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印度南部部分硬岩含水层地下水的地球化学特征及用于饮用、灌溉和工业目的的地下水质量评价

Geochemical characteristics and quality of groundwater evaluation for drinking, irrigation, and industrial purposes from a part of hard rock aquifer of South India.

机构信息

Department of Geology, Andhra University, Visakhapatnam, 530 003, India.

Anuhya Architects, Sreeramnagar Colony, Hyderabad, 500 050, India.

出版信息

Environ Sci Pollut Res Int. 2021 Jun;28(24):31941-31961. doi: 10.1007/s11356-021-12404-z. Epub 2021 Feb 22.

DOI:10.1007/s11356-021-12404-z
PMID:33619616
Abstract

The present study is a part of hard rock aquifer of Telangana, South India, where the groundwater is withdrawn heavily for drinking, irrigation, and small-scale industrial purposes. Geochemical characteristics explain the chemical processes, which control the groundwater chemistry and consequently the groundwater quality, while the chemical quality of groundwater is adversely affected by anthropogenic activities, which damage the water environment. The focus of the present study was, thus, to know the origin of geochemical characteristics and also to evaluate the quality of groundwater for various purposes for taking the suitable remedial measures to provide safe water to the local community. Geochemical relations (GR) and hierarchical cluster analysis (HCA) were used to assess the geochemical characteristics. Entropy weighted groundwater quality index (EWGQI), United States Soil Salinity Laboratory Staff (USSLS)'s diagram, and groundwater quality criteria for water supply pipes (GQCW) were used to evaluate the groundwater quality for drinking, irrigation, and industrial purposes, respectively. The study found that the water-rock interactions associated with ion exchange and evaporation were the prime geochemical factors controlling the geochemical characteristics and the anthropogenic activities as the secondary factor. These observations were further supported by HCA. According to the EWGQI, 34.97% of the spatial area was found to have the poor and very poor groundwater quality zones for drinking purpose, because of the dominance of TDS, Na, Cl, [Formula: see text], [Formula: see text], and F contents in the groundwater system. Based on the USSLS's diagram, 79.55% of the present study area was observed to be poor and very poor water quality type for irrigation utilization due to salinity hazard. The GQCW demonstrated that the 7.91% and 8.82% of the areas were not suitable for industrial purpose due to influence of incrustation based on [Formula: see text] and [Formula: see text], respectively, and 1.85%, 12.32%, and 1.25 of the areas are unfit due to influence of corrosion based on pH, TDS, and Cl, respectively. Therefore, boiling, activated carbon filter, rainwater harvesting, suitable coatings on metal surfaces of water supply pipes, etc. are the important suggested effective strategic measures to provide safe water for drinking, irrigation, and industrial purposes.

摘要

本研究是印度南部特伦甘纳邦硬岩含水层的一部分,该地区地下水被大量开采用于饮用、灌溉和小规模工业用途。地球化学特征解释了控制地下水化学并因此影响地下水质量的化学过程,而人为活动会对地下水质量造成不利影响,破坏水环境。因此,本研究的重点是了解地球化学特征的起源,并评估各种用途的地下水质量,以便采取适当的补救措施为当地社区提供安全用水。地球化学关系(GR)和层次聚类分析(HCA)用于评估地球化学特征。熵权地下水质量指数(EWGQI)、美国土壤盐度实验室工作人员(USSLS)图和供水管地下水质量标准(GQCW)分别用于评估饮用水、灌溉和工业用途的地下水质量。研究发现,与离子交换和蒸发有关的水-岩相互作用是控制地球化学特征的主要地球化学因素,人为活动是次要因素。这些观察结果得到了 HCA 的进一步支持。根据 EWGQI,由于地下水系统中 TDS、Na、Cl、[Formula: see text]、[Formula: see text]和 F 含量占主导地位,34.97%的空间区域被认为是饮用水质量较差和极差的区域。根据 USSLS 的图,由于盐分危害,本研究区 79.55%的地区被认为是灌溉利用的水质较差和极差的类型。GQCW 表明,由于[Formula: see text]和[Formula: see text]的影响,分别有 7.91%和 8.82%的地区不适合工业用途,由于 pH、TDS 和 Cl 的影响,分别有 1.85%、12.32%和 1.25%的地区不适合工业用途。因此,煮沸、活性炭过滤、雨水收集、供水管金属表面的适当涂层等是提供饮用水、灌溉和工业用途安全用水的重要建议有效战略措施。

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