Effects of vegetation extreme degradation on soil hydrothermal processes in alpine wet meadow on the central Qinghai–Tibet Plateau
Author:
Funder
Youth Innovation Promotion Association of the Chinese Academy of Sciences
National Natural Science Foundation of China
Publisher
Elsevier BV
Reference63 articles.
1. Response characteristics of vegetation and soil environment to permafrost degradation in the upstream regions of the Shule River Basin;Chen;Environ. Res. Lett.,2012
2. Carbon and nitrogen cycling on the Qinghai-Tibetan Plateau;Chen;Nat. Rev. Earth Environ.,2022
3. Understory vegetation restoration improves soil physicochemical properties, enzymatic activity, and changes diazotrophic communities in Cunninghamia lanceolata plantations but depends on site history;Ding;Plant Soil,2023
4. Variations in active layer soil hydrothermal dynamics of typical wetlands in permafrost region in the Great Hing’an Mountains, Northeast China;Dong;Ecol. Indic.,2021
5. Spatial and temporal differences in alpine meadow, alpine steppe and all vegetation of the Qinghai-Tibetan Plateau and their responses to climate change;Duan;Remote Sens.,2021
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