Rationale for alternative water sources for mining regions with high environmental footprint on the example of Levikha village of the Sverdlovsk region

IF 0.2 Q4 FORESTRY
L. Rybnikova, P. Rybnikov, Roman Shapochkin
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Abstract

Introduction. Mine drainage has always been one of the main threats to the hydrosphere of mining areas, both during and after active mining. The most common method of mine water neutralization is associated with the slaked lime. On the abandoned Levikha copper-sulphide mine territory (Sverdlovsk region), acid mine drainage discharge reaches 3,000 m³/day. To neutralize acid waters, more than 400 m³/day of water with a neutral pH is required (to produce the slaked lime). Due to the worn out state of water pipe from the river Tagil, heavy losses, and frequent accidents, the neutralization station receives no more than half of the required amount of water. As a result, the neutralization technology is violated, acid mine drainage is not properly cleaned, the regulatory requirements for wastewater are not achieved, and sulfate waters with increased mineralization and metal concentrations are discharged into the river Tagil. Research objective is to substantiate the possibility of finding sources of drinking, household and process water supply for Levikha village and acid mine drainage neutralization stations by applying groundwater. Methods of research include a comprehensive approach containing research results analysis and field and laboratory research data processing. Results and discussion. Promising areas have been identified representing private catchment areas of potential water intakes with the most favorable conditions for underground runoff. A combination of the following factors was the criterion for promising areas and load points: favorable geological and tectonic conditions (the presence of tectonic faults); groundwater inflow testing results (relatively high specific flow rates of wells); geomorphological position (confinement to low relief areas, location near surface sources of groundwater recharge); hydrochemical sampling data (satisfactory chemical composition of groundwater); sanitary and hygienic situation (absence of potential sources of pollution in the local catchment area). Conclusions. The total resources of the five promising sites are 1,340 m3 /day, including 282 m3 /day for drinking purposes. Exploration and development of promising areas no. II (favorable geological and tectonic conditions within it are confirmed by the groundwater inflow testing results) and no. III (favorable sanitary and hygienic conditions) seem to be the most reasonable. These sites might cover half of the village water needs for drinking and household purposes.
以斯维尔德洛夫斯克地区列维哈村为例,为环境足迹高的矿区提供替代水源的理由
介绍。矿井排水一直是矿区水圈的主要威胁之一,无论是在活跃开采期间还是开采后。矿井水中和最常用的方法是与熟石灰相结合。在废弃的Levikha硫化铜矿区(斯维尔德洛夫斯克地区),酸性矿井排放达到3000立方米/天。为了中和酸性水,需要超过400立方米/天的中性pH水(以生产熟石灰)。由于来自塔吉尔河的水管磨损严重,损失严重,事故频发,中和站的水量不足所需水量的一半。结果,违反了中和技术,酸性矿水没有得到很好的净化,没有达到废水的监管要求,导致矿化度和金属浓度增加的硫酸盐水排入塔吉尔河。研究目的是证实利用地下水为Levikha村和酸性矿井排水中和站寻找饮用水、家庭用水和工艺用水来源的可能性。研究方法包括研究结果分析和现场和实验室研究数据处理的综合方法。结果和讨论。有希望的地区已被确定,代表潜在取水的私人集水区,具有最有利的地下径流条件。以下因素的组合是有利地区和荷载点的标准:有利的地质和构造条件(构造断裂的存在);地下水流入测试结果(井比流量较高);地貌位置(限制在低起伏地区,靠近地表地下水补给源);水化学采样数据(地下水化学成分满意);卫生和卫生状况(当地集水区没有潜在污染源)。结论。5个有潜力的场地的总资源量为1340立方米/天,其中饮用水282立方米/天。勘探开发潜力区II(地下水入流试验结果证实区内地质构造条件优越);第三(良好的卫生条件)似乎是最合理的。这些站点可以满足村庄饮用水和家庭用水需求的一半。
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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