Articles | Volume 70, issue 2
https://doi.org/10.5194/gh-70-167-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Special issue:
https://doi.org/10.5194/gh-70-167-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
The use of a raindrop aggregate destruction device to evaluate sediment and soil organic carbon transport
L. Xiao
CORRESPONDING AUTHOR
Physical Geography and Environmental Change Group, Department of Environmental Sciences, University of Basel, Klingelbergstrasse 27, 4056 Basel, Switzerland
Y. Hu
Physical Geography and Environmental Change Group, Department of Environmental Sciences, University of Basel, Klingelbergstrasse 27, 4056 Basel, Switzerland
P. Greenwood
Physical Geography and Environmental Change Group, Department of Environmental Sciences, University of Basel, Klingelbergstrasse 27, 4056 Basel, Switzerland
N. J. Kuhn
Physical Geography and Environmental Change Group, Department of Environmental Sciences, University of Basel, Klingelbergstrasse 27, 4056 Basel, Switzerland
Related authors
No articles found.
Nikolaus Josef Kuhn and Federica Trudu
Earth Surf. Dynam. Discuss., https://doi.org/10.5194/esurf-2023-11, https://doi.org/10.5194/esurf-2023-11, 2023
Revised manuscript has not been submitted
Short summary
Short summary
In many ways, the surface of the planet Mars is similar to that of Earth. However, Mars' lower gravity has an effect on the sedimentation and transport of sedimentary material and the texture of sedimentary rocks. Using specific experimental equipment to measure settling velocity aboard a parabolic flight, it was possible to observe how sediments settled at Martian gravity. These experiments serve as analogues for surface processes on Mars.
Brice Prudat, Wolfgang Fister, Lena Bloemertz, Juliane Krenz, and Nikolaus J. Kuhn
Geogr. Helv., 77, 39–51, https://doi.org/10.5194/gh-77-39-2022, https://doi.org/10.5194/gh-77-39-2022, 2022
Short summary
Short summary
Soil quality depends on water availability for plants. Sandy soils with a poorly permeable layer (fragipan) are considered inept for agriculture. However they are cultivated in Namibia as they secure a minimum harvest during droughts. In order to understand the hydrological influence of fragipans in these soils, soil moisture content was measured. The results illustrate that the combination of sandy topsoil and shallow fragipan has beneficial effects on plant-available water during dry periods.
Philip Greenwood, Jan Bauer, and Nikolaus J. Kuhn
Geogr. Helv., 76, 319–333, https://doi.org/10.5194/gh-76-319-2021, https://doi.org/10.5194/gh-76-319-2021, 2021
Short summary
Short summary
Soil erosion by wind and water is a commonly recognized phenomenon on agricultural land. Erosion in forests is studied less and generally considered to be limited because of the soil protection by vegetation. However, trees, when toppled because of old age or wind, loosen a considerable amount of soil when their roots are pulled from the ground. In addition, the holes left in the ground act as collectors for water and concentrated runoff, causing significant soil loss on forested slopes.
Matthias Hunziker, Olafur Arnalds, and Nikolaus J. Kuhn
SOIL, 5, 223–238, https://doi.org/10.5194/soil-5-223-2019, https://doi.org/10.5194/soil-5-223-2019, 2019
Short summary
Short summary
Afforestation on severely degraded volcanic soils/landscapes is an important process concerning ecological restoration in Iceland. These landscapes have a high potential to act as carbon sinks. We tested the soil (0–30 cm) of different stages of afforested (mountain birch) landscapes and analysed the quantity and quality of the soil organic carbon. There is an increase in the total SOC stock during the encroachment. The increase is mostly because of POM SOC. Such soils demand SOC quality tests.
Wolfgang Fister, Nina Goldman, Marius Mayer, Manuel Suter, and Nikolaus J. Kuhn
Geogr. Helv., 74, 81–91, https://doi.org/10.5194/gh-74-81-2019, https://doi.org/10.5194/gh-74-81-2019, 2019
Vladimir R. Wingate, Nikolaus J. Kuhn, Stuart R. Phinn, and Cornelis van der Waal
Biogeosciences Discuss., https://doi.org/10.5194/bg-2019-28, https://doi.org/10.5194/bg-2019-28, 2019
Manuscript not accepted for further review
Brice Prudat, Lena Bloemertz, and Nikolaus J. Kuhn
SOIL, 4, 47–62, https://doi.org/10.5194/soil-4-47-2018, https://doi.org/10.5194/soil-4-47-2018, 2018
Short summary
Short summary
Soil degradation is a major threat for farmers of semi-arid north-central Namibia. Having tools to assess soil quality is important to evaluate soil conditions and helps targeting important issues. We developed a soil evaluation toolbox that integrates farmers' field experiences and technical knowledge. The combination of local soil descriptions, field soil texture evaluation and soil colour provides locally meaningful information that reveals soil quality improvement potentials.
P. Greenwood, M. Hoelzle, and N. J. Kuhn
Geogr. Helv., 70, 311–313, https://doi.org/10.5194/gh-70-311-2015, https://doi.org/10.5194/gh-70-311-2015, 2015
Short summary
Short summary
Editorial introducing the special issue of Geographica Helvetica: Mapping, Measuring and Modeling in Geomorphology.
P. Greenwood, S. Kuonen, W. Fister, and N. J. Kuhn
Geogr. Helv., 70, 63–73, https://doi.org/10.5194/gh-70-63-2015, https://doi.org/10.5194/gh-70-63-2015, 2015
Short summary
Short summary
Alpine and mountain slopes represent important pathways that link high-altitude grazing areas to meadows and rangelands at lower elevations. Given the acute gradients associated with such environments, we hypothesize that terracettes act as efficient runoff conveyance routes that facilitate the movement of runoff and associated material during erosion events. This hypothesis was partially disproved during a series of rainfall/runoff simulations on a well-developed terracette system, however.
Y. Hu and N. J. Kuhn
Biogeosciences, 11, 6209–6219, https://doi.org/10.5194/bg-11-6209-2014, https://doi.org/10.5194/bg-11-6209-2014, 2014
Related subject area
Physical Geography
Patrimoine géologique et géomorphologique : base pour le géotourisme et la création d'un géoparc UNESCO dans le Dahar (Sud-est tunisien)
Chancen, Herausforderungen und Risiken der Inwertsetzung des regionalen Geo-Erbes: Geotopschutz und Geotourismus im Spannungsfeld unterschiedlichster Interessen
The potential of fragipans in sustaining pearl millet during drought periods in north-central Namibia
The 1513 Monte Crenone rock avalanche: numerical model and geomorphological analysis
Evolution of fluvial environments and history of human settlements on the Ticino river alluvial plain
Schmidt hammer exposure-age dating of periglacial and glacial landforms in the Southern Swiss Alps based on R-value calibration using historical data
Assessing the ecological value of dynamic mountain geomorphosites
Assessing hillslope sediment generation potential by tree throw: a preliminary field study along a small river valley in the Jura Mountains, northwest Switzerland
Glacial lake outburst flood hazard assessment by satellite Earth observation in the Himalayas (Chomolhari area, Bhutan)
Reconstruction and actual trends of landslide activities in Bruust–Haltiwald, Horw, canton of Lucerne, Switzerland
Monitoring the crisis of a rock glacier with repeated UAV surveys
Regional-scale inventory of periglacial moving landforms connected to the torrential network system
Piecing together the Lateglacial advance phases of the Reussgletscher (central Swiss Alps)
A study of the Würm glaciation focused on the Valais region (Alps)
Last Glacial Maximum precipitation pattern in the Alps inferred from glacier modelling
Avalanche fatalities in the European Alps: long-term trends and statistics
Challenges and solutions for long-term permafrost borehole temperature monitoring and data interpretation
Introduction to the special issue of Geographica Helvetica: "Mapping, measuring and modeling in geomorphology"
Methods for detecting channel bed surface changes in a mountain torrent – experiences from the Dorfbach torrent
Risiko des Eintrags von Phosphor in den Hallwilersee durch Bodenerosion
Investigation on protalus ramparts in the Swiss Alps
Improvements in 3-D digital mapping for geomorphological and Quaternary geological cartography
Ground temperature variations in a talus slope influenced by permafrost: a comparison of field observations and model simulations
The influence of terracettes on the surface hydrology of steep-sloping and subalpine environments: some preliminary findings
Experimentelle Erkundung von Wildbächen, Murgängen, Hangrutschungen und Steinschlag: Aktuelle Beispiele der WSL
Editorial Publishing physical geography papers in Geographica Helvetica
Implications of climate change on Glacier de la Plaine Morte, Switzerland
Auswirkungen der Klimaänderung auf die schweizerische Wasserkraftnutzung
Topoclimatological case-study of Alpine pastures near the Albula Pass in the eastern Swiss Alps
A spatial and temporal analysis of different periglacial materials by using geoelectrical, seismic and borehole temperature data at Murtèl–Corvatsch, Upper Engadin, Swiss Alps
Emmanuel Reynard, Tarek Ben Fraj, Aziza Ghram Messedi, Hédi Ben Ouezdou, Mohamed Ouaja, and Yves Matthijs
Geogr. Helv., 77, 97–119, https://doi.org/10.5194/gh-77-97-2022, https://doi.org/10.5194/gh-77-97-2022, 2022
Short summary
Short summary
The study is a geomorphological analysis of Djebel Dahar, in south-eastern Tunisia, carried out as the basis for a UNESCO Global Geopark. We made a synthesis of the geographical, geological and geomorphological context of the area, proposed a delimitation for the future geopark, based on geological and geomorphological characteristics, and established a preliminary list of geosites, indicating their scientific value and their potential for geotourism.
Heidi Megerle, Simon Martin, and Géraldine Regolini
Geogr. Helv., 77, 53–66, https://doi.org/10.5194/gh-77-53-2022, https://doi.org/10.5194/gh-77-53-2022, 2022
Short summary
Short summary
In the field of regional geo-heritage promotion, this paper presents some opportunities, challenges and risks for geotope protection and geotourism.
Brice Prudat, Wolfgang Fister, Lena Bloemertz, Juliane Krenz, and Nikolaus J. Kuhn
Geogr. Helv., 77, 39–51, https://doi.org/10.5194/gh-77-39-2022, https://doi.org/10.5194/gh-77-39-2022, 2022
Short summary
Short summary
Soil quality depends on water availability for plants. Sandy soils with a poorly permeable layer (fragipan) are considered inept for agriculture. However they are cultivated in Namibia as they secure a minimum harvest during droughts. In order to understand the hydrological influence of fragipans in these soils, soil moisture content was measured. The results illustrate that the combination of sandy topsoil and shallow fragipan has beneficial effects on plant-available water during dry periods.
Alessandro De Pedrini, Christian Ambrosi, and Cristian Scapozza
Geogr. Helv., 77, 21–37, https://doi.org/10.5194/gh-77-21-2022, https://doi.org/10.5194/gh-77-21-2022, 2022
Short summary
Short summary
The Monte Crenone rock avalanche of 1513 is well known on the southern side of the Alps because in 1515 it generated the largest inundation that has occurred in Switzerland in the Common Era, the Buzza di Biasca. New geological and historical observations allowed the setup of a numerical model of this major event, permitting a better definition of the chain of consequences that affected the alluvial plain of the river Ticino from Biasca to Lake Maggiore between the 16th and the 19th century.
Dorota Czerski, Daphné Giacomazzi, and Cristian Scapozza
Geogr. Helv., 77, 1–20, https://doi.org/10.5194/gh-77-1-2022, https://doi.org/10.5194/gh-77-1-2022, 2022
Short summary
Short summary
The paper presents the results of recent geoarchaeological studies on the Ticino river alluvial plain. The sedimentological descriptions are combined with archaeological observations and constrained with radiocarbon dating. This approach, together with data from previous research and historical sources, provides an interesting overview of the eveolution of Ticino river morphosedimentary dynamics in relation to human settlements since the Neolithic.
Cristian Scapozza, Chantal Del Siro, Christophe Lambiel, and Christian Ambrosi
Geogr. Helv., 76, 401–423, https://doi.org/10.5194/gh-76-401-2021, https://doi.org/10.5194/gh-76-401-2021, 2021
Short summary
Short summary
Exposure ages make it possible to determine the time of weathering of a rock surface. They can be determined from rebound values measured with the Schmidt hammer and calibrated on surfaces of known age, defined in this study thanks to historical cartography and two mule tracks built in 300 and 1250 CE, which allowed us to reconstruct glacier fluctuations over the last 3 centuries in Val Scaradra and to define the time of deglaciation and rock glacier development in the Splügenpass region.
Jonathan Bussard and Elisa Giaccone
Geogr. Helv., 76, 385–399, https://doi.org/10.5194/gh-76-385-2021, https://doi.org/10.5194/gh-76-385-2021, 2021
Short summary
Short summary
In mountain environments, active geomorphological processes have a strong influence on plant diversity because they act as renovators for habitats of pioneer species. In this paper, we propose criteria to assess the ecological value of dynamic mountain geomorphosites. We show that the interest of plant communities and the influence of geomorphological processes on plant communities are fundamental criteria for assessing ecological value in an exhaustive and objective way.
Philip Greenwood, Jan Bauer, and Nikolaus J. Kuhn
Geogr. Helv., 76, 319–333, https://doi.org/10.5194/gh-76-319-2021, https://doi.org/10.5194/gh-76-319-2021, 2021
Short summary
Short summary
Soil erosion by wind and water is a commonly recognized phenomenon on agricultural land. Erosion in forests is studied less and generally considered to be limited because of the soil protection by vegetation. However, trees, when toppled because of old age or wind, loosen a considerable amount of soil when their roots are pulled from the ground. In addition, the holes left in the ground act as collectors for water and concentrated runoff, causing significant soil loss on forested slopes.
Cristian Scapozza, Christian Ambrosi, Massimiliano Cannata, and Tazio Strozzi
Geogr. Helv., 74, 125–139, https://doi.org/10.5194/gh-74-125-2019, https://doi.org/10.5194/gh-74-125-2019, 2019
Short summary
Short summary
A glacial lake outburst flood hazard assessment by satellite Earth observation and numerical modelling was done for the lakes linked to the Thangothang Chhu glacier, Chomolhari area (Bhutan), combining detailed geomorphological mapping, landslide and rock glacier inventories, as well as surface displacements quantified by satellite InSAR. Outburst scenario modelling revealed that only a flood wave can have an impact on the two human settlements located downslope of the glacier.
Philippe Burkhalter, Markus Egli, and Holger Gärtner
Geogr. Helv., 74, 93–103, https://doi.org/10.5194/gh-74-93-2019, https://doi.org/10.5194/gh-74-93-2019, 2019
Short summary
Short summary
A spatiotemporal reconstruction of slope movements on the edge of Lake Lucerne near the municipality of Horw, canton of Lucerne is presented. The reconstruction was realized by analyzing growth reactions of beech (Fagus sylvatica L.) and fir (Abies alba Mill.) trees growing on this slope. Results show that the area has been moving at least since 1948. A significant concentration of events was observed between 1990 and 2000 as well as after 2006.
Sebastián Vivero and Christophe Lambiel
Geogr. Helv., 74, 59–69, https://doi.org/10.5194/gh-74-59-2019, https://doi.org/10.5194/gh-74-59-2019, 2019
Mario Kummert and Reynald Delaloye
Geogr. Helv., 73, 357–371, https://doi.org/10.5194/gh-73-357-2018, https://doi.org/10.5194/gh-73-357-2018, 2018
Max Boxleitner, Susan Ivy-Ochs, Dagmar Brandova, Marcus Christl, Markus Egli, and Max Maisch
Geogr. Helv., 73, 241–252, https://doi.org/10.5194/gh-73-241-2018, https://doi.org/10.5194/gh-73-241-2018, 2018
Patrick Becker, Martin Funk, Christian Schlüchter, and Kolumban Hutter
Geogr. Helv., 72, 421–442, https://doi.org/10.5194/gh-72-421-2017, https://doi.org/10.5194/gh-72-421-2017, 2017
Short summary
Short summary
This article studies the ice flow in the Valais region during the last glaciation (Würm) in detail. The numerical modelling shows a discrepancy of the height of the ice cap compared to the geomorphological evidence based on trimlines. However, geomorphological evidence at the Simplon Pass indicating an ice flow from the Rhone valley into the valley of Toce was confirmed. Furthermore it is shown that for this confirmation a sufficient ice thickness is obligatory.
Patrick Becker, Julien Seguinot, Guillaume Jouvet, and Martin Funk
Geogr. Helv., 71, 173–187, https://doi.org/10.5194/gh-71-173-2016, https://doi.org/10.5194/gh-71-173-2016, 2016
Frank Techel, Frédéric Jarry, Georg Kronthaler, Susanna Mitterer, Patrick Nairz, Miha Pavšek, Mauro Valt, and Gian Darms
Geogr. Helv., 71, 147–159, https://doi.org/10.5194/gh-71-147-2016, https://doi.org/10.5194/gh-71-147-2016, 2016
Short summary
Short summary
During the last 45 years, about 100 people lost their lives in avalanches in the European Alps each year. Avalanche fatalities in settlements and on transportation corridors have considerably decreased since the 1970s. In contrast, the number of avalanche fatalities during recreational activities away from avalanche-secured terrain doubled between the 1960s and 1980s and has remained relatively stable since, despite a continuing strong increase in winter backcountry recreational activities.
Rachel Luethi and Marcia Phillips
Geogr. Helv., 71, 121–131, https://doi.org/10.5194/gh-71-121-2016, https://doi.org/10.5194/gh-71-121-2016, 2016
Short summary
Short summary
Long-term borehole temperature monitoring in mountain permafrost environments is challenging under the hostile conditions reigning there. On the basis of data measured in the SLF borehole network we show situations where ground temperature data should be interpreted with caution. A selection of recently observed problems are discussed, and advantages and possible drawbacks of various solutions including data correction, measurement redundancy or alternate instrumentation are presented.
P. Greenwood, M. Hoelzle, and N. J. Kuhn
Geogr. Helv., 70, 311–313, https://doi.org/10.5194/gh-70-311-2015, https://doi.org/10.5194/gh-70-311-2015, 2015
Short summary
Short summary
Editorial introducing the special issue of Geographica Helvetica: Mapping, Measuring and Modeling in Geomorphology.
C. Willi, C. Graf, Y. Deubelbeiss, and M. Keiler
Geogr. Helv., 70, 265–279, https://doi.org/10.5194/gh-70-265-2015, https://doi.org/10.5194/gh-70-265-2015, 2015
Short summary
Short summary
The erosion of and depositions on channel bed surfaces are instrumental to understanding debris flow processes. We present different methods and highlight their pro and cons. Terrestrial and airborne laser scanning, erosion sensors, cross sections and geomorphological mapping are compared. Two of these approaches are tested and applied in a torrent. The results indicate that the methods are associated with variable temporal and spatial resolution as well as data quality and invested effort.
S. Müller and D. Schaub
Geogr. Helv., 70, 193–198, https://doi.org/10.5194/gh-70-193-2015, https://doi.org/10.5194/gh-70-193-2015, 2015
C. Scapozza
Geogr. Helv., 70, 135–139, https://doi.org/10.5194/gh-70-135-2015, https://doi.org/10.5194/gh-70-135-2015, 2015
Short summary
Short summary
In the scientific literature, “protalus ramparts” can designate both a nivo-gravitational landform (also called “pronival ramparts”) and a permafrost-related landform. Thanks to a selection of eight major diagnostic criteria defined from observations carried out in the Swiss Alps, it was highlighted that the structure, ice content and creep dynamics of protalus ramparts are the same as many rock glaciers. Protalus rampart were therefore defined simply as a (small) active talus rock glacier.
C. Ambrosi and C. Scapozza
Geogr. Helv., 70, 121–133, https://doi.org/10.5194/gh-70-121-2015, https://doi.org/10.5194/gh-70-121-2015, 2015
Short summary
Short summary
Some examples of 3-D digital mapping for Quaternary geological and geomorphological cartography are presented in this paper. Examples concern in particular the Quaternary geological cartography around the well-know Flims rockslide area (Graubünden), performed in the framework of the GeoCover project launched by the Swiss Geological Survey, and the landslide and glacial/periglacial landform mapping and inventorying in the southern Swiss Alps (Ticino) for assessing the slope tectonic activity.
B. Staub, A. Marmy, C. Hauck, C. Hilbich, and R. Delaloye
Geogr. Helv., 70, 45–62, https://doi.org/10.5194/gh-70-45-2015, https://doi.org/10.5194/gh-70-45-2015, 2015
P. Greenwood, S. Kuonen, W. Fister, and N. J. Kuhn
Geogr. Helv., 70, 63–73, https://doi.org/10.5194/gh-70-63-2015, https://doi.org/10.5194/gh-70-63-2015, 2015
Short summary
Short summary
Alpine and mountain slopes represent important pathways that link high-altitude grazing areas to meadows and rangelands at lower elevations. Given the acute gradients associated with such environments, we hypothesize that terracettes act as efficient runoff conveyance routes that facilitate the movement of runoff and associated material during erosion events. This hypothesis was partially disproved during a series of rainfall/runoff simulations on a well-developed terracette system, however.
M. Stähli, C. Graf, C. Scheidl, C. R. Wyss, and A. Volkwein
Geogr. Helv., 70, 1–9, https://doi.org/10.5194/gh-70-1-2015, https://doi.org/10.5194/gh-70-1-2015, 2015
M. Hoelzle and E. Reynard
Geogr. Helv., 68, 225–226, https://doi.org/10.5194/gh-68-225-2013, https://doi.org/10.5194/gh-68-225-2013, 2013
M. Huss, A. Voinesco, and M. Hoelzle
Geogr. Helv., 68, 227–237, https://doi.org/10.5194/gh-68-227-2013, https://doi.org/10.5194/gh-68-227-2013, 2013
R. Weingartner, B. Schädler, and P. Hänggi
Geogr. Helv., 68, 239–248, https://doi.org/10.5194/gh-68-239-2013, https://doi.org/10.5194/gh-68-239-2013, 2013
P. Michna, W. Eugster, R. V. Hiller, M. J. Zeeman, and H. Wanner
Geogr. Helv., 68, 249–263, https://doi.org/10.5194/gh-68-249-2013, https://doi.org/10.5194/gh-68-249-2013, 2013
S. Schneider, S. Daengeli, C. Hauck, and M. Hoelzle
Geogr. Helv., 68, 265–280, https://doi.org/10.5194/gh-68-265-2013, https://doi.org/10.5194/gh-68-265-2013, 2013
Cited articles
Angima, S. D., Stott, D. E., O'Neill, M. K., Ong, C. K., and Weesies, G. A.: Soil erosion prediction using RUSLE for central Kenyan highland conditions, Agric. Ecosyst. Environ., 97, 295–308, 2003.
Borselli, L., Torri, D., Poesen, J., and Sanchis, P.: Effects of water quality on infiltration, runoff and interrill erosion processes during simulated rainfall, Earth Surf. Process. Landf., 26, 329–342, 2001.
Cheng, N. S.: Simplified settling velocity formula for sediment particle, J. Hydraul. Res., 123, 149–152, 1997.
Croft, H., Kuhn, N. J., and Anderson, K.: On the use of remote sensing techniques for monitoring spatio-temporal soil organic carbon dynamics in agricultural systems, Catena, 94, 64–74, 2012a.
Croft, H., Anderson, K., and Kuhn, N. J.: Reflectance anisotropy for measuring soil surface roughness of multiple soil types, Catena, 93, 87–96, 2012b.
De Baets, D., Torri, D., Poesen, J., and Meersmans, J.: Modelling increased soil cohesion due to roots with EUROSEM, Earth Surf. Process. Land., 33, 1948–1963, 2008.
Dietrich, W. E.: Settling velocity of natural particles, Water Resour. Res., 18, 1615–1626, 1982.
FAO/ISRIC/ISSS: World Reference Base for Soil Resources, FAO: Rome, 1998.
Ferguson, R. I. and Church, M.: A simple universal equation for grain settling velocity, J. Sediment Res., 74, 933–937, 2004.
Gibbs, R. J., Matthews, M. D., and Link, D. A.: The relationship between sphere size and settling velocity, J. Sediment Petrol., 41, 7–18, 1971.
Hairsine, P. B. and McTainsh, G. H.: The Griffith tube: a simple settling tube for the measurement of settling velocity of soil aggregates, AES working paper 3/86, Griffith University, Brisbane, 1986.
Hallermeier, R. J.: Terminal settling velocity of commonly occurring sand grains, Sedimentology, 28, 859–865, 1981.
Hu, Y. and Kuhn, N. J.: Aggregates reduce transport distance of soil organic carbon: are our balances correct?, Biogeosciences, 11, 6209–6219, https://doi.org/10.5194/bg-11-6209-2014, 2014.
Hu, Y., Fister, W., and Kuhn, N. J.: Temporal variation of SOC enrichment from interrill erosion over prolonged rainfall simulations, Agriculture, 3, 726–740, 2013a.
Hu, Y., Fister, W., Rüegg, H. R., Kinnell, P. I. A., and Kuhn, N. J.: The use of Equivalent Quatz Size and settling tube apparatus to fractionate soil aggregates by settling velocity, Geomorphol. Tech. Online Ed. Br. Soc. Geomorphol., Section 1.1.1, 2013b.
Iserloh, T., Fister, W., Seeger, M., Willger, H., and Ries, J. B.: A small portable rainfall simulator for reproducible experiments on soil erosion, Soil Tillage Res., 124, 131–137, 2012.
Kaiser, M., Berhe, A. A., Sommer, M., and Kleber, M.: Application of ultrasound to disperse soil aggregates of high mechanical stability, J. Plant. Nutr. Soil. Sci., 175, 521–526, 2012.
Kinnell, P. I. A.: Particle travel distances and bed and sediment compositions associated with rain-Impacted flows, Earth. Surf. Proc. Land., 26, 749–758, 2001.
Kinnell, P. I. A.: Raindrop-impact-induced erosion processes and prediction: a review, Hydrol. Proc., 19, 2815–2844, 2005.
Kuhn, N. J.: Assessing lateral organic Carbon movement in small agricultural catchments, in: Mattertal – ein Tal in Bewegung, edited by: Graf, C., Publikation zur Jahrestagung der Schweizerischen Geomorphologischen Gesellschaft 29 Juni–1 Juli 2011, St. Niklaus. Birmensdorf, Eidg. Forschungsanstalt WSL, 151–164, 2013.
Kuhn, N. J. and Armstrong, E. K.: Erosion of organic matter from sandy soils: solving the mass balance, Catena, 98, 87–95, 2012.
Kuhn, N. J., Hoffmann, T., Schwanghart, W., and Dotterweich, M.: Agricultural soil erosion and global carbon cycle: controversy over?, Earth. Surf. Proc. Land., 34, 1033–1038, 2009.
Lal, R.: Soil carbon sequestration impacts on global climate change and food security, Science, 304, 1623–1627, 2004.
Lal, R.: Soil erosion and carbon dynamics, Soil Till. Res., 81, 137–142, 2005.
Le Bissonnais, Y.: Aggregate stability and assessment of soil crustability and erodibility: I. Theory and methodology, Eur. J. Soil Sci., 47, 425–437, 1996.
Legout, C., Leguedois, S., and Le Bissonnais, Y.: Aggregate breakdown dynamics under rainfall compared with aggregate stability measurements, Eur. J. Soil Sci., 56, 225–237, 2005.
Loch, R. J.: Settling velocity – a new approach to assessing soil and sediment properties, Comput. Electron. Agr., 31, 305–316, 2001.
Lu, H., Moran, C. J., and Prosser, I. P.: Modelling sediment delivery ratio over the Murray Darling Basin, Environ. Model. Softw., 21, 1297–1308, 2006.
MeteoSwiss: Monthly total precipitation during April, May, and June at Station Arisdorf near Möhlin from 1985 to 2012, 2013.
Nadeu, E., De Vente, J., Martínez-Mena, M., and Boix-Fayos, C.: Exploring particle size distribution and organic carbon pools mobilized by different erosion processes at the catchment scale, J. Soil. Sediment., 11, 667–678, 2011.
Olsen, P. and Kristensen, P. R.: Using a GIS system in mapping risks of nitrate leaching and erosion on the basis of SOIL/SOIL-N and USLE simulations, Nutr. Cycl. Agroecosys., 50, 307–311, 1998.
Pieri, L., Bittelli, M., Wu, J. Q., Dun, S., Flanagan, D. C., Pisa, P. R., Ventura, F., and Salvatorelli, F.: Using the Water Erosion Prediction Project (WEPP) model to simulate field-observed runoff and erosion in the Apennines Mountain Range, Italy. J. Hydrol., 336, 84–97, 2007.
Quinton, J. N., Catt, J. A., and Hess, T. M.: The selective removal of phosphorus from soil: is event size important?, J. Environ. Qual., 30, 538–545, 2001.
Stallard, R. F.: Terrestrial sedimentation and the carbon cycling: coupling weathering and erosion to carbon burial, Global Biogeochem. Cy., 12, 231–257, 1998.
Starr, G. C., Lal, R., Malone, R., Hothem, D., Owens, L., and Kimble, J.: Modeling soil carbon transported by water erosion process, Land Degrad. Dev., 11, 83–91, 2000.
Stokes, G. G.: On the effect of the internal friction of fluids on the motion of pendulums, Trans. Camb. Phil. Soc., 9, 8–106, 1851.
Torri ,D., Regüés, D., Pellegrini, S., and Bazzoffi, P.: Within-storm soil surface dynamics and erosive effects of rainstorms, Catena, 38, 131–150, 1999.
van Oost, K., Beuselinck, L., Hairsine, P. B., and Govers, G.: Spatial evaluation of a multi-class sediment transport and deposition model, Earth. Surf. Proc. Land., 29, 1027–1044, 2004.
van Oost, K., Quine, T. A., Govers, G., De Gryze, S., Six, J., Harden, J. W., Ritchie, J. C., McCarty, G. W., Heckrath, G., Kosmas, C., Giraldez, J. V., Marques da Silva, J. R., and Merckx, R.: The impact of agricultural soil erosion on the global carbon cycle, Science, 318, 626–629, 2007.
Walling, D. E.: Erosion and sediment yield research – some recent perspectives, J. Hydrol., 100, 113–141, 1988.
Wang, J. G., Li, Z. X., Cai, C. F., and Ma R. M.: Particle size and shape variation of Ultisol aggregates affected by abrasion under different transport distances in overland flow, Catena, 123, 153–162, 2014.
Theme issue