基于环境同位素的重度废弃的水文过程的特殊性在内和外盆地之间的过渡区内
Juan Gui1, Zongxing Li2, Baijuan Zhang2
1Observation and Research Station of Eco-Hydrology and National Park By Stable Isotope Tracing in Alpine Region/ Gansu Qilian Mountains Ecology Research Center/ Key Laboratory of Ecological Safety and Sustainable Development in Arid Lands, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, 730000, China; University of Chinese Academy of Sciences, Beijing, 100049, China.
Journal of environmental management
|June 4, 2023
概括
降水是中国连山脉河流的主要来源. 受冰层影响的河流显示出不确定的水源,原因是复杂的排水过程和海拔对融水贡献的高度影响.
科学领域:
- 水文学的水文学
- 冰川学的冰川学
- 环境科学 环境科学
背景情况:
- 冰层变化对山区的水资源产生重大影响.
- 了解流水形成对于该地区的水资源管理至关重要.
研究的目的:
- 在强烈的废弃期内量化评估排水组成部分和形成过程.
- 分析海拔高度对内盆地和外盆地之间过渡区的水源的影响.
主要方法:
- 1906年样本的稳定同位素分析.
- 在2018年,2020年和2021年8月期间进行了调查.
- 专注于中国连山脉的过渡区.
主要成果:
- 降水是河流流失的主要来源,随着海拔的降低而增加.
- 冰川/雪融水和永久土水的贡献随着海拔的增加而减少.
- 受冰层影响的河流对同位素的高度影响较小,排水成分较慢.
结论:
- 受冰层影响的河流的水源比不受影响的河流更不确定.
- 这些河流的下水流包括在供应地表流之前转化为地下水.
- 未来的研究将专注于极端事件和冲流演变的预测模型.
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