[基于稳定的和氧同位素的黄河流域内蒙古部分的水转化关系]
Sen-Sen Pei1, Yan-Yun Luo1,2,3, Hao Pan1
1College of Water Conservancy and Civil Engineering, Inner Mongolia Agricultural University, Hohhot 010018, China.
Huan jing ke xue= Huanjing kexue
|December 4, 2024
概括
稳定同位素分析显示,大气降水是黄河流域表面水的主要来源,而表面水主要补充地下水,特别是在干旱季节.
科学领域:
- 环境科学 环境科学
- 水文学的水文学
- 同位素地球化学 同位素地球化学
背景情况:
- 黄河流域的水资源对于干旱和半干旱地区至关重要.
- 了解水体的转变对于可持续的水资源管理至关重要.
研究的目的:
- 分析和氧稳定同位素在降水,地表水和地下水中的时间和空间变化.
- 使用混合模型揭示水体转换关系.
主要方法:
- 收集不同季节 (湿,正常,干) 的大气降水,地表水和地下水样本.
- 稳定同位素分析 (和氧同位素).
- 应用MixSIAR混合模型来进行源分配.
主要成果:
- 地下水的季节性同位素变化最小,表明再生速度缓慢,保留时间长.
- 表面水δD值在雨季比正常和干旱季节更高.
- 表面水的同位素特征表明,在降水充电后的蒸发分化.
- 沿黄河北岸和南岸观察到地表水δD的空间变化.
- 大气降水是表面水的主要来源 (雨季为97.1%),地下水的主要来源是表面水 (雨季为52.4%,在正常季节增加到69.3%,干季为62.2%).
结论:
- 大气降水是表面水的主要来源,在雨季有更高的贡献.
- 地表水是地下水补充的主要来源,其贡献从湿季到干季增加.
- 蒸发显著影响了地表水的同位素组成.
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