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探索中国干旱地区不同土壤层内土壤水不足的多方面的原因

Liang He1, Jianbin Guo2, Xuefeng Liu3

  • 1Key Laboratory of State Forestry Administration on Soil and Water Conservation, School of Soil and Water Conservation, Beijing Forestry University, Beijing, China; Key Laboratory for Restoration and Reconstruction of Degraded Ecosystem in Northwest China of Ministry of Education, Ningxia University, Yinchuan, Ningxia, China.

Journal of environmental management
|December 8, 2024
PubMed
概括

干旱地区的土壤含水量通常随着深度的增加而减少. 降水是浅土壤水的关键,而植被 (NDVI) 主导着更深层,极端天气事件显著影响土壤水分动态.

关键词:
气候变化 气候变化 气候变化干旱地区是干旱地区.生态恢复 生态恢复水文循环的水文循环定量贡献 定量贡献不同层面的土壤水动态.

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