Articles | Volume 21, issue 7
https://doi.org/10.5194/hess-21-3839-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/hess-21-3839-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Soil water stable isotopes reveal evaporation dynamics at the soil–plant–atmosphere interface of the critical zone
Matthias Sprenger
CORRESPONDING AUTHOR
Northern Rivers Institute, School of Geosciences, University of
Aberdeen, Aberdeen, AB24 3UF, UK
Doerthe Tetzlaff
Northern Rivers Institute, School of Geosciences, University of
Aberdeen, Aberdeen, AB24 3UF, UK
Chris Soulsby
Northern Rivers Institute, School of Geosciences, University of
Aberdeen, Aberdeen, AB24 3UF, UK
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Discussed (final revised paper)
Latest update: 06 Dec 2024
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.
We sampled the isotopic composition in the top 20 cm at four different sites in the Scottish...