人类过程驱动了来自多水层系统的地下水中的硫酸盐的时空变异性:矿山排水造成的稀释
Chenyu Wang1, Ankun Luo2, Shen Qu3
1China University of Geosciences, Beijing 100083, China.
Journal of contaminant hydrology
|May 1, 2024
概括
中国西北部的矿井排水改变了地下水流动,影响了硫酸盐水平. 稀释,而不是化氧化,控制硫酸盐演变,影响表面和地下水质量.
科学领域:
- 水地地化学 水地地化学
- 环境科学 环境科学
- 同位素水文学 同位素水文学
背景情况:
- 采矿活动和矿井排水对全球地表水和地下水质量产生重大影响.
- 了解受采矿影响的地下水系统中的硫酸盐演变对于资源管理至关重要.
研究的目的:
- 为了研究矿井排水对中国西北地区多水表系统中硫酸盐演变的影响.
- 区分硫酸盐来源和由煤矿开采影响的进化途径.
主要方法:
- 使用了多同位素分析 (δ34SSO4, δ18OSO4, δD, δ18O水).
- 应用正矩阵因子化 (PMF) 模型来识别硫酸盐来源.
- 分析了罗纪和罗纪水层和地表水的水地化学特征.
主要成果:
- 最初,罗纪的含水层表现出石膏溶解,而热的含水层和地表水则以碳酸盐为主.
- 煤炭开采导致水层硫酸盐增加,这是由于矿井排水造成的.
- 变化的地下水流和增强的含水层连接导致所有水体的硫酸盐稀释.
结论:
- 矿井排水引起的地下水流量变化,而不是矿氧化,控制了硫酸盐的演变.
- 罗纪水层中的水地化学变化模仿了水条件,需要仔细识别来源.
- 通过阐明水地化学过程,这些发现有助于管理矿业影响地区的地下水资源.
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