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: 7,557 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
4,454 2,860 243 7,557 475 182 246
  • HTML: 4,454
  • PDF: 2,860
  • XML: 243
  • Total: 7,557
  • Supplement: 475
  • BibTeX: 182
  • EndNote: 246
Views and downloads (calculated since 21 Feb 2017)
Cumulative views and downloads (calculated since 21 Feb 2017)

Viewed (geographical distribution)

Total article views: 7,557 (including HTML, PDF, and XML) Thereof 7,302 with geography defined and 255 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 27 Mar 2026
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.
Share