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土壤水分对降雨的反应,这是中国山丘地土壤深度干燥后的降雨反应
Xianzhong Wu1, Xing Wang2, Yuan Teng2
1College of Urban Environment, Lanzhou City University, Lanzhou 730070, China.
The Science of the total environment
|August 1, 2024
概括
在中国,深层土壤干燥.
科学领域:
- 土壤科学 土壤科学
- 水文学的水文学
- 生态生态学 生态生态学
背景情况:
- 深层土壤干燥是中国洛斯高原森林覆盖地区的一个重大问题.
- 了解土壤水分回收对于可持续的土地管理至关重要.
研究的目的:
- 研究影响深层土壤干燥后恢复水分的因素.
- 分析土壤透特性及其对水分补充的影响.
主要方法:
- 使用10米深的地下柱子进行监控.
- 采用自动土壤湿度和气象监测系统 (2014-2019).
- 分类降雨模式和分析月度和年度规模的透.
主要成果:
- 土壤水分回收主要取决于25-49.9毫米和>50毫米的降雨事件.
- 深层土壤的水分补充发生在4月至10月之间,蒸发损失很大.
- 每月透深度与每月降雨量有二次关系 (R2 = 0.9577).
- 每年的深层土壤水分补充依赖于多年的累积透.
结论:
- 洛斯高原的深层土壤水分回收是一个缓慢的过程,通常需要多年的降水积累.
- 降雨强度和季节性模式显著影响土壤透和水分补充.
- 这些发现对于了解半干旱干旱土壤地区的水文过程至关重要.
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