Articles | Volume 21, issue 9
https://doi.org/10.5194/hess-21-4419-2017
https://doi.org/10.5194/hess-21-4419-2017
Research article
 | 
07 Sep 2017
Research article |  | 07 Sep 2017

Origin of water in the Badain Jaran Desert, China: new insight from isotopes

Xiujie Wu, Xu-Sheng Wang, Yang Wang, and Bill X. Hu

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AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (further review by Editor and Referees) (12 Jun 2017) by Christine Stumpp
AR by xiujie wu on behalf of the Authors (20 Jun 2017)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (23 Jun 2017) by Christine Stumpp
RR by Anonymous Referee #2 (17 Jul 2017)
ED: Publish as is (01 Aug 2017) by Christine Stumpp
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Short summary
It is critical to identify the origins of water in arid and semiarid regions for management and protection of the water resources. The D, 18O, 3H and 14C in water samples from the Badain Jaran Desert, China, were analyzed. The results show that groundwater supplies the lakes and originates from local precipitation and adjacent mountains. Negative d-excess values of water in the area were the result of evaporation. The 14C ages do not represent the residence time of local groundwater.