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矿山关闭后地下水供应坑湖的液压演变
Birte Moser1, Peter G Cook1, Anthony D Miller2
1College of Science and Engineering, National Centre for Groundwater Research and Training (NCGRT), Flinders University, P.O. Box 2100, Adelaide, South Australia, 5001, Australia.
Ground water
|June 3, 2024
概括
矿山关闭后,干旱地区的坑湖经常成为通道流系统,将水释放到含水层中. 这种过渡会影响长期的水质,并受到蒸发和液压梯度等因素的影响.
科学领域:
- 水文地质学 水文地质学
- 环境科学 环境科学
- 采矿工程 采矿工程 采矿工程
背景情况:
- 开放式采矿降低了区域的地下水位,需要排水.
- 矿山关闭允许地下水恢复,形成坑洞湖.
- 干旱地区的坑湖充当终端水槽或通道系统.
研究的目的:
- 为了了解地下水养坑湖的液压演变.
- 确定影响坑湖从终端水槽向通流系统过渡的因素.
- 为评估坑湖水力状况提供工具.
主要方法:
- 使用了数字地下水建模.
- 分析区域液压梯度,含水层特性,净蒸发率和坑洞几何.
- 为稳定状态条件开发一个近似的分析解决方案.
主要成果:
- 坑湖经常在区域水表恢复之前过渡到通流系统.
- 透流可以在20年内发生,即使是低梯度或高蒸发.
- 坑湖只在特定条件下 (高蒸发,低梯度,低导电性) 保持终端水槽.
结论:
- 坑湖的液压状况 (终端水槽与通道流) 对采矿后的水质至关重要.
- 了解坑洞湖的演变对于矿山关闭和土地利用规划至关重要.
- 数字和分析模型有助于预测坑湖行为.
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