Research BackgroundThe hydrological processes of plants in forest ecosystems of arid regions are an essential component of regional water cycles. They not only influence community structure, ecological functions, and productivity but also affect the regional balance of matter and energy. As the primary source of water input into arid ecosystems, precipitation exhibits significant seasonal variability and limited temporal availability. The coniferous forests at the northern foothills of the Tianshan Mountains represent a typical cool-temperate forest characterized by relatively abundant rainfal...
release time:
2026
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09
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01
Views：4
Research BackgroundIn karst regions, the soil layer is shallow and bedrock is often exposed. Groundwater distribution varies significantly across different soil layers and rock fractures, making water availability a critical factor limiting vegetation restoration and long-term stability. Limestone and dolomite differ markedly in terms of weathering degree, soil thickness, and fracture structure, which may further influence plant root water uptake, xylem water transport, and leaf transpiration processes. However, existing studies have largely focused on the impacts of climate or vegetation type...
release time:
2026
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07
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25
Views：3
Against the backdrop of global change, the water cycle is being reshaped. How does precipitation enter the soil? How is soil water absorbed by plants? Does deep soil water contribute to groundwater recharge? These questions may seem disparate, yet they all point to the same critical medium—the soil water.Recently, the team led by Professor Zhu Guofeng from Northwest Normal University published a data paper in Scientific Data, presenting and releasing a global-scale dataset of stable isotopes in soil water. This dataset systematically integrates observations of stable hydrogen and oxygen isotop...
release time:
2026
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07
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10
Views：0
Research BackgroundGlobal warming is accelerating the degradation of permafrost in high-altitude cold regions and is also altering the way rivers receive water. The Qinghai-Tibet Plateau is the world’s largest and highest-altitude permafrost region, as well as an important source area for numerous rivers. As the active layer of permafrost deepens and seasonal freeze-thaw processes intensify, the connections among surface water, soil water, and groundwater are being reshaped, leading to changes in the sources of river runoff. Previous studies have shown that precipitation, snowmelt, soil water,...
release time:
2026
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06
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18
Views：0