Articles | Volume 20, issue 3
https://doi.org/10.5194/hess-20-1301-2016
© 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-20-1301-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
01 Apr 2016
Research article |
| 01 Apr 2016
Does drought alter hydrological functions in forest soils?
Katharina F. Gimbel
CORRESPONDING AUTHOR
Hydrology, Faculty of Environment and Natural Resources, University of Freiburg, Freiburg, Germany
Heike Puhlmann
Forest Research Institute Baden-Württemberg, Freiburg, Germany
Markus Weiler
Hydrology, Faculty of Environment and Natural Resources, University of Freiburg, Freiburg, Germany
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22 citations as recorded by crossref.
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- A review of preferential water flow in soil science Y. Zhang et al. 10.1139/cjss-2018-0046
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- Spatio-temporal relevance and controls of preferential flow at the landscape scale D. Demand et al. 10.5194/hess-23-4869-2019
- Understanding Preferential Flow in the Vadose Zone: Recent Advances and Future Prospects N. Jarvis et al. 10.2136/vzj2016.09.0075
- Field observations of soil hydrological flow path evolution over 10 millennia A. Hartmann et al. 10.5194/hess-24-3271-2020
- Estimating Freshwater Inflows for an Ungauged Watershed at the Big Boggy National Wildlife Refuge, USA J. Madewell et al. 10.3390/jmse12010015
- The impact of late medieval deforestation and 20th century forest decline on extreme flood magnitudes in the Ore Mountains (Southeastern Germany) C. Reinhardt-Imjela et al. 10.1016/j.quaint.2017.12.010
- Unimodal pattern of soil hydrophobicity along an altitudinal gradient encompassing Mediterranean, temperate, and alpine ecosystems G. Bonanomi et al. 10.1007/s11104-016-3020-0
- Forest cover lessens the impact of drought on streamflow in Puerto Rico J. Hall et al. 10.1002/hyp.14551
- Accelerated lagged compound floods and droughts in northwest North America under 1.5 °C − 4 °C global warming levels R. Rezvani et al. 10.1016/j.jhydrol.2023.129906
- Linking fire-induced evapotranspiration shifts to streamflow magnitude and timing in the western United States N. Collar et al. 10.1016/j.jhydrol.2022.128242
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- What We Know About Stemflow's Infiltration Area J. Van Stan & S. Allen 10.3389/ffgc.2020.00061
- Simulation and mapping of drought and soil erosion in Central Yunnan Province, China Y. Yu et al. 10.1016/j.asr.2021.08.028
- Spatial variation of grassland canopy affects soil wetting patterns and preferential flow G. Demir et al. 10.1002/hyp.14760
- Estimating karst groundwater recharge from soil moisture observations – a new method tested at the Swabian Alb, southwest Germany R. Berthelin et al. 10.5194/hess-27-385-2023
4 citations as recorded by crossref.
- Phosphorus fractions in preferential flow pathways and soil matrix in hillslope soils in the Thuringian Forest (Central Germany) D. Julich et al. 10.1002/jpln.201600305
- Influence of soil and climate on root zone storage capacity T. de Boer‐Euser et al. 10.1002/2015WR018115
- Differences in preferential flow with antecedent moisture conditions and soil texture: Implications for subsurface P transport K. Grant et al. 10.1002/hyp.13454
- Similar responses of soil carbon storage to drought and irrigation in terrestrial ecosystems but with contrasting mechanisms: A meta-analysis X. Zhou et al. 10.1016/j.agee.2016.04.030
Saved (preprint)
Latest update: 18 Apr 2024
Short summary
It is usually assumed that soil properties are not affected by drought events. We used dye tracer experiments to test this assumption on six forest soils, which were forced into drought conditions. The results of this study show clear evidence for changes in infiltration pathways. In addition, most soils developed soil water repellency. Overall, the results suggest that the past climatic conditions are more important than the actual soil moisture status regarding hydrophobicity and infiltration.
It is usually assumed that soil properties are not affected by drought events. We used dye...
