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Movement of lateral hyporheic flow between stream and groundwater

文献类型：期刊论文

作者Zhang Yu1,2,3; Wang JianLi1,2,3; Yang PingHeng1,2,3,4; Xie ShiYou1,2,3
刊名SCIENCE CHINA-EARTH SCIENCES
出版日期2017-11-01
卷号60期号:11页码:2033-2040
关键词Hyporheic Zone Lateral Hyporheic Flow Permeability Coefficient Hydrogen And Oxygen Isotopes Ma'an Creek
ISSN号1674-7313
DOI10.1007/s11430-016-9103-9
文献子类Article
英文摘要The hyporheic zone plays an important role in groundwater and stream water quality protection. To investigate the stream-groundwater interaction mechanisms in the lateral hyporheic zone, this study examined Ma'an Creek in Chongqing during the dry season from December 2015 to April 2016. The water level, water temperature, pH and Cl- concentration in the hyporheic zone and groundwater were monitored in situ. The sediment permeability coefficient, stable isotopes of hydrogen and oxygen and concentration of DOC were analyzed. The results show that the water level changes of hyporheic zone and the movement of hyporheic flow were influenced significantly by the permeability coefficient of sediment. The hyporheic flow approximately 10 cm from the stream bank was clearly affected by precipitation infiltration and evapotranspiration. During the study period, the groundwater recharged the stream, and the impact of groundwater on the hyporheic flow gradually decreased with the flow path. The hyporheic flow approximately 30 cm from the stream bank was still mainly affected by groundwater. Approximately 10-30 cm from the stream bank, the mixing of groundwater with precipitation and stream water intensified. Due to the sediment properties, moisture accumulated approximately 10 cm from the stream bank and drained into the stream via hyporheic flow, with potential impacts on stream water quality.
WOS关键词STABLE-ISOTOPES ; ZONE ; RIVER ; RECHARGE ; WATER ; EXCHANGE ; HYDROGEN ; REGION ; OXYGEN ; BED
WOS研究方向Geology
语种英语
WOS记录号WOS:000413691300009
出版者SCIENCE PRESS
资助机构National Key Technology R&D Program of China(2011BAC09B01) ; Fundamental Research Funds for the Central Universities(XDJK2014A016 ; Scientific and Technical Innovative Program of graduate students in Chongqing(CYS16050) ; XDJK2016D046) ; National Key Technology R&D Program of China(2011BAC09B01) ; Fundamental Research Funds for the Central Universities(XDJK2014A016 ; Scientific and Technical Innovative Program of graduate students in Chongqing(CYS16050) ; XDJK2016D046) ; National Key Technology R&D Program of China(2011BAC09B01) ; Fundamental Research Funds for the Central Universities(XDJK2014A016 ; Scientific and Technical Innovative Program of graduate students in Chongqing(CYS16050) ; XDJK2016D046) ; National Key Technology R&D Program of China(2011BAC09B01) ; Fundamental Research Funds for the Central Universities(XDJK2014A016 ; Scientific and Technical Innovative Program of graduate students in Chongqing(CYS16050) ; XDJK2016D046)
源URL[http://ir.iggcas.ac.cn/handle/132A11/62455]  
专题地质与地球物理研究所_中国科学院页岩气与地质工程重点实验室
通讯作者Yang PingHeng
作者单位1.Southwest Univ, Sch Geog Sci, Chongqing Key Lab Karst Environm, Key Lab Ecoenvironm Three Gorges Reservoir,Minst, Chongqing 400715, Peoples R China
2.Minist Land & Resources, Field Sci Observat, Chongqing 408435, Peoples R China
3.Minist Land & Resources, Res Base Karst Ecoenvironm Nanchuan Chongqing, Chongqing 408435, Peoples R China
4.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Shale Gas & Geoengn, Beijing 100029, Peoples R China
推荐引用方式
GB/T 7714		 Zhang Yu,Wang JianLi,Yang PingHeng,et al. Movement of lateral hyporheic flow between stream and groundwater[J]. SCIENCE CHINA-EARTH SCIENCES,2017,60(11):2033-2040.
APA Zhang Yu,Wang JianLi,Yang PingHeng,&Xie ShiYou.(2017).Movement of lateral hyporheic flow between stream and groundwater.SCIENCE CHINA-EARTH SCIENCES,60(11),2033-2040.
MLA Zhang Yu,et al."Movement of lateral hyporheic flow between stream and groundwater".SCIENCE CHINA-EARTH SCIENCES 60.11(2017):2033-2040.

入库方式： OAI收割

来源：地质与地球物理研究所

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