表面和地下下水产生过程及其影响因素在中国北部山坡上
Tonggang Fu1, Jintong Liu1, Hui Gao1
1Key Laboratory of Agricultural Water Resources, Hebei Laboratory of Agricultural Water-Saving, Hebei Key Laboratory of Soil Ecology, Center for Agricultural Resources Research, Institute of Genetics and Developmental Biology, Chinese Academy of Sciences, 286 Huaizhong Road, Shijiazhuang 050021, China.
The Science of the total environment
|September 27, 2023
概括
了解山区的排水产生是关键. 土壤和液压导电性 (Ks) 极大地控制了地表和地下水流,影响了水流穿过不同的斜坡位置和土壤层.
科学领域:
- 水文学 水文学
- 土壤科学 土壤科学
- 地质形态学 地质形态学
背景情况:
- 山区的下水流产生对水文循环至关重要.
- 表面和地下排水的机制及其驱动因素需要进一步研究.
研究的目的:
- 调查泰山地区山坡上的排水过程和影响因素.
- 分析土壤特性对地表和地底流水和土壤含水量 (SWC) 的影响.
主要方法:
- 在微型下水场进行降雨模拟实验.
- 分析了表面和地下水流量,土壤含水量 (SWC) 和土壤特性 (Ks, BD, CP, NCP, SOM).
- 检查了不同斜率位置和土壤层的变化.
主要成果:
- 根据土壤深度和斜坡位置,SWC对降雨的反应有显著的变化.
- 表面下水流占据了下坡的优势,而地下下水流占据了中部和上坡的优势.
- 土壤和液压导电性 (Ks) 被确定为控制排水生成的最关键因素.
结论:
- 土壤层之间的水平和垂直Ks的比率决定了地下下水的产生.
- 这些发现有助于更好地理解山地地形中的水文过程.
- 结果为类似环境中的水资源管理提供了宝贵的见解.
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