Kumar Nirmal, Tiwari Mahendra Kumar, Singh Rambabu, Singha Sudhakar, Singha Soumya S, Babu K Prasad
Mining Department, Western Coalfield Limited, Nagpur, Maharashtra, 440014, India.
Department of environmental science, AKS University, Satna, Madhya Pradesh, 485001, India.
Geochem Trans. 2025 Apr 13;26(1):2. doi: 10.1186/s12932-025-00098-y.
The quality of water can significantly affect the regional water resources due to scarcity of potable water in industrial area. The purpose of this study was to explore potentially toxic trace elements (PTEs) contamination and their seasonal variations in different water sources within the coal mining area of the Mahan River command area, Central India. To achieve this, 96 water samples were collected across two distinct seasons and analysed for PTEs. The results indicate that during the pre-monsoon season, the concentrations of Mn (18%), Cu (4%), Pb (8%), Ni (18%), Cd (2%), Al (4%), Cr (2%), and Fe (30%) exceeded permissible limits. In the post-monsoon season, Mn (15%), Pb (6%), Ni (15%), Cd (2%), Al (15%), Fe (46%) and Ba (4%) surpassed the standards. The multiple groundwater pollution indexical methods further revealed that 14% [Heavy metal pollution index (HPI)], 14% [Heavy metal evaluation index (HEI)], 18% [Contamination index (CI)], 14% [the entropy-weight based HM contamination index (EHCI)] and 20% [Heavy metal index (HMI)] of the samples exceeded permissible thresholds during the pre-monsoon season. Similarly, during the post-monsoon period, 10% (HPI), 10% (HEI), 15% (CI), 15% (EHCI) and 17% (HMI) of the samples were above acceptable limits. The relationship between the pH of water and the total load of dissolved metals is established using Caboi plot, confirming that mine water from mine water from Bhatgaon Underground (UG), Mahamaya UG, and Mahan Opencast (OC) [PR40, PR41, PR42, PR43, PR47, and PR48], surrounding rivers, and groundwater sources, exhibited an "Acid-High Metal" characteristic. This suggests significant contamination from acid mine drainage and mineral dissolution. Apart from the anthropogenic inputs, geogenic and environmental processes are responsible for the current distribution of PTEs and their seasonal variations.
由于工业区饮用水稀缺,水质会对区域水资源产生重大影响。本研究的目的是探索印度中部马哈讷迪河指挥区煤矿开采区内不同水源中潜在有毒微量元素(PTEs)的污染情况及其季节变化。为此,在两个不同季节采集了96个水样,并对PTEs进行了分析。结果表明,在季风前季节,锰(18%)、铜(4%)、铅(8%)、镍(18%)、镉(2%)、铝(4%)、铬(2%)和铁(30%)的浓度超过了允许限值。在季风后季节,锰(15%)、铅(6%)、镍(15%)、镉(2%)、铝(15%)、铁(46%)和钡(4%)超过了标准。多种地下水污染指数方法进一步显示,在季风前季节,14%[重金属污染指数(HPI)]、14%[重金属评价指数(HEI)]、18%[污染指数(CI)]、14%[基于熵权的重金属污染指数(EHCI)]和20%[重金属指数(HMI)]的样本超过了允许阈值。同样,在季风后时期,10%(HPI)、10%(HEI)、15%(CI)、15%(EHCI)和17%(HMI)的样本高于可接受限值。利用卡博伊图建立了水的pH值与溶解金属总负荷之间的关系,证实来自巴特冈地下矿(UG)、玛哈玛雅UG和马哈讷露天矿(OC)[PR40、PR41、PR42、PR43、PR47和PR48]的矿井水、周边河流和地下水源呈现出“酸性-高金属”特征。这表明酸性矿山排水和矿物溶解造成了严重污染。除了人为输入外,地质成因和环境过程也是造成PTEs当前分布及其季节变化的原因。