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DOI	10.1002/hyp.10495
	Stable isotopic and geochemical identification of groundwater evolution and recharge sources in the arid Shule River Basin of Northwestern China
	Guo, Xiaoyan; Feng, Qi; Liu, Wei; Li, Zongxing; Wen, Xiaohu; Si, Jianhua; Xi, Haiyang; Guo, Rui; Jia, Bing
发表日期	2015
ISSN	0885-6087
EISSN	1099-1085
卷号	29 期号:22
英文摘要	Stable isotopic (D-VSMOW and O-18(VSMOW)) and geochemical signatures were employed to constrain the geochemical evolution and sources of groundwater recharge in the arid Shule River Basin, Northwestern China, where extensive groundwater extraction occurs for agricultural and domestic supply. Springs in the mountain front of the Qilian Mountains, the Yumen-Tashi groundwater (YTG), and the Guazhou groundwater (GZG) were Ca-HCO3, Ca-Mg-HCO3-SO4 and Na-Mg-SO4-Cl type waters, respectively. Total dissolved solids (TDS) and major ion (Mg2+, Na+, Ca2+, K+, SO42-, Cl- and NO3-) concentrations of groundwater gradually increase from the mountain front to the lower reaches of the Guazhou Basin. Geochemical evolution in groundwater was possibly due to a combination of mineral dissolution, mixing processes and evapotranspiration along groundwater flow paths. The isotopic and geochemical variations in melt water, springs, river water, YTG and GZG, together with the end-member mixing analysis (EMMA) indicate that the springs in the mountain front mainly originate from precipitation, the infiltration of melt water and river in the upper reaches; the lateral groundwater from the mountain front and river water in the middle reaches are probably effective recharge sources for the YTG, while contribution of precipitation to YTG is extremely limited; the GZG is mainly recharged by lateral groundwater flow from the Yumen-Tashi Basin and irrigation return flow. The general characteristics of groundwater in the Shule River Basin have been initially identified, and the results should facilitate integrated management of groundwater and surface water resources in the study area. Copyright (c) 2015 John Wiley & Sons, Ltd.
关键词	groundwater stable isotope geochemical evolution recharge sources
学科领域	Water Resources
语种	英语
WOS研究方向	Water Resources
来源期刊	HYDROLOGICAL PROCESSES
来源机构	中国科学院西北生态环境资源研究院
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/111795
作者单位	Chinese Acad Sci, Cold & Arid Reg Environm & Engn Res Inst, Key Lab Ecohydrol Inland River Basin Gansu, Hydrol & Water Resources Engn Res Ctr, Lanzhou 730000, Peoples R China
推荐引用方式 GB/T 7714	Guo, Xiaoyan,Feng, Qi,Liu, Wei,et al. Stable isotopic and geochemical identification of groundwater evolution and recharge sources in the arid Shule River Basin of Northwestern China[J]. 中国科学院西北生态环境资源研究院,2015,29(22).
APA	Guo, Xiaoyan.,Feng, Qi.,Liu, Wei.,Li, Zongxing.,Wen, Xiaohu.,...&Jia, Bing.(2015).Stable isotopic and geochemical identification of groundwater evolution and recharge sources in the arid Shule River Basin of Northwestern China.HYDROLOGICAL PROCESSES,29(22).
MLA	Guo, Xiaoyan,et al."Stable isotopic and geochemical identification of groundwater evolution and recharge sources in the arid Shule River Basin of Northwestern China".HYDROLOGICAL PROCESSES 29.22(2015).