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矿区开采对水环境的破坏过程——同位素和水化学示踪剂的结合。

Destruction processes of mining on water environment in the mining area combining isotopic and hydrochemical tracer.

机构信息

Institute of Loess Plateau, Shanxi University, Taiyuan, Shanxi, 030006, China.

College of Environmental and Resource Sciences, Shanxi University, Taiyuan, Shanxi, 030006, China.

出版信息

Environ Pollut. 2018 Jun;237:356-365. doi: 10.1016/j.envpol.2018.02.002. Epub 2018 Mar 15.

Abstract

There is less research on the hydrological system and its destruction processes mechanism in the mining areas, especially combined application of isotope technology and chemical signals, which is a key scientific problem that need to be solved. This study takes Jinci spring area in Shanxi as a case study. It is based on the data of hydrology and mining condition from 1954 to 2015, combining monitoring experiments, O, D, S and N tracing, chemical and model simulation. This study investigates the hydrological regularity and impacts of mining activities on water quantity and quality, and reveals the destruction process of hydrological system. The results show that: (1) Water chemical type shows an evolutionary trend of HCO-Ca-Mg→SO-HCO-Ca-Mg→SO-Ca-Mg, due to the influence of exploitation and fault zones. Isotope tracer shows that mine pit water is formed by a mixture of pore water, karst water and surface water. (2) Although precipitation and seepage have a certain impact on the reducing of groundwater quantity, over-exploitation of water resource is still the main reason for reducing of groundwater quantity. Under the conditions of keeping the exploitation intensity at the current level or reducing it by 10%, groundwater level shows a declining trend. Under the condition of reducing it by 30%, groundwater level starts to rise up. When reducing by 50%, groundwater level reaches its highest point. Coalmining changes the runoff, recharge and discharge paths. (3) From 1985 to 2015, Water quality in the mining area is worsening. Ca increases by 35.30%, SO increases by 52.80%, and TDS (Total Dissolved Solid) increases by 67.50%. Nitrates come from the industrial and domestic wastewater, which is generated by mining. The percentage of groundwater coming from gypsum dissolusion is 67.51%, and the percentage from coal measure strata water is 34.49%. The water qualities of river branches are generally deteriorated.

摘要

矿区水文系统及其破坏过程机制的研究较少,尤其是同位素技术与化学示踪剂的综合应用,这是需要解决的关键科学问题。本研究以山西晋祠泉域为例,基于 1954 年至 2015 年的水文和采矿条件数据,结合监测实验、O、D、S 和 N 示踪、化学和模型模拟,研究了采矿活动对水量和水质的水文规律及影响,揭示了水文系统的破坏过程。结果表明:(1)受开采和断裂带的影响,水化学类型表现出 HCO-Ca-Mg→SO-HCO-Ca-Mg→SO-Ca-Mg 的演化趋势。同位素示踪表明,矿坑水是由孔隙水、岩溶水和地表水混合形成的。(2)尽管降水和渗漏对地下水减少有一定影响,但过度开采水资源仍是地下水减少的主要原因。在保持当前开采强度或减少 10%的情况下,地下水位呈下降趋势。在减少 30%的情况下,地下水位开始上升。当减少 50%时,地下水位达到最高点。采煤改变了径流、补给和排泄路径。(3)1985 年至 2015 年,矿区水质恶化。Ca 增加了 35.30%,SO 增加了 52.80%,TDS(总溶解固体)增加了 67.50%。硝酸盐来自工业和生活污水,是由采煤产生的。来自石膏溶解的地下水比例为 67.51%,来自煤系地层水的比例为 34.49%。支流的水质普遍恶化。

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