Arid
DOI10.1016/j.jhydrol.2019.01.003
Water resources in inland regions of central Asia: Evidence from stable isotope tracing
Li, Zongxing1; Gui, Juan1; Wang, Xufeng1; Feng, Qi1; Zhao, Tongtiegang3; Ouyang, Chaojun2; Guo, Xiaoyan1; Zhang, Baijuan1; Shi, Yang1
通讯作者Li, Zongxing ; Feng, Qi
来源期刊JOURNAL OF HYDROLOGY
ISSN0022-1694
EISSN1879-2707
出版年2019
卷号570页码:1-16
英文摘要Complex hydrological processes affect valuable water resources in inland regions across arid central Asia. Historically, this was a critical part of the Silk Road, and it is now named the modern Silk Road Economic Belt. Using the Qilian Mountains and Hexi Corridor in China as a case-study of the inland region, we collected a total of 2311 water samples from the area and performed a comprehensive investigation of the water cycle. Results from stable isotope tracing indicate clear spatial patterns. In the upstream mountainous regions, glacier snow meltwater becomes groundwater at the periglacial belt. Supra-permafrost water develops into river runoff in the permafrost region. There are also frequent exchanges between groundwater and river runoff along the vegetation belt. In the middle/downstream region, river runoff becomes groundwater. Throughout these processes, both river runoff and groundwater are consumed by evapotranspiration, are recycled, and make a substantial contribution to precipitation. Overall, the upstream mountainous region is a critical part of the water resources. The cryosphere belt accounts for 44% of the mountainous region but contributes to about 80% of water resources. Recycling of moisture also plays an important role. During the summer months (May to September) moisture recycling accounted for 24% and 14% of precipitation in upstream and middle/downstream regions, respectively. The findings from the stable isotope tracing provide insights into hydrological processes and can help improve water management in inland regions of Central Asia.
英文关键词Inland region Stable isotope Water cycle Hydrological process
类型Article
语种英语
国家Peoples R China ; Australia
收录类别SCI-E
WOS记录号WOS:000460709400001
WOS关键词HEIHE RIVER-BASIN ; TIBETAN PLATEAU ; HYDROGRAPH SEPARATION ; DEUTERIUM EXCESS ; QILIAN MOUNTAINS ; ABLATION PERIOD ; MINQIN BASIN ; PRECIPITATION ; EVOLUTION ; NORTH
WOS类目Engineering, Civil ; Geosciences, Multidisciplinary ; Water Resources
WOS研究方向Engineering ; Geology ; Water Resources
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/217131
作者单位1.Chinese Acad Sci, Key Lab Ecohydrol Inland River Basin, Gansu Qilian Mt Ecol Res Ctr, Northwest Inst Ecoenvironm & Resources, Lanzhou 730000, Gansu, Peoples R China;
2.Chinese Acad Sci, Inst Mt Hazards & Environm, Key Lab Mt Hazards & Earth Surface Proc, Chengdu 610041, Sichuan, Peoples R China;
3.Univ Melbourne, Sch Engn, Parkville, Vic, Australia
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GB/T 7714
Li, Zongxing,Gui, Juan,Wang, Xufeng,et al. Water resources in inland regions of central Asia: Evidence from stable isotope tracing[J],2019,570:1-16.
APA Li, Zongxing.,Gui, Juan.,Wang, Xufeng.,Feng, Qi.,Zhao, Tongtiegang.,...&Shi, Yang.(2019).Water resources in inland regions of central Asia: Evidence from stable isotope tracing.JOURNAL OF HYDROLOGY,570,1-16.
MLA Li, Zongxing,et al."Water resources in inland regions of central Asia: Evidence from stable isotope tracing".JOURNAL OF HYDROLOGY 570(2019):1-16.
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