Articles | Volume 22, issue 5
https://doi.org/10.5194/hess-22-2881-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/hess-22-2881-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Effects of climatic seasonality on the isotopic composition of evaporating soil waters
Laboratory of Ecohydrology ENAC/IIE/ECHO, École Polytechinque Fédérale de Lausanne (EPFL), Lausanne, Switzerland
Till H. M. Volkmann
Biosphere 2, University of Arizona, Tucson, AZ, USA
Jana von Freyberg
Department of Environmental Systems Science, ETH Zurich, Zurich, Switzerland
Research Unit Mountain Hydrology and Mass Movements, Swiss Federal Institute for Forest, Snow and Landscape Research (WSL), Birmensdorf, Switzerland
Jay Frentress
Faculty of Science and Technology, Free University of Bolzano, Bolzano, Italy
Daniele Penna
Department of Agricultural, Food and Forestry Systems, University of Florence, Florence, Italy
Todd E. Dawson
Department of Integrative Biology, University of California, Berkeley, CA, USA
James W. Kirchner
Department of Environmental Systems Science, ETH Zurich, Zurich, Switzerland
Research Unit Mountain Hydrology and Mass Movements, Swiss Federal Institute for Forest, Snow and Landscape Research (WSL), Birmensdorf, Switzerland
Department of Earth and Planetary Science, University of California, Berkeley, CA, USA
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- Tracing sources of stormflow and groundwater recharge in an urban, semi-arid watershed using stable isotopes S. Wallace et al. 10.1016/j.ejrh.2021.100806
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Latest update: 20 Nov 2024
Short summary
Evaporation causes the isotopic composition of soil water to become different from that of the original precipitation source. If multiple samples originating from the same source are available, they can be used to reconstruct the original source composition. However, soil water is influenced by seasonal variability in both precipitation sources and evaporation patterns. We show that this variability, if not accounted for, can lead to biased estimates of the precipitation source water.
Evaporation causes the isotopic composition of soil water to become different from that of the...