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Featured researches published by Marcus Schindewolf.


Zeitschrift Fur Geomorphologie | 2013

Comparative measurements with seven rainfall simulators on uniform bare fallow land

Thomas Iserloh; Johannes B. Ries; Artemi Cerdà; M.T. Echeverría; Wolfgang Fister; Christian Geißler; Nikolaus J. Kuhn; F.J. León; Piet Peters; Marcus Schindewolf; Jürgen Schmidt; Thomas Scholten; Manuel Seeger

To assess the inflfl uence of rainfall simulator type and plot dimensions on runoff and erosion, seven small portable rainfall simulators from Freiberg, Tubingen, Trier (all Germany), Valencia, Zaragoza (both Spain), Basel (Switzerland) and Wageningen (the Netherlands) were compared on a prepared bare fallow fifi eld. The experiments were carried out during an international rainfall simulator workshop, organized at Trier University (Germany) from 30th of June to 1st of July 2011.The tested rainfall simulators differ in design, rainfall intensities, rain spectra, etc. and represent most of the devices which have been used over the last decade in Europe. The plots for the different rainfall simulators were selected as similar as possible concerning soil physical and chemical properties, aspect and inclination and were chosen to be placed side by side in horizontal direction. Test procedure was standardized in order to examine the inflfl uence of the rainfall simulator andplot dimension only. The results show a clear and consistent relationship in runoff, erosion and infifi ltration behaviour of the different used rainfall simulators. With all the devices total soil loss is measurable, but different plot sizes, intensities and kinetic energies of the simulated rainfall caused differences in soil loss and runoff quantities per unit of area. Regarding course characteristics over runs, similarities could be observed especially in runoff behaviour. The rainfall simulators (> 1 m² plot size) are able to reproduce infifi ltration and interrillerosion processes. With an increase of plot size (≥ 1 m²), rill-erosion will be also reflfl ected. Therefore it can be concluded that up to a certain plot size, the results of the different simulators are comparable and depend in their magnitude on the properties of the applied rainfall. The increase in process complexity with increasing plot size shows, that the scale of the simulation is one of the most important parameters to be taken intoaccount when comparing values of erosion and runoff.


Archive | 2015

Simulation of Reservoir Siltation with a Process-based Soil Loss and Deposition Model

Marcus Schindewolf; Constanze Bornkampf; Michael von Werner; Jürgen Schmidt

Soil erosion on arable land is the key driver of reservoir siltation in the German lo‐ ess belt. In this regard, the Baderitz Reservoir suffers from deleterious sediment in‐ puts and resulting siltation processes. In order to estimate the reservoir lifespan, the event-based soil erosion and deposition model EROSION 3D was applied. Simula‐ tions of sediment input and sediment deposition processes within the reservoir were realized using a typical crop rotation and a normal heavy rainfall year of the region. Model parameterization was enabled by existing data based on a large num‐ ber of artificial rainfall simulations. Yearly soil losses of approximately 12 t/ha cor‐ respond to sediment inputs of nearly 8800 t. The mean annual increase of the reservoir bottom of 9 cm causes a 13% loss of reservoir storage in only 10 years. The model results are plausible and could be used for planning and dimensioning of mitigation measures.


Catena | 2012

Parameterization of the EROSION 2D/3D soil erosion model using a small-scale rainfall simulator and upstream runoff simulation

Marcus Schindewolf; Jürgen Schmidt


Hydrology | 2016

Feasibility of High-Resolution Soil Erosion Measurements by Means of Rainfall Simulations and SfM Photogrammetry

Phoebe Hänsel; Marcus Schindewolf; Anette Eltner; Andreas Kaiser; Jürgen Schmidt


SOIL | 2015

Determination of hydrological roughness by means of close range remote sensing

Andreas Kaiser; Fabian Neugirg; Florian Haas; Jürgen Schmidt; Michael Becht; Marcus Schindewolf


Catena | 2017

Wind effects on soil erosion by water — A sensitivity analysis using model simulations on catchment scale

Jürgen Schmidt; Michael von Werner; Marcus Schindewolf


Land Degradation & Development | 2017

Sediment reallocations due to erosive rainfall events in the Three Gorges Reservoir Area, Central China

Felix Stumpf; Philipp Goebes; Karsten Schmidt; Marcus Schindewolf; Sarah Schönbrodt-Stitt; Alexandre Wadoux; Wei Xiang; Thomas Scholten


Catena | 2016

Using terrestrial LiDAR data to analyse morphodynamics on steep unvegetated slopes driven by different geomorphic processes

Fabian Neugirg; Andreas Kaiser; Alena Huber; Tobias Heckmann; Marcus Schindewolf; Jürgen Schmidt; Michael Becht; Florian Haas


Earth Surface Processes and Landforms | 2017

Time lapse structure from motion photogrammetry for continuous geomorphic monitoring

Anette Eltner; Andreas Kaiser; Antonio Abellán; Marcus Schindewolf


Archive | 2015

Seasonal erosion patterns under alpine conditions: benefits and challenges of a novel approach in physically based soil erosion modeling

Marcus Schindewolf; Andreas Kaiser; Fabian Neugirg; Constanze Richter; Florian Haas; Jürgen Schmidt

Collaboration


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Jürgen Schmidt

Freiberg University of Mining and Technology

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Andreas Kaiser

Freiberg University of Mining and Technology

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Fabian Neugirg

Catholic University of Eichstätt-Ingolstadt

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Florian Haas

Catholic University of Eichstätt-Ingolstadt

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Michael Becht

The Catholic University of America

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Anette Eltner

Dresden University of Technology

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Alena Huber

Catholic University of Eichstätt-Ingolstadt

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Felix Stumpf

University of Tübingen

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