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延缓运输通过一个纪水层
Alexander van Geen1, Benjamín C Bostick, Thi Kim Trang Pham
1Lamont-Doherty Earth Observatory, Columbia University, Palisades, New York 10964, USA. avangeen@ldeo.columbia.edu
Nature
|September 13, 2013
概括
东南亚的地下水抽取正在污染安全的普莱斯托时代含水层,从浅层的全新时代来源. 亚是一种.
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:
- 在南亚和东南亚,数以百万计的人面临来自浅层全新纪水层的中毒.
- 较古老,通常不含的普世水层是更安全的饮用水替代品.
- 了解浮世纪含水层中的污染动态对于公共卫生至关重要.
研究的目的:
- 为了重建在越南河内附近的普世水层中最初的污染阶段.
- 为了调查地下水抽取如何影响层在世水层中的水平.
- 评估控制的运输和延迟在含水层系统的因素.
主要方法:
- 重建最初的污染阶段.
- 分析地下水流动条件和氧化还原状态的变化.
- 测量的吸附和运输延迟在含水层的沙子.
主要成果:
- 地下水的抽取诱导了污染 (>120m) 的横向入侵,从全新纪进入纪的含水层.
- 吸附到含水层的沙子上造成了显著的运输延迟 (16-20倍).
- 普莱斯托时代的含层被污染可能会因运输延迟而延迟.
结论:
- 地下水的抽水可以将从浅处的来源调动到更深的,以前安全的含水层中.
- 由于吸附,的运输显著减缓,可能会延迟广泛的污染.
- 地下水资源的管理策略必须考虑的动员和运输动态.
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