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研究控制矿区地下水演变的因素,采用综合方法
Yewei Song1,2,3, Jie Guo1,2, Fangrui Li1,2,3
1Key Laboratory of Shale Gas and Geoengineering, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029,China.
Heliyon
|October 21, 2024
概括
采矿区的地下水演变主要是由浅水,深水和雨水源的混合效应驱动的. 水与岩石的相互作用也显著改变了水地化学特征,影响了水资源管理.
科学领域:
- 环境科学 环境科学
- 水文地质学 水文地质学
- 地质化学 地质化学
背景情况:
- 地下水的演变对于水资源管理和污染控制至关重要.
- 在受严重影响的采矿地区对地下水演变的研究有限.
- 人类活动显著影响地下水的水地化学过程.
研究的目的:
- 调查矿区地下水水地化学演变的主要控制因素.
- 区分自然过程和人类对地下水质量的影响.
- 为采矿地区建立地下水循环模型.
主要方法:
- 层次集群分析和主要组件分析用于地下水分类.
- 液化和同位素分析以确定地下水源.
- 一种三端元素混合模型,用于量化污染源和混合比率.
主要成果:
- 矿区的地下水是浅岩基裂水,深岩基裂水和雨水的混合物.
- 混合效应是影响地下水演变的主要因素,超过了循环深度.
- 水与岩石的相互作用,包括矿物溶解和离子交换,改变了地下水的化学成分.
结论:
- 地下水的混合是采矿区水地化学演变的关键驱动力.
- 水与岩石的相互作用在改变地下水特性方面发挥着重要作用.
- 已建立的水循环模型为采矿环境和类似地质环境中的地下水保护提供了洞察力.
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