Articles | Volume 18, issue 9
https://doi.org/10.5194/hess-18-3681-2014
© Author(s) 2014. 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-18-3681-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
24 Sep 2014
Research article |
| 24 Sep 2014
Hillslope-scale experiment demonstrates the role of convergence during two-step saturation
A. I. Gevaert
Hydrology and Quantitative Water Management Group, Wageningen University, Wageningen, the Netherlands
Biosphere 2 – College of Science, University of Arizona, Tucson, Arizona, USA
now at: Department of Earth Sciences, VU University, Amsterdam, the Netherlands
A. J. Teuling
Hydrology and Quantitative Water Management Group, Wageningen University, Wageningen, the Netherlands
R. Uijlenhoet
Hydrology and Quantitative Water Management Group, Wageningen University, Wageningen, the Netherlands
S. B. DeLong
Biosphere 2 – College of Science, University of Arizona, Tucson, Arizona, USA
now at: US Geological Survey, Menlo Park, California, USA
T. E. Huxman
Biosphere 2 – College of Science, University of Arizona, Tucson, Arizona, USA
Department of Ecology and Evolutionary Biology, University of California, Irvine, California, USA
L. A. Pangle
Biosphere 2 – College of Science, University of Arizona, Tucson, Arizona, USA
D. D. Breshears
Biosphere 2 – College of Science, University of Arizona, Tucson, Arizona, USA
School of Natural Resources and the Environment, University of Arizona, Tucson, Arizona, USA
J. Chorover
Biosphere 2 – College of Science, University of Arizona, Tucson, Arizona, USA
Department of Soil, Water and Environmental Science, University of Arizona, Tucson, Arizona, USA
J. D. Pelletier
Biosphere 2 – College of Science, University of Arizona, Tucson, Arizona, USA
Department of Geosciences, University of Arizona, Tucson, Arizona, USA
S. R. Saleska
Biosphere 2 – College of Science, University of Arizona, Tucson, Arizona, USA
Department of Ecology and Evolutionary Biology, University of Arizona, Tucson, Arizona, USA
Biosphere 2 – College of Science, University of Arizona, Tucson, Arizona, USA
Department of Atmospheric Sciences, University of Arizona, Tucson, Arizona, USA
P. A. Troch
Biosphere 2 – College of Science, University of Arizona, Tucson, Arizona, USA
Department of Hydrology and Water Resources, University of Arizona, Tucson, Arizona, USA
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Cited
31 citations as recorded by crossref.
- Richards Equation at the Hillslope Scale: Can We Resolve the Heterogeneity of Soil Hydraulic Material Properties? H. Bauser et al. 10.1029/2022WR032294
- Testing the hybrid‐3‐D hillslope hydrological model in a controlled environment P. Hazenberg et al. 10.1002/2015WR018106
- Observing Heterogeneous Unsaturated Flow at the Hillslope Scale Using Time‐Lapse Electrical Resistivity Tomography M. Kotikian et al. 10.2136/vzj2018.07.0138
- The Influence of Local and Nonlocal Factors on Soil Water Content in a Steep Forested Catchment K. Jarecke et al. 10.1029/2020WR028343
- Characterization of subsurface fluxes at the plot scale during flash floods in the Valescure catchment, France C. Bouvier et al. 10.1002/hyp.14144
- The behavior of wetting front on slopes with different slope morphologies during rainfall C. Fan & H. Wang 10.1016/j.jher.2019.07.005
- CO2 diffusion into pore spaces limits weathering rate of an experimental basalt landscape J. van Haren et al. 10.1130/G38569.1
- Whither field hydrology? The need for discovery science and outrageous hydrological hypotheses T. Burt & J. McDonnell 10.1002/2014WR016839
- Disentangling the factors that vary the impact of trees on flooding (a review) T. Marapara et al. 10.1111/wej.12647
- Effects of soil heterogeneity and preferential flow on the water flow and isotope transport in an experimental hillslope X. Chen et al. 10.1016/j.scitotenv.2024.170548
- Particle tracer transport in a sloping soil lysimeter under periodic, steady state conditions C. Wang et al. 10.1016/j.jhydrol.2018.11.050
- A novel physical model demonstrating critical zone structure and flow processes in headwaters for teaching and research purposes X. Shen et al. 10.1002/hyp.14259
- Peripheral gully and landslide erosion on an extreme anthropogenic landscape produced by mountaintop removal coal mining M. Reed & S. Kite 10.1002/esp.4867
- Forest catchment structure mediates shallow subsurface flow and soil base cation fluxes A. Pennino et al. 10.1016/j.geoderma.2024.117045
- Cape Fear: monitoring basic hydrological processes in an outdoor hillslope plot A. Petroselli & F. Tauro 10.1007/s10661-017-5851-4
- Water availability and hydrological connectivity mediate the responses of alpine soil prokaryotes to temperature changes at the watershed scale W. Lv et al. 10.1016/j.jenvman.2025.126299
- Pore water chemistry reveals gradients in mineral transformation across a model basaltic hillslope M. Pohlmann et al. 10.1002/2016GC006270
- Potential of time‐lapse photography for identifying saturation area dynamics on agricultural hillslopes R. Silasari et al. 10.1002/hyp.11272
- Impact of extreme rainfall events on soil erosion on karst Slopes: A study of hydrodynamic mechanisms Y. Yan et al. 10.1016/j.jhydrol.2024.131532
- A Modified Distributed CN-VSA Method for Mapping of the Seasonally Variable Source Areas K. Panjabi et al. 10.3390/w13091270
- Variable storage behavior controlled by rainfall intensity and profile structure upon saturation excess overland flow generation J. Zhang et al. 10.1016/j.jhydrol.2022.127860
- Challenges with effective representations of heterogeneity in soil hydrology based on local water content measurements H. Bauser et al. 10.1002/vzj2.20040
- Examination of the seepage face boundary condition in subsurface and coupled surface/subsurface hydrological models C. Scudeler et al. 10.1002/2016WR019277
- Transit time distributions and StorAge Selection functions in a sloping soil lysimeter with time‐varying flow paths: Direct observation of internal and external transport variability M. Kim et al. 10.1002/2016WR018620
- Direct Observation of Hillslope Scale StorAge Selection Functions in Experimental Hydrologic Systems: Geomorphologic Structure and Preferential Discharge of Old Water M. Kim et al. 10.1029/2020WR028959
- Microtopography mediates the community assembly of soil prokaryotes on the local-site scale W. Lv et al. 10.1016/j.catena.2022.106815
- Impact of sensor failure on the observability of flow dynamics at the Biosphere 2 LEO hillslopes D. Pasetto et al. 10.1016/j.advwatres.2015.04.014
- Multiresponse modeling of variably saturated flow and isotope tracer transport for a hillslope experiment at the Landscape Evolution Observatory C. Scudeler et al. 10.5194/hess-20-4061-2016
- The Landscape Evolution Observatory: A large-scale controllable infrastructure to study coupled Earth-surface processes L. Pangle et al. 10.1016/j.geomorph.2015.01.020
- Developing observational methods to drive future hydrological science: Can we make a start as a community? K. Beven et al. 10.1002/hyp.13622
- Incipient subsurface heterogeneity and its effect on overland flow generation – insight from a modeling study of the first experiment at the Biosphere 2 Landscape Evolution Observatory G. Niu et al. 10.5194/hess-18-1873-2014
29 citations as recorded by crossref.
- Richards Equation at the Hillslope Scale: Can We Resolve the Heterogeneity of Soil Hydraulic Material Properties? H. Bauser et al. 10.1029/2022WR032294
- Testing the hybrid‐3‐D hillslope hydrological model in a controlled environment P. Hazenberg et al. 10.1002/2015WR018106
- Observing Heterogeneous Unsaturated Flow at the Hillslope Scale Using Time‐Lapse Electrical Resistivity Tomography M. Kotikian et al. 10.2136/vzj2018.07.0138
- The Influence of Local and Nonlocal Factors on Soil Water Content in a Steep Forested Catchment K. Jarecke et al. 10.1029/2020WR028343
- Characterization of subsurface fluxes at the plot scale during flash floods in the Valescure catchment, France C. Bouvier et al. 10.1002/hyp.14144
- The behavior of wetting front on slopes with different slope morphologies during rainfall C. Fan & H. Wang 10.1016/j.jher.2019.07.005
- CO2 diffusion into pore spaces limits weathering rate of an experimental basalt landscape J. van Haren et al. 10.1130/G38569.1
- Whither field hydrology? The need for discovery science and outrageous hydrological hypotheses T. Burt & J. McDonnell 10.1002/2014WR016839
- Disentangling the factors that vary the impact of trees on flooding (a review) T. Marapara et al. 10.1111/wej.12647
- Effects of soil heterogeneity and preferential flow on the water flow and isotope transport in an experimental hillslope X. Chen et al. 10.1016/j.scitotenv.2024.170548
- Particle tracer transport in a sloping soil lysimeter under periodic, steady state conditions C. Wang et al. 10.1016/j.jhydrol.2018.11.050
- A novel physical model demonstrating critical zone structure and flow processes in headwaters for teaching and research purposes X. Shen et al. 10.1002/hyp.14259
- Peripheral gully and landslide erosion on an extreme anthropogenic landscape produced by mountaintop removal coal mining M. Reed & S. Kite 10.1002/esp.4867
- Forest catchment structure mediates shallow subsurface flow and soil base cation fluxes A. Pennino et al. 10.1016/j.geoderma.2024.117045
- Cape Fear: monitoring basic hydrological processes in an outdoor hillslope plot A. Petroselli & F. Tauro 10.1007/s10661-017-5851-4
- Water availability and hydrological connectivity mediate the responses of alpine soil prokaryotes to temperature changes at the watershed scale W. Lv et al. 10.1016/j.jenvman.2025.126299
- Pore water chemistry reveals gradients in mineral transformation across a model basaltic hillslope M. Pohlmann et al. 10.1002/2016GC006270
- Potential of time‐lapse photography for identifying saturation area dynamics on agricultural hillslopes R. Silasari et al. 10.1002/hyp.11272
- Impact of extreme rainfall events on soil erosion on karst Slopes: A study of hydrodynamic mechanisms Y. Yan et al. 10.1016/j.jhydrol.2024.131532
- A Modified Distributed CN-VSA Method for Mapping of the Seasonally Variable Source Areas K. Panjabi et al. 10.3390/w13091270
- Variable storage behavior controlled by rainfall intensity and profile structure upon saturation excess overland flow generation J. Zhang et al. 10.1016/j.jhydrol.2022.127860
- Challenges with effective representations of heterogeneity in soil hydrology based on local water content measurements H. Bauser et al. 10.1002/vzj2.20040
- Examination of the seepage face boundary condition in subsurface and coupled surface/subsurface hydrological models C. Scudeler et al. 10.1002/2016WR019277
- Transit time distributions and StorAge Selection functions in a sloping soil lysimeter with time‐varying flow paths: Direct observation of internal and external transport variability M. Kim et al. 10.1002/2016WR018620
- Direct Observation of Hillslope Scale StorAge Selection Functions in Experimental Hydrologic Systems: Geomorphologic Structure and Preferential Discharge of Old Water M. Kim et al. 10.1029/2020WR028959
- Microtopography mediates the community assembly of soil prokaryotes on the local-site scale W. Lv et al. 10.1016/j.catena.2022.106815
- Impact of sensor failure on the observability of flow dynamics at the Biosphere 2 LEO hillslopes D. Pasetto et al. 10.1016/j.advwatres.2015.04.014
- Multiresponse modeling of variably saturated flow and isotope tracer transport for a hillslope experiment at the Landscape Evolution Observatory C. Scudeler et al. 10.5194/hess-20-4061-2016
- The Landscape Evolution Observatory: A large-scale controllable infrastructure to study coupled Earth-surface processes L. Pangle et al. 10.1016/j.geomorph.2015.01.020
2 citations as recorded by crossref.
- Developing observational methods to drive future hydrological science: Can we make a start as a community? K. Beven et al. 10.1002/hyp.13622
- Incipient subsurface heterogeneity and its effect on overland flow generation – insight from a modeling study of the first experiment at the Biosphere 2 Landscape Evolution Observatory G. Niu et al. 10.5194/hess-18-1873-2014
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