Arid
DOI10.1016/j.jhydrol.2019.06.037
Isotopic and geochemical interpretation of groundwater under the influences of anthropogenic activities
Li, Zijun1,2; Yang, Qingchun1,2; Yang, Yuesuo3; Ma, Honhyun4; Wang, Hui5; Luo, Jiannan1,2; Bian, Jianmin1,2; Delgado Martin, Jordi6
通讯作者Yang, Qingchun
来源期刊JOURNAL OF HYDROLOGY
ISSN0022-1694
EISSN1879-2707
出版年2019
卷号576页码:685-697
英文摘要Groundwater resources are increasingly exploited for industrial and agricultural purposes in many arid/semiarid regions globally. In order to gain a harmonious development among groundwater resources and economic benefits, urgent investigation of the impacts of anthropogenic activities on the groundwater chemistry is required. Understanding hydrochemical mechanism of groundwater in Yinchuan Plain, arid and semi-arid area in Northwestern China, plays a significant role in water resources planning in this ecologically sensitive area. In this paper, a total of 460 phreatic water samples were collected, including 58 water samples containing isotopic data (D and H-2). Results demonstrate that water chemistry type and isotopic data of phreatic water presents a zonation characteristic from west to east and from south to north. In the eastern part of the Helan Mountain (A(1) zone), the type of hydrochemistry is mainly HCO3 center dot SO4-CaMg, SO4 center dot HCO3-Ca center dot Mg, which is mainly recharged by the bedrock fissure water of Helan Mountain. However, in the southern Qingtongxia (A(2) zone) are HCO3-Na HCO3-Ca center dot Mg, which receives irrigation and spring water recharge. Phreatic aquifer in Multi-layered structure zone (A(3) zone) reflect multiple recharge sources to the aquifer, the water chemistry demonstrates diverse variations. The anion was dominated by the HCO3, while the cation is dominated by sodium. The predominant controlling factors of phreatic water hydrochemistry are divided into anthropogenic activities and natural conditions. Natural conditions mainly include the existence form and lithology of the aquifer, sources of groundwater recharge, soil salinity, and evaporation, mineral dissolution, ion exchange and adsorption and mixing effect. Meanwhile, among natural factors, minerals dissolution in groundwater is the main process dominating the hydrochemical evolution of the groundwater. The other is anthropogenic activities which can be classified as groundwater pollution, excessive exploitation or excretion of groundwater, and excessive groundwater recharge.
英文关键词Hydrochemical mechanism Anthropogenic activities Hydrochemistry Isotope Groundwater
类型Article
语种英语
国家Peoples R China ; Spain
收录类别SCI-E
WOS记录号WOS:000486092200054
WOS关键词HYDROCHEMICAL CHARACTERISTICS ; CONTAMINATION ; REGION ; BASIN ; RIVER
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/2XILL650/217175
作者单位1.Jilin Univ, Key Lab Groundwater Resources & Environm, Minist Educ, Changchun 130021, Jilin, Peoples R China;
2.Jilin Univ, Coll New Energy & Environm, Changchun 130021, Jilin, Peoples R China;
3.Shenyang Univ, Key Lab Ecorestorat Reg Contaminated Environm, Minist Educ, Shenyang 110044, Liaoning, Peoples R China;
4.CGS, Key Lab Groundwater & Ecol Arid & Semiarid Areas, Xian Ctr Geol Survey, Xian 710054, Shaanxi, Peoples R China;
5.Reg Survey Geol & Resources Jilin Prov, Changchun 130021, Jilin, Peoples R China;
6.Univ A Coruna, Escuela Ingenieros Caminos, Campus Elvina, La Coruna 15192, Spain
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GB/T 7714
Li, Zijun,Yang, Qingchun,Yang, Yuesuo,et al. Isotopic and geochemical interpretation of groundwater under the influences of anthropogenic activities[J],2019,576:685-697.
APA Li, Zijun.,Yang, Qingchun.,Yang, Yuesuo.,Ma, Honhyun.,Wang, Hui.,...&Delgado Martin, Jordi.(2019).Isotopic and geochemical interpretation of groundwater under the influences of anthropogenic activities.JOURNAL OF HYDROLOGY,576,685-697.
MLA Li, Zijun,et al."Isotopic and geochemical interpretation of groundwater under the influences of anthropogenic activities".JOURNAL OF HYDROLOGY 576(2019):685-697.
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