Articles | Volume 20, issue 9
https://doi.org/10.5194/hess-20-3873-2016
© Author(s) 2016. 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-20-3873-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Exploring water cycle dynamics by sampling multiple stable water isotope pools in a developed landscape in Germany
Natalie Orlowski
CORRESPONDING AUTHOR
Institute for Landscape Ecology and Resources Management
(ILR), Research Centre for BioSystems, Land Use and Nutrition (iFZ), Justus
Liebig University Gießen, Gießen, Germany
Global Institute for Water Security, University of
Saskatchewan, Saskatoon, Canada
Philipp Kraft
Institute for Landscape Ecology and Resources Management
(ILR), Research Centre for BioSystems, Land Use and Nutrition (iFZ), Justus
Liebig University Gießen, Gießen, Germany
Jakob Pferdmenges
Institute for Landscape Ecology and Resources Management
(ILR), Research Centre for BioSystems, Land Use and Nutrition (iFZ), Justus
Liebig University Gießen, Gießen, Germany
Lutz Breuer
Institute for Landscape Ecology and Resources Management
(ILR), Research Centre for BioSystems, Land Use and Nutrition (iFZ), Justus
Liebig University Gießen, Gießen, Germany
Centre for International Development and Environmental
Research, Justus Liebig University Gießen, Gießen, Germany
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Latest update: 23 Nov 2024
Short summary
The 2-year measurements of δ2H and δ18O in rainfall, stream, soil, and groundwater revealed that surface and groundwater are isotopically disconnected from the annual precipitation cycle but showed bidirectional interactions in the Schwingbach catchment. We established a hydrological model to estimate spatially distributed groundwater ages and flow directions. Our model revealed complex age dynamics and showed that runoff must have been stored in the catchment for much longer than event water.
The 2-year measurements of δ2H and δ18O in rainfall, stream, soil, and groundwater revealed...