在多层含水层系统中,地质的垂直变异性受到限制
Wenhui Liu1, Yao Du1, Wenkai Qiu1
1Key Laboratory of Groundwater Quality and Health China University of Geosciences, Ministry of Education, Wuhan 430078, China; School of Environmental Studies & State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan, 430078, China.
地下水中的地质增加了浅层含水层,这是由于丰富的富含的有机物质,先进的降解和较慢的水流. 这种垂直变化是理解地下水污染的关键.
科学领域:
- 水文地质学 水文地质学
- 环境地质化学环境地质化学
- 水的质量 水的质量
背景情况:
- 地下水中的地质氨含量升高是一个越来越令人担忧的问题.
- 对水层中垂直氨分布的理解是有限的.
研究的目的:
- 描述地质性在多层含水层中的垂直异质性.
- 为了确定控制在浅地下水中缩的控制因素.
主要方法:
- 地下水和地下水层沉积物的水地化学分析.
- 溶解有机物 (DOM) 分子组成的分析.
- 试验用于评估液压导电性.
主要成果:
- 氨的度从深层到浅层含水层显著增加 (2.13到9.88毫克/L N).
- 浅层含水层中的DOM显示了更高的N含量和更多的降解.
- 在较浅的含水层中,液压导电性下降,增强了氨的保留.
结论:
- 地质的垂直变化是由富含的有机物,DOM降解和水力动力学驱动的.
- 结合的因素控制了氨在多层含水层系统中的分布.
- 这些发现对于理解地质地下水污染异质性至关重要.
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