Articles | Volume 21, issue 7
https://doi.org/10.5194/hess-21-3839-2017
https://doi.org/10.5194/hess-21-3839-2017
Research article
 | 
27 Jul 2017
Research article |  | 27 Jul 2017

Soil water stable isotopes reveal evaporation dynamics at the soil–plant–atmosphere interface of the critical zone

Matthias Sprenger, Doerthe Tetzlaff, and Chris Soulsby

Viewed

Total article views: 5,841 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
3,455 2,205 181 5,841 398 108 142
  • HTML: 3,455
  • PDF: 2,205
  • XML: 181
  • Total: 5,841
  • Supplement: 398
  • BibTeX: 108
  • EndNote: 142
Views and downloads (calculated since 21 Feb 2017)
Cumulative views and downloads (calculated since 21 Feb 2017)

Viewed (geographical distribution)

Total article views: 5,841 (including HTML, PDF, and XML) Thereof 5,602 with geography defined and 239 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Discussed (final revised paper)

Latest update: 06 Dec 2024
Download
Short summary
We sampled the isotopic composition in the top 20 cm at four different sites in the Scottish Highlands at 5 cm intervals over 1 year. The relationship between the soil water isotopic fractionation and evapotranspiration showed a hysteresis pattern due to a lag response to onset and offset of the evaporative losses. The isotope data revealed that vegetation had a significant influence on the soil evaporation with evaporation being double from soils beneath Scots pine compared to heather.