用同位素和多种模型确定大流域的地表水的蒸发和演变
Xiang Dong1, Xing Chen2, Fazhi Xie3
1School of Resources and Environmental Engineering, Anhui University, Hefei 230601, China; Laboratory of Mine Ecological Restoration Engineering, Hefei, Anhui Province 230601, China.
Journal of contaminant hydrology
|October 22, 2024
概括
长江的地表水主要是由岩石风化和人类活动形成的. 地质因素主导离子来源,上游蒸发较高.
科学领域:
- 环境科学 环境科学
- 地质化学 地质化学
- 水文学的水文学
背景情况:
- 了解地表水的化学成分对于评估地质影响和人类影响至关重要.
- 长江是中国最大的水源,需要详细研究其离子起源和形成过程.
研究的目的:
- 量化评估长江地表水中的水源补充和蒸发强度.
- 确定主要的离子来源和影响地表水组成的控制因素.
主要方法:
- 使用了水化学分析.
- 使用的稳定同位素 (δ18O, δD).
- 应用Craig-Gordon和APCS-MLR模型进行定量评估.
主要成果:
- 水化学类型的变化在上游 (HCO3−-Ca2+,Na+-K+) 和中游/下游 (HCO3−-Ca2+,SO42−-Ca2+) 之间.
- 岩石气候变化和人类投入是液化化学进化的关键驱动力.
- 地表水由降水补充;上游显示出更高的蒸发强度.
- 地质因素 (80.5%) 是水化成分的主要来源,其次是工业投入 (11.1%) 和农业投入 (6.4%).
结论:
- 这项研究阐明了长江地表水的化学组成,水源和演化机制.
- 这些发现为水质管理和盆地的可持续发展提供了科学基础.
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