Articles | Volume 22, issue 8
https://doi.org/10.5194/hess-22-4449-2018
https://doi.org/10.5194/hess-22-4449-2018
Comment/reply
 | 
22 Aug 2018
Comment/reply |  | 22 Aug 2018

Comment on “Origin of water in the Badain Jaran Desert, China: new insight from isotopes” by Wu et al. (2017)

Lucheng Zhan, Jiansheng Chen, Ling Li, and David A. Barry

Viewed

Total article views: 2,629 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,777 786 66 2,629 82 75
  • HTML: 1,777
  • PDF: 786
  • XML: 66
  • Total: 2,629
  • BibTeX: 82
  • EndNote: 75
Views and downloads (calculated since 08 May 2018)
Cumulative views and downloads (calculated since 08 May 2018)

Viewed (geographical distribution)

Total article views: 2,629 (including HTML, PDF, and XML) Thereof 2,532 with geography defined and 97 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 20 Nov 2024
Short summary
Using the arithmetic averages of precipitation isotope values, Wu et al. (2017) concluded that the Badain Jaran Desert (BJD) groundwater is recharged by modern local meteoric water. However, based on weighted mean precipitation isotope values, our further analysis shows that modern precipitation on the Qilian Mountains is more likely to be the main source of the groundwater and lake water in the BJD, as found. We believe this comment provides an important improvement for their study.