Articles | Volume 23, issue 6
https://doi.org/10.5194/hess-23-2751-2019
© Author(s) 2019. 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-23-2751-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
28 Jun 2019
Research article |
| 28 Jun 2019
Mechanisms of consistently disjunct soil water pools over (pore) space and time
Institute of Environmental Assessment and Water Research (IDAEA-CSIC), Calle Jordi Girona, 18–26, 08034 Barcelona, Spain
Department of Forestry and Environmental Resources, North Carolina
State University, 2720 Faucette Dr, Raleigh, NC 27606, USA
Pilar Llorens
Institute of Environmental Assessment and Water Research (IDAEA-CSIC), Calle Jordi Girona, 18–26, 08034 Barcelona, Spain
Carles Cayuela
Institute of Environmental Assessment and Water Research (IDAEA-CSIC), Calle Jordi Girona, 18–26, 08034 Barcelona, Spain
Francesc Gallart
Institute of Environmental Assessment and Water Research (IDAEA-CSIC), Calle Jordi Girona, 18–26, 08034 Barcelona, Spain
Jérôme Latron
Institute of Environmental Assessment and Water Research (IDAEA-CSIC), Calle Jordi Girona, 18–26, 08034 Barcelona, Spain
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- Hydrological functioning of thawing soil water in a permafrost‐influenced alpine meadow hillslope X. Xiao et al. 10.1002/vzj2.20022
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Latest update: 26 Mar 2023
Short summary
We find that the stable isotopic compositions of mobile and matrix bound soil water are continuously different over 8 months. Long-term data further show that these isotopic differences result from the refilling of small soil pores by isotopically depleted rains during low soil moisture conditions. Thus, subsurface water is not well mixed, but flow velocities and storage in soils are highly variable; this has important implications for ecohydrological studies and soil hydrological modeling.
We find that the stable isotopic compositions of mobile and matrix bound soil water are...
