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Isotopic and geochemical evidence of recharge sources and water quality in the Quaternary aquifer beneath Jinchang city, NW China

文献类型：期刊论文

作者Ma, Jinzhu1; Pan, Feng1; Chen, Lihua1,2; Edmunds, W. Mike3; Ding, Zhenyu1; He, Jianhua1; Zhou, Kunpeng1; Huang, Tianming1,4
刊名APPLIED GEOCHEMISTRY
出版日期2010-07-01
卷号25期号:7页码:996-1007
ISSN号0883-2927
DOI10.1016/j.apgeochem.2010.04.006
文献子类Article
英文摘要Multiple isotopic and hydrogeochemical tracers were utilized to understand the recharge sources and geochemical evolution of groundwater in the Quaternary aquifer beneath Jinchang city and the adjacent Gobi desert area. The groundwater shows markedly depleted stable isotopic composition compared to modern rainfall. The signature of groundwaters from Jinchang and the northern Gobi desert area differ clearly from that of the alluvial fan in the south Yongchang basin and modern rainfall, and has lower or non-detectable (3)H activity, implying that the aquifer is likely maintained by palaeowater. This groundwater in the Gobi desert has a (14)C age older than 12 ka, indicating that the groundwater resources are non-renewable. The build-up of dissolved solids through evaporation is a major control on groundwater composition, and the dominant anion species change systematically from HCO(3)(-), SO(4)(2-) to Cl(-), but cations from weathering of albite, calcite, dolomite and gypsum also make a significant contribution. The scientific results have important implications for groundwater management in Jinchang city and as well as in the Shiyang River basin under China's West Development Strategy. It is recommended that the water allocation program of diverting water from the Dongda river to the Minqin basin be reconsidered. (C) 2010 Elsevier Ltd. All rights reserved.
WOS关键词HEIHE RIVER-BASIN ; GROUNDWATER RECHARGE ; NORTHWEST CHINA ; CLIMATE-CHANGE ; GOBI DESERT ; EVOLUTION ; RESOURCES ; MANAGEMENT ; IMPACTS ; REGIONS
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000279093900007
出版者PERGAMON-ELSEVIER SCIENCE LTD
资助机构National Science Foundation of China(40872161 ; National Science Foundation of China(40872161 ; Royal Society(2007/R3) ; Royal Society(2007/R3) ; 111 project(B06026) ; 111 project(B06026) ; 40721061) ; 40721061) ; National Science Foundation of China(40872161 ; National Science Foundation of China(40872161 ; Royal Society(2007/R3) ; Royal Society(2007/R3) ; 111 project(B06026) ; 111 project(B06026) ; 40721061) ; 40721061) ; National Science Foundation of China(40872161 ; National Science Foundation of China(40872161 ; Royal Society(2007/R3) ; Royal Society(2007/R3) ; 111 project(B06026) ; 111 project(B06026) ; 40721061) ; 40721061) ; National Science Foundation of China(40872161 ; National Science Foundation of China(40872161 ; Royal Society(2007/R3) ; Royal Society(2007/R3) ; 111 project(B06026) ; 111 project(B06026) ; 40721061) ; 40721061)
源URL[http://ir.iggcas.ac.cn/handle/132A11/72268]  
专题中国科学院地质与地球物理研究所
通讯作者Ma, Jinzhu
作者单位1.Lanzhou Univ, Minist Educ, Key Lab Western Chinas Environm Syst, Lanzhou 730000, Peoples R China
2.NW Univ Nationalities, Coll Chem Engn, Lanzhou 730000, Peoples R China
3.Univ Oxford, Ctr Environm, Oxford Ctr Water Res, Oxford OX1 3QY, England
4.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
推荐引用方式
GB/T 7714		 Ma, Jinzhu,Pan, Feng,Chen, Lihua,et al. Isotopic and geochemical evidence of recharge sources and water quality in the Quaternary aquifer beneath Jinchang city, NW China[J]. APPLIED GEOCHEMISTRY,2010,25(7):996-1007.
APA Ma, Jinzhu.,Pan, Feng.,Chen, Lihua.,Edmunds, W. Mike.,Ding, Zhenyu.,...&Huang, Tianming.(2010).Isotopic and geochemical evidence of recharge sources and water quality in the Quaternary aquifer beneath Jinchang city, NW China.APPLIED GEOCHEMISTRY,25(7),996-1007.
MLA Ma, Jinzhu,et al."Isotopic and geochemical evidence of recharge sources and water quality in the Quaternary aquifer beneath Jinchang city, NW China".APPLIED GEOCHEMISTRY 25.7(2010):996-1007.

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来源：地质与地球物理研究所

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