Hydrogeochemical and isotopic evidence of groundwater evolution and recharge in aquifers in Beijing Plain, China

Environmental Earth Sciences

Volumn 69, Issue 7, 2013, Pages 2167-2177

  Zhai, Yuanzheng ^a,b   Wang, Jinsheng ^a,b   Teng, Yanguo ^a,b   Zuo, Rui ^a,b  

^a BEIJING NORMAL UNIVERSITY   (China)

^b BEIJING UNIVERSITY OF POSTS AND TELECOMMUNICATIONS   (China)

Author keywords

Beijing; Groundwater age; Groundwater evolution; Groundwater recharge; Groundwater residence time

Indexed keywords

BEIJING; GROUND WATER RECHARGE; GROUNDWATER AGES; GROUNDWATER EXPLOITATION; GROUNDWATER RESIDENCE TIME; ISOTOPIC MEASUREMENT; QUATERNARY AQUIFERS; SHALLOW GROUNDWATER;

AQUIFERS; CALCIUM; FLOW OF FLUIDS; GROUNDWATER FLOW; GROUNDWATER RESOURCES; HYDROCHEMISTRY; HYDROGEOLOGY; ISOTOPES; RIVERS; SODIUM;

RECHARGING (UNDERGROUND WATERS);

CONFINED AQUIFER; EVAPORATION; FLOW FIELD; GROUNDWATER FLOW; HYDROGEOCHEMISTRY; ISOTOPIC ANALYSIS; PIEDMONT; QUATERNARY; RECHARGE; RESIDENCE TIME; TRITIUM;

BEIJING [CHINA]; CHINA;

EID: 84880510458     PISSN: 18666280     EISSN: 18666299     Source Type: Journal    
DOI: 10.1007/s12665-012-2045-9     Document Type: Article

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