Observation and Research Station of Eco-Hydrology and Environmental Protection by
Stable Isotope Tracing in High and Cold Mountainous Areas/Key Laboratory of
Ecohydrology of Inland River Basin/Gansu Qilian Mountains Ecology Research
Center, Northwest Institute of Eco-Environment and Resources, Chinese
Academy of Sciences, Lanzhou 730000, China
Ling-Ling Song
College of Forestry, Gansu Agricultural University, Lanzhou, Gansu
730070, China
Juan Gui
Observation and Research Station of Eco-Hydrology and Environmental Protection by
Stable Isotope Tracing in High and Cold Mountainous Areas/Key Laboratory of
Ecohydrology of Inland River Basin/Gansu Qilian Mountains Ecology Research
Center, Northwest Institute of Eco-Environment and Resources, Chinese
Academy of Sciences, Lanzhou 730000, China
Jian Xue
Observation and Research Station of Eco-Hydrology and Environmental Protection by
Stable Isotope Tracing in High and Cold Mountainous Areas/Key Laboratory of
Ecohydrology of Inland River Basin/Gansu Qilian Mountains Ecology Research
Center, Northwest Institute of Eco-Environment and Resources, Chinese
Academy of Sciences, Lanzhou 730000, China
Bai Juan Zhang
College of Energy and Power Engineering, Lanzhou University of
Technology, Lanzhou 730050, China
Wen De Gao
College of Energy and Power Engineering, Lanzhou University of
Technology, Lanzhou 730050, China
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169
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EndNote: 169
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Total article views: 3,787 (including HTML, PDF, and XML)
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2,875
839
73
3,787
98
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BibTeX: 98
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356
290
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667
33
35
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Total article views: 4,454 (including HTML, PDF, and XML)
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Total article views: 3,787 (including HTML, PDF, and XML)
Thereof 3,450 with geography defined
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Total article views: 667 (including HTML, PDF, and XML)
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This study mainly explores the hydraulic relations, recharge–drainage relations and their transformation paths, and the processes of each water body. It determines the composition of runoff, quantifies the contribution of each runoff component to different types of tributaries, and analyzes the hydrological effects of the temporal and spatial variation in runoff components. More importantly, we discuss the hydrological significance of permafrost and hydrological processes.
This study mainly explores the hydraulic relations, recharge–drainage relations and their...
