analyzed by standard BIS and APHA procedures by titrimetric and using sensors. Uranium in all samples was analyzed using an LED fluorimeter. Strict quality assurance and quality control features were adopted in all stages of the study to ensure the quality of the data. The observed sequence of the dominance of major cations and anions is Ca2+ Na+ Mg2+ K+ and HCO3- Cl- SO42- respectively. The observed uranium values were in the range of 0.1 to 16.2 mu g/L with an average value of 2.04 mu g/L, well below the safe limits recommended by WHO and AERB i.e. 30 and 60 mu g/L, respectively. Piper trilinear diagram indicates dominant hydrochemical facies of groundwater in the study area are Mixed Ca2+-Na+-HCO3-, Na+-Cl- and Ca+-HCO3- while Gibbs plot infers host rock-water interaction is the major geochemical process in these aquifers. The correlation analysis, cluster analysis, and factor analysis tests are performed. Groundwater was assessed for its suitability for irrigation purposes using multiple indices such as SAR, RSC, and Na percentage. From the estimated indices, it was found that the groundwater in hard rock aquifers of the Deccan trap basalt is suitable for irrigation purposes.
机译:在目前的调查中,从马哈拉施特州杰拉斯特·瓦尔纳区的Deccan Trap玄武岩的硬岩含水层评估了地下水质量的水文地球化学和多元统计分析。从系统网格图案中从研究区域收集地下水样品(n = 105),以避免在取样中偏置。通过标准BIS和APHA程序通过滴定测量和使用传感器来分析所有这些地下水样本的水质参数。使用LED荧光计分析所有样品中的铀。研究的所有阶段都采用了严格的质量保证和质量控制功能,以确保数据的质量。观察到的主要阳离子和阴离子的优势序列是Ca2 +& na +& mg2 +& K +和HCO3-& cl-& SO42-分别。观察到的铀值在0.1至16.2μg/ L的范围内,平均值为2.04μg/ l,远低于WHO和AERB I. 30和60μg/ L推荐的安全限制。 Piper三线性图表明研究区域的地下水的主干水化学相混合Ca2 + -Na + -HCO3-,Na + -Cl-和Ca + -HCO3-而Gibbs Plot Infers宿主岩水相互作用是这些含水层中的主要地球化学过程。执行相关分析,聚类分析和因子分析测试。使用多种指数(如SAR,RSC和NA百分比)评估地下水的适用性。从估计的指数从估计的指数中发现,Deccan陷阱玄武岩的硬质岩含水层的地下水适合灌溉目的。

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