Articles | Volume 24, issue 6
https://doi.org/10.5194/hess-24-3271-2020
© Author(s) 2020. 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-24-3271-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Field observations of soil hydrological flow path evolution over 10 millennia
Anne Hartmann
CORRESPONDING AUTHOR
Section Hydrology, GFZ German Research Centre for Geosciences, Potsdam, Germany
Ekaterina Semenova
Chair of Hydrology, University of Freiburg, Freiburg, Germany
Markus Weiler
Chair of Hydrology, University of Freiburg, Freiburg, Germany
Theresa Blume
Section Hydrology, GFZ German Research Centre for Geosciences, Potsdam, Germany
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- Modeling wildfire effects on streamflow in the Cascade Mountains, Oregon, USA K. Wampler et al. 10.1016/j.jhydrol.2023.129585
- Subsurface flow paths in a chronosequence of calcareous soils: impact of soil age and rainfall intensities on preferential flow occurrence A. Hartmann et al. 10.5194/hess-26-4953-2022
- Assessment of plot-scale sediment transport on young moraines in the Swiss Alps using a fluorescent sand tracer F. Maier et al. 10.5194/hess-27-4609-2023
- Brief communication: Mountain permafrost acts as an aquitard during an infiltration experiment monitored with electrical resistivity tomography time-lapse measurements M. Pavoni et al. 10.5194/tc-17-1601-2023
- The impact of landscape evolution on soil physics: evolution of soil physical and hydraulic properties along two chronosequences of proglacial moraines A. Hartmann et al. 10.5194/essd-12-3189-2020
- Preferential flow patterns in forested hillslopes of east Tibetan Plateau revealed by dye tracing and soil moisture network F. Wang et al. 10.1111/ejss.13294
- The Evolution of Hillslope Hydrology: Links Between Form, Function and the Underlying Control of Geology A. Hartmann & T. Blume 10.1029/2023WR035937
- A new flow path: eDNA connecting hydrology and biology D. URycki et al. 10.1002/wat2.1749
- Preface: Linking landscape organisation and hydrological functioning: from hypotheses and observations to concepts, models and understanding C. Jackisch et al. 10.5194/hess-25-5277-2021
- Deposition and in-situ translocation of microplastics in floodplain soils C. Weber et al. 10.1016/j.scitotenv.2021.152039
- Soil Formation and Mass Redistribution during the Holocene Using Meteoric 10Be, Soil Chemistry and Mineralogy A. Musso et al. 10.3390/geosciences12020099
- Vertical root distribution and biomass allocation along proglacial chronosequences in Central Switzerland K. Greinwald et al. 10.1080/15230430.2020.1859720
- Long‐Term Changes in Runoff Generation Mechanisms for Two Proglacial Areas in the Swiss Alps I: Overland Flow F. Maier & I. van Meerveld 10.1029/2021WR030221
- Long‐Term Changes in Runoff Generation Mechanisms for Two Proglacial Areas in the Swiss Alps II: Subsurface Flow F. Maier et al. 10.1029/2021WR030223
- The development of nutrient pools along two holocene chronosequences with contrasting bedrocks in the Swiss Alps K. Greinwald et al. 10.1016/j.catena.2023.107507
14 citations as recorded by crossref.
- Towards a hydrogeomorphological understanding of proglacial catchments: an assessment of groundwater storage and release in an Alpine catchment T. Müller et al. 10.5194/hess-26-6029-2022
- Soil structure and solute transport pathways in biogas digestate-amended soils S. Koch et al. 10.1016/j.still.2024.106074
- Modeling wildfire effects on streamflow in the Cascade Mountains, Oregon, USA K. Wampler et al. 10.1016/j.jhydrol.2023.129585
- Subsurface flow paths in a chronosequence of calcareous soils: impact of soil age and rainfall intensities on preferential flow occurrence A. Hartmann et al. 10.5194/hess-26-4953-2022
- Assessment of plot-scale sediment transport on young moraines in the Swiss Alps using a fluorescent sand tracer F. Maier et al. 10.5194/hess-27-4609-2023
- Brief communication: Mountain permafrost acts as an aquitard during an infiltration experiment monitored with electrical resistivity tomography time-lapse measurements M. Pavoni et al. 10.5194/tc-17-1601-2023
- The impact of landscape evolution on soil physics: evolution of soil physical and hydraulic properties along two chronosequences of proglacial moraines A. Hartmann et al. 10.5194/essd-12-3189-2020
- Preferential flow patterns in forested hillslopes of east Tibetan Plateau revealed by dye tracing and soil moisture network F. Wang et al. 10.1111/ejss.13294
- The Evolution of Hillslope Hydrology: Links Between Form, Function and the Underlying Control of Geology A. Hartmann & T. Blume 10.1029/2023WR035937
- A new flow path: eDNA connecting hydrology and biology D. URycki et al. 10.1002/wat2.1749
- Preface: Linking landscape organisation and hydrological functioning: from hypotheses and observations to concepts, models and understanding C. Jackisch et al. 10.5194/hess-25-5277-2021
- Deposition and in-situ translocation of microplastics in floodplain soils C. Weber et al. 10.1016/j.scitotenv.2021.152039
- Soil Formation and Mass Redistribution during the Holocene Using Meteoric 10Be, Soil Chemistry and Mineralogy A. Musso et al. 10.3390/geosciences12020099
- Vertical root distribution and biomass allocation along proglacial chronosequences in Central Switzerland K. Greinwald et al. 10.1080/15230430.2020.1859720
3 citations as recorded by crossref.
- Long‐Term Changes in Runoff Generation Mechanisms for Two Proglacial Areas in the Swiss Alps I: Overland Flow F. Maier & I. van Meerveld 10.1029/2021WR030221
- Long‐Term Changes in Runoff Generation Mechanisms for Two Proglacial Areas in the Swiss Alps II: Subsurface Flow F. Maier et al. 10.1029/2021WR030223
- The development of nutrient pools along two holocene chronosequences with contrasting bedrocks in the Swiss Alps K. Greinwald et al. 10.1016/j.catena.2023.107507
Latest update: 16 Aug 2024
Short summary
Our field observation-based examination of flow path evolution, soil formation, and vegetation succession across 10 millennia shows how water flow paths and subsurface water storage are linked to the organization of evolving landscapes.
The increase found in water storage and preferential flow paths with increasing soil age shows the effect of the complex interaction of vegetation and soil development on flow paths, water balance, and runoff formation during landscape evolution.
Our field observation-based examination of flow path evolution, soil formation, and vegetation...