Changes of δ18O and δd along the Dousitu River, Inner Mongolia, China, and their evidence of river water evaporation

Aquatic Geochemistry

Volumn 13, Issue 2, 2007, Pages 127-142

  Hui, Qian ^a   Mengyao, Li ^a   Yadong, Ji ^a   Bingchao, Yang ^b   Zhenhong, Zhao ^b  

^a CHANG'AN UNIVERSITY   (China)

^b XI AN INSTITUTE OF GEOLOGY AND MINERAL RESOURCES   (China)

Author keywords

Changes in river water flow rate; Changes of isotope composition; Dousitu River; Evaporation fraction, China

Indexed keywords

DRAINAGE BASIN; EVAPORATION; FRACTIONATION; HYDROGEOLOGY; ISOTOPIC COMPOSITION; OXYGEN ISOTOPE; RECHARGE; RIVER DISCHARGE; RIVER WATER; WATER FLOW;

CHINA; DOUSITU RIVER; NEI MONGGOL;

EID: 72549105300     PISSN: 13806165     EISSN: 15731421     Source Type: Journal    
DOI: 10.1007/s10498-007-9011-2     Document Type: Article

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