Soil water components control plant water uptake along a subalpine elevation gradient on the Eastern Qinghai-Tibet Plateau

Sun, Juying; Sun, Xiangyang; Wang, Genxu; Dong, Wenchang; Hu, Zhaoyong; Sun, Shouqin; Wang, Fei; Song, Chunlin; Lin, Shan

doi:10.1016/j.agrformet.2023.109827

Cited by 4 publications

(1 citation statement)

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“…Soil water is an important ecological factor and is also holding great significance for climate modeling and prediction [2]. Soil water plays an important role in maintaining biodiversity, promoting vegetation growth, improving the surface environment, and revealing pollution migration [3][4][5][6]. T S is an important indicator of climate change [2] and is one of the key factors affecting the growth and development of plants and soil microorganisms.…”

Section: Introductionmentioning

confidence: 99%

Soil Hydrothermal Dynamics in the Hengduan Mountains of Southeast Tibet and Associated Influencing Factors

Meng,

Li,

Zhang

et al. 2024

Water

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Soil water and soil temperature are important ecological factors and driving forces for ecosystem restoration and sustainable development, possessing great significance for climate modeling and prediction. The Hengduan Mountains in southeastern Tibet, China, are located in a climate-change-sensitive area, and the study of soil hydrothermal dynamics in this area is of great significance for local and global climatic change and water resource utilization. This study, based on the soil hydrothermal and meteorological data of the Hengduan Mountain area in Southeast Tibet, analyzes the dynamic change patterns of soil hydrothermal and meteorological factors and explores their influencing relationships. It was found that the dynamic change in soil water content affected by precipitation was “bimodal” type. Among the meteorological factors, soil water content has the strongest correlation with relative humidity. The intra-annual variation curve of soil temperature is similar to that of the atmospheric temperature, showing a “unimodal” type, and has the highest correlation with atmospheric temperature. Specifically, it takes 70 mm and 170 mm of precipitation to change the soil water content and soil temperature at the 150 cm depth. For every 20 °C change in atmospheric temperature, soil temperature above 150 cm changes by an average of 7.2 °C.

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