Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1016/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![]() | |
通讯作者 | Li, Zongxing ; Feng, Qi |
来源期刊 | JOURNAL OF HYDROLOGY
![]() |
ISSN | 0022-1694 |
EISSN | 1879-2707 |
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 |
推荐引用方式 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. |
条目包含的文件 | 条目无相关文件。 |
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。