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

Viewed

Total article views: 3,423 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
2,120 1,180 123 3,423 77 129
  • HTML: 2,120
  • PDF: 1,180
  • XML: 123
  • Total: 3,423
  • BibTeX: 77
  • EndNote: 129
Views and downloads (calculated since 16 Feb 2017)
Cumulative views and downloads (calculated since 16 Feb 2017)

Viewed (geographical distribution)

Total article views: 3,423 (including HTML, PDF, and XML) Thereof 3,291 with geography defined and 132 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 14 Dec 2024
Download

The requested paper has a corresponding corrigendum published. Please read the corrigendum first before downloading the article.

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.