Major ion chemistry and suitability of groundwater resources for different utilizations in mica mining areas, Jharkhand, India

IF 0.9 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS
Soma Giri, Ashwani Kumar Tiwari, Mukesh Kumar Mahato, Abhay Kumar Singh
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引用次数: 0

Abstract

Groundwater resources in mica mining areas of Jharkhand are vital for local communities, agriculture, and domestic utilization. The study investigates the major ion chemistry of groundwater in the mica mining regions, focusing on key physicochemical parameters such as pH, electrical conductivity (EC), total dissolved solids (TDS), and concentrations of major cations (Ca²⁺, Mg²⁺, Na⁺, K⁺) and anions (HCO₃⁻, Cl⁻, SO₄²⁻, NO₃⁻, F). Groundwater samples from the study area were collected before the monsoon season, during the monsoon season, and after the monsoon season. The hydro-chemical analysis reveals that groundwater in the mica mining zones exhibits elevated levels of dissolved ions, with NO₃⁻, F, Ca²⁺, Mg²⁺ and total hardness exceeding permissible limits set by Bureau of Indian Standards (BIS) for drinking purposes at some locations. Water Quality Index (WQI) assessments suggest that a significant proportion of groundwater samples fall into the “good” to “very good” category for drinking and about 29% of the samples fall under the “poor” category. The groundwater was generally suitable for irrigational use with exception of a few due to high salinity. The principal component analysis revealed rock weathering as a dominant source of ions along with anthropogenic sources like mining and agriculture contributing minorly to the ionic load. The predominant hydro-chemical facies identified were Ca-Mg-HCO3 and Ca-Mg-Cl-SO4 types. Both carbonate and silicate weathering play an important role in the geochemical signature of the groundwater in the area. The study implicates the potential health impacts of using the groundwater as drinking water without treatment at a few locations owing to high fluoride, nitrate and dissolved solids. The study also highlights the need for sustainable water management practices and regular monitoring of groundwater quality to mitigate the anthropogenic impacts on groundwater resources.

印度贾坎德邦云母矿区地下水不同利用方式的主要离子化学及适宜性
贾坎德邦云母矿区的地下水资源对当地社区、农业和家庭利用至关重要。该研究调查了云母矿区地下水的主要离子化学,重点研究了关键的物理化学参数,如pH、电导率(EC)、总溶解固形物(TDS),以及主要阳离子(Ca 2 +、Mg 2 +、Na +、K +)和阴离子(HCO₃⁻,Cl⁻,SO₄²⁻,NO₃⁻,F−)的浓度。研究区地下水样品分别在季风季节前、季风季节中和季风季节后采集。水化学分析表明,云母矿区的地下水中溶解离子的含量较高,NO₃⁻、F−、Ca 2⁺、Mg 2⁺和总硬度在一些地方超过了印度标准局(BIS)规定的饮用水标准。水质指数(WQI)评估表明,相当大比例的地下水样本属于“良好”至“非常好”的饮用类别,约29%的样本属于“差”类别。地下水除少数盐分高的地区外,一般适合灌溉。主成分分析表明,岩石风化是离子负荷的主要来源,而采矿和农业等人为来源对离子负荷的贡献较小。确定的主要水化学相为Ca-Mg-HCO3型和Ca-Mg-Cl-SO4型。碳酸盐岩和硅酸盐风化在该区地下水地球化学特征中都起着重要作用。该研究表明,由于氟化物、硝酸盐和溶解固体含量高,在一些地方使用地下水作为饮用水而不进行处理可能对健康产生影响。该研究还强调需要可持续的水管理实践和定期监测地下水质量,以减轻人为对地下水资源的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Geochemical Transactions
Geochemical Transactions 地学-地球化学与地球物理
CiteScore
3.70
自引率
4.30%
发文量
2
审稿时长
>12 weeks
期刊介绍: Geochemical Transactions publishes high-quality research in all areas of chemistry as it relates to materials and processes occurring in terrestrial and extraterrestrial systems.
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