利用熵加权法和地球化学模型评价印度Vindhyan地区一个潜水含水层的水化学

IF 1.4 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
Ashutosh Mishra, Aman Rai, Prabuddh Kumar Mishra, Suresh Chand Rai
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引用次数: 2

摘要

潜水含水层的地下水质量监测和地球化学特征对于确保人人普遍公平地获得清洁、可靠和廉价的饮用水至关重要。本研究旨在调查印度萨特纳区地下水的水文地球化学特征和调节地下水化学的机制,并评估地下水质量的空间变化。为此,结合熵加权水质指数(EWQI)、多元统计、地球化学建模和地理信息系统,分析了2020年5月38个潜水含水层位置的地下水数据,其中包括13个物理化学参数。研究结果表明,地下水是新鲜的,呈微碱性。硬度是一个重大问题,因为57.89%的样本超过了世界卫生组织的允许限值。离子的优势顺序为Ca2+ >; Na+ >; Mg2+ >; K+和HCO3− >; SO42− >; Cl− >; NO3− >; F−。这些离子的较高浓度主要集中在东北部和东部地区。Pearson相关分析和主成分分析(PCA)表明,自然因素和人为因素共同调节着该地区的地下水化学。Q型凝聚层次聚类分析突出了三个重要的水聚类。Ca–HCO3是所有三个簇中最普遍的水化学相。通过各种常规地块进行的地球化学建模表明,研究区域的地下水化学受到方解石/白云石溶解、反向离子交换以及硅酸盐和岩盐风化的影响。研究区域的EWQI数据显示,73.69%的样本适合饮用。由于盐度高、镁(Mg2+)、硝酸盐(NO3−)和碳酸氢盐(HCO3−)浓度高,中北部和东北部地区特别容易受到影响。政策制定者和地下水管理者可以完成这项研究的结果,以实现区域范围内的可持续地下水开发。
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 hydro-chemistry in a phreatic aquifer in the Vindhyan Region, India, using entropy weighted approach and geochemical modelling

Groundwater quality monitoring and geochemical characterization in the phreatic aquifer are critical for ensuring universal and equitable access to clean, reliable, and inexpensive drinking water for all. This research was intended to investigate the hydrogeochemical attributes and mechanisms regulating the chemistry of groundwater as well as to assess spatial variation in groundwater quality in Satna district, India. To accomplish this, the groundwater data comprising 13 physio-chemical parameters from thirty-eight phreatic aquifer locations were analysed for May 2020 by combining entropy-weighted water quality index (EWQI), multivariate statistics, geochemical modelling, and geographical information system. The findings revealed that the groundwater is fresh and slightly alkaline. Hardness was a significant concern as 57.89% of samples were beyond the permissible limit of the World Health Organisation. The dominance of ions were in the order of Ca2+  > Na+  > Mg2+  > K+ and HCO3 > SO42− > Cl > NO3 > F. Higher concentration of these ions is mainly concentrated in the northeast and eastern regions. Pearson correlation analysis and principal component analysis (PCA) demonstrated that both natural and human factors regulate groundwater chemistry in the region. The analysis of Q-mode agglomerative hierarchical clustering highlighted three significant water clusters. Ca–HCO3 was the most prevalent hydro-chemical facies in all three clusters. Geochemical modelling through various conventional plots indicated that groundwater chemistry in the research region is influenced by the dissolution of calcite/dolomite, reverse ion exchange, and by silicate and halite weathering. EWQI data of the study area disclosed that 73.69% of the samples were appropriate for drinking. Due to high salinity, Magnesium (Mg2+), Nitrate (NO3), and Bicarbonate (HCO3) concentrations, the north-central and north-eastern regions are particularly susceptible. The findings of the study may be accomplished by policymakers and groundwater managers to achieve sustainable groundwater development at the regional scale.

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来源期刊
Acta Geochimica
Acta Geochimica GEOCHEMISTRY & GEOPHYSICS-
CiteScore
2.80
自引率
6.20%
发文量
1134
期刊介绍: Acta Geochimica serves as the international forum for essential research on geochemistry, the science that uses the tools and principles of chemistry to explain the mechanisms behind major geological systems such as the Earth‘s crust, its oceans and the entire Solar System, as well as a number of processes including mantle convection, the formation of planets and the origins of granite and basalt. The journal focuses on, but is not limited to the following aspects: • Cosmochemistry • Mantle Geochemistry • Ore-deposit Geochemistry • Organic Geochemistry • Environmental Geochemistry • Computational Geochemistry • Isotope Geochemistry • NanoGeochemistry All research articles published in this journal have undergone rigorous peer review. In addition to original research articles, Acta Geochimica publishes reviews and short communications, aiming to rapidly disseminate the research results of timely interest, and comprehensive reviews of emerging topics in all the areas of geochemistry.
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