Articles | Volume 25, issue 10
Hydrol. Earth Syst. Sci., 25, 5399–5413, 2021
https://doi.org/10.5194/hess-25-5399-2021
Hydrol. Earth Syst. Sci., 25, 5399–5413, 2021
https://doi.org/10.5194/hess-25-5399-2021
Technical note
07 Oct 2021
Technical note | 07 Oct 2021

Technical note: Evaporating water is different from bulk soil water in δ2H and δ18O and has implications for evaporation calculation

Hongxiu Wang et al.

Viewed

Total article views: 1,864 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,289 546 29 1,864 86 13 22
  • HTML: 1,289
  • PDF: 546
  • XML: 29
  • Total: 1,864
  • Supplement: 86
  • BibTeX: 13
  • EndNote: 22
Views and downloads (calculated since 26 Jan 2021)
Cumulative views and downloads (calculated since 26 Jan 2021)

Viewed (geographical distribution)

Total article views: 1,864 (including HTML, PDF, and XML) Thereof 1,706 with geography defined and 158 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 28 Jan 2023
Download
Short summary
Evaporation led to progressively more heavy-isotope-enriched bulk soil water (BW) following the precipitation/irrigation of heavy-isotope-depleted new water but causes progressively more heavy-isotope-depleted BW following irrigation of heavy-isotope-enriched new water. The results indicated that δ2H and δ18O in evaporating water (EW) were similar to new water and differed from BW. However, the evaporative water loss calculated from BW did not differ significantly from that of EW.