Articles | Volume 21, issue 10
Hydrol. Earth Syst. Sci., 21, 5181–5199, 2017
https://doi.org/10.5194/hess-21-5181-2017
Hydrol. Earth Syst. Sci., 21, 5181–5199, 2017
https://doi.org/10.5194/hess-21-5181-2017

Research article 17 Oct 2017

Research article | 17 Oct 2017

Impacts of a capillary barrier on infiltration and subsurface stormflow in layered slope deposits monitored with 3-D ERT and hydrometric measurements

Rico Hübner et al.

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Cited articles

Alfieri, L., Burek, P., Feyen, L., and Forzieri, G.: Global warming increases the frequency of river floods in Europe, Hydrol. Earth Syst. Sci., 19, 2247–2260, https://doi.org/10.5194/hess-19-2247-2015, 2015.
Ali, G., Tetzlaff, D., McDonnell, J. J., Soulsby, C., Carey, S., Laudon, H., McGuire, K., Buttle, J., Seibert, J., and Shanley, J.: Comparison of threshold hydrologic response across northern catchments, Hydrol. Proc., 29, 3575–3591, https://doi.org/10.1002/hyp.10527, 2015.
Anderson, M. G. and Burt, T. P. (Eds.): Process studies in hillslope hydrology, Wiley, Chichester, West Sussex, England, New York, 1990.
Bechtold, M., Vanderborght, J., Weihermueller, L., Herbst, M., Günther, T., Ippisch, O., Kasteel, R., and Vereecken, H.: Upward Transport in a Three-Dimensional Heterogeneous Laboratory Soil under Evaporation Conditions, Vadose Zone J., 11, https://doi.org/10.2136/vzj2011.0066, 2012.
Beff, L., Günther, T., Vandoorne, B., Couvreur, V., and Javaux, M.: Three-dimensional monitoring of soil water content in a maize field using Electrical Resistivity Tomography, Hydrol. Earth Syst. Sci., 17, 595–609, https://doi.org/10.5194/hess-17-595-2013, 2013.
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Short summary
In our study, we used a spatially and temporally high resolved 3-D ERT in addition to matric potential measurements to monitor the infiltration and subsurface water flow on a hillslope with layered slope deposits. We derived some interesting findings about the capillary barrier effect as a main driving factor for the activation of different flow pathways. Thus, the maintenance or breakdown of a capillary barrier has a decisive influence on the precipitation runoff response of of the catchment.