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Soil property changes following a thaw-induced mass movement event in the permafrost region of the Qinghai-Tibetan Plateau

Jiahui Yang, Ruhan Zhang, Xiaobin Li, Xiangwei Wang, Miles Dyck, Luyang Wang, Qingbai Wu, Hailong He*

Catena, 252: 108850 (2025)

论文解读

本研究调查了青藏高原多年冻土区热融滑塌事件后的土壤性质变化。热融作用引发的质量运动显著改变了土壤理化性质和碳氮储量,揭示了气候变暖背景下冻土退化对土壤生态系统的深远影响。

图文摘要:青藏高原热融滑塌后土壤性质变化
图文摘要:青藏高原热融滑塌后土壤性质变化

研究要点

  • 调查青藏高原热融滑塌后土壤性质变化
  • 热融事件显著改变了土壤理化性质和碳氮储量
  • 揭示了冻土退化对土壤生态系统的深远影响
  • 为气候变暖下冻土区生态风险评估提供依据

引用格式

APA

Jiahui Yang, Ruhan Zhang, Xiaobin Li, Xiangwei Wang, Miles Dyck, Luyang Wang, Qingbai Wu, Hailong He (2025). Soil property changes following a thaw-induced mass movement event in the permafrost region of the Qinghai-Tibetan Plateau. Catena, 252, 108850. https://doi.org/10.1016/j.catena.2025.108850

BibTeX
@article{Yang2025,
  author    = {Jiahui Yang, Ruhan Zhang, Xiaobin Li, Xiangwei Wang, Miles Dyck, Luyang Wang, Qingbai Wu, Hailong He},
  title     = {Soil property changes following a thaw-induced mass movement event in the permafrost region of the Qinghai-Tibetan Plateau},
  journal   = {Catena},
  year      = {2025},
  volume    = {252},
  pages     = {108850},
  doi       = {10.1016/j.catena.2025.108850},
}