Articles | Volume 6, issue 2
https://doi.org/10.5194/soil-6-337-2020
© 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/soil-6-337-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Modeling soil and landscape evolution – the effect of rainfall and land-use change on soil and landscape patterns
W. Marijn van der Meij
CORRESPONDING AUTHOR
Soil Geography and Landscape Group, Wageningen University and
Research, P.O. Box 47, 6700 AA, Wageningen, the Netherlands
Research Area Landscape Functioning, Working Group Landscape Pedology,
Leibniz-Centre for Agricultural Landscape Research ZALF, Eberswalder
Straße 84, 15374 Müncheberg, Germany
Arnaud J. A. M. Temme
Department of Geography, Kansas State University, 920 N17th Street,
Manhattan, KS 66506, USA
Institute of Arctic and Alpine Research, University of Colorado,
Campus, P.O. Box 450, Boulder, CO 80309-0450, USA
Jakob Wallinga
Soil Geography and Landscape Group, Wageningen University and
Research, P.O. Box 47, 6700 AA, Wageningen, the Netherlands
Michael Sommer
Research Area Landscape Functioning, Working Group Landscape Pedology,
Leibniz-Centre for Agricultural Landscape Research ZALF, Eberswalder
Straße 84, 15374 Müncheberg, Germany
Institute of Environmental Science & Geography, University of
Potsdam, Karl-Liebknecht-Straße 24–25, 14476 Potsdam, Germany
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This preprint is open for discussion and under review for SOIL (SOIL).
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In the study, we reprocessed mapping results using a catchment-based method to reveal how properties change vertically with depth and horizontally across the landscape. Vertically, variations arise from factors like parent material, topography and tree uprooting. Horizontally, soils reflect erosion by wind and water. We identified sensitive areas. By combining two approach, we can better visualize soil variability, supporting better land management decisions in environmentally sensitive zones.
W. Marijn van der Meij and Peter Finke
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We used soil evolution model SoilGen to simulate long-term soil organic carbon (SOC) sequestration under varying environmental conditions and internal protection mechanisms. Our results revealed a strong role of pedogenetic and environmental history on current-day and future SOC sequestration potential. We propose a framework for developing topical digital twins of long-term soil processes to monitor and project future development of specific soil properties under global change.
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We investigated geomorphological activity and stability of surfaces and soils along a climatic transect in the Atacama Desert. Single grain luminescence data and sediment analyses reveal recent deposition and shallow post-depositional mixing. Two distinct phases of enhanced activity align with previously reported wetter intervals, demonstrating the sensitivity of arid landscape dynamics to climatic variability.
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Geoscientific projects often struggle to manage complex data effectively, resulting in valuable information being lost due to poor findability and accessibility. To address this, we present a comprehensive research data framework for storing and processing data throughout a project, from fieldwork to data analysis. This ensures that datasets are clearly defined, reproducible and adhere to the FAIR principles (findability, accessibility, interoperability and reusability).
W. Marijn van der Meij
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A soil-landscape evolution model was used to calculate hillslope erosion rates from OSL-based (Optically Stimulated Luminescence) deposition ages through inverse modelling, with consideration of uncertainties in model input. The results show that erosion rates differ systematically from the deposition rates, highlighting important shortcomings of assessing land degradation through measurable deposition rates.
W. Marijn van der Meij, Svenja Riedesel, and Tony Reimann
SOIL, 11, 51–66, https://doi.org/10.5194/soil-11-51-2025, https://doi.org/10.5194/soil-11-51-2025, 2025
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Soil mixing (bioturbation) plays a key role in soil functions, but the underlying processes are poorly understood and difficult to quantify. In this study, we use luminescence, a light-sensitive soil mineral property, and numerical models to better understand different types of bioturbation. We provide a conceptual model that helps to determine which types of bioturbation processes occur in a soil and a numerical model that can derive quantitative process rates from luminescence measurements.
W. Marijn van der Meij, Arnaud J. A. M. Temme, Steven A. Binnie, and Tony Reimann
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We present our model ChronoLorica. We coupled the original Lorica model, which simulates soil and landscape evolution, with a geochronological module that traces cosmogenic nuclide inventories and particle ages through simulations. These properties are often measured in the field to determine rates of landscape change. The coupling enables calibration of the model and the study of how soil, landscapes and geochronometers change under complex boundary conditions such as intensive land management.
W. Marijn van der Meij
SOIL, 8, 381–389, https://doi.org/10.5194/soil-8-381-2022, https://doi.org/10.5194/soil-8-381-2022, 2022
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The development of soils and landscapes can be complex due to changes in climate and land use. Computer models are required to simulate this complex development. This research presents a new method to analyze and visualize the results of these models. This is done with the use of evolutionary pathways (EPs), which describe how soil properties change in space and through time. I illustrate the EPs with examples from the field and give recommendations for further use of EPs in soil model studies.
Shuran Gao, Zhuodong Zhang, W. Marijn van der Meij, Yuxin Feng, Min Wu, and Yihua Song
EGUsphere, https://doi.org/10.5194/egusphere-2026-1837, https://doi.org/10.5194/egusphere-2026-1837, 2026
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Short summary
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In the study, we reprocessed mapping results using a catchment-based method to reveal how properties change vertically with depth and horizontally across the landscape. Vertically, variations arise from factors like parent material, topography and tree uprooting. Horizontally, soils reflect erosion by wind and water. We identified sensitive areas. By combining two approach, we can better visualize soil variability, supporting better land management decisions in environmentally sensitive zones.
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SOIL, 12, 165–186, https://doi.org/10.5194/soil-12-165-2026, https://doi.org/10.5194/soil-12-165-2026, 2026
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We used soil evolution model SoilGen to simulate long-term soil organic carbon (SOC) sequestration under varying environmental conditions and internal protection mechanisms. Our results revealed a strong role of pedogenetic and environmental history on current-day and future SOC sequestration potential. We propose a framework for developing topical digital twins of long-term soil processes to monitor and project future development of specific soil properties under global change.
Linda Andrea Elisabeth Maßon, Simon Matthias May, Svenja Riedesel, Willem Marijn van der Meij, Stephan Opitz, Andreas Peffeköver, and Tony Reimann
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We investigated geomorphological activity and stability of surfaces and soils along a climatic transect in the Atacama Desert. Single grain luminescence data and sediment analyses reveal recent deposition and shallow post-depositional mixing. Two distinct phases of enhanced activity align with previously reported wetter intervals, demonstrating the sensitivity of arid landscape dynamics to climatic variability.
Tjitske J. Kooistra, Anna-Maartje de Boer, Tjeerd J. Bouma, Natascia Pannozzo, Stuart G. Pearson, Ad van der Spek, Henko de Stigter, Jakob Wallinga, Rob Witbaard, and Karline Soetaert
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On intertidal flats, it is hard to distinguish sediment mixing by animals from reworking by waves and currents. We used a combination of tracers to identify reworking of grains of different sizes on the short- and long term. Coarse (sand) grains were less mobile than fine (mud) grains, and partly kept their layering after deposition. The luminescence properties of sand grains can be used dating and can show sediment mixing, but this method needs to be tested more for young, intertidal sediments.
Luis Alfredo Pires Barbosa, Martin Leue, Marc Wehrhan, and Michael Sommer
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Healthy soils rely on plant biomass, especially roots. We studied how wheat cultivar development interacts with soil erosion-deposition in carbon inputs. Tillage erosion reduced total biomass, while modern varieties yielded more grain but returned less carbon. Simulations showed newer cultivars are more drought-sensitive, revealing a trade-off between high yields and soil health.
Dennis Handy, W. Marijn Van der Meij, Mirijam Zickel, and Tony Reimann
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Geoscientific projects often struggle to manage complex data effectively, resulting in valuable information being lost due to poor findability and accessibility. To address this, we present a comprehensive research data framework for storing and processing data throughout a project, from fieldwork to data analysis. This ensures that datasets are clearly defined, reproducible and adhere to the FAIR principles (findability, accessibility, interoperability and reusability).
W. Marijn van der Meij
Earth Surf. Dynam., 13, 845–860, https://doi.org/10.5194/esurf-13-845-2025, https://doi.org/10.5194/esurf-13-845-2025, 2025
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A soil-landscape evolution model was used to calculate hillslope erosion rates from OSL-based (Optically Stimulated Luminescence) deposition ages through inverse modelling, with consideration of uncertainties in model input. The results show that erosion rates differ systematically from the deposition rates, highlighting important shortcomings of assessing land degradation through measurable deposition rates.
Sigrid van Grinsven, Noortje E. M. Janssen, Collin van Rooij, Ruben Peters, and Arnaud Temme
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When glaciers retreat, new land surface is revealed. Using detailed glacial retreat maps, it is possible to determine for how long a location has been ice-free. This age is used in this study to analyse how fast carbon is incorporated into the soil. Our results show that the wetness of the soil strongly determines the CO2 uptake and carbon incorporation rates. Wetlands cover a small percentage of the land surface but are nonetheless important for the carbon storage in the deglaciated area.
W. Marijn van der Meij, Svenja Riedesel, and Tony Reimann
SOIL, 11, 51–66, https://doi.org/10.5194/soil-11-51-2025, https://doi.org/10.5194/soil-11-51-2025, 2025
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Soil mixing (bioturbation) plays a key role in soil functions, but the underlying processes are poorly understood and difficult to quantify. In this study, we use luminescence, a light-sensitive soil mineral property, and numerical models to better understand different types of bioturbation. We provide a conceptual model that helps to determine which types of bioturbation processes occur in a soil and a numerical model that can derive quantitative process rates from luminescence measurements.
Jungyu Choi, Roy van Beek, Elizabeth L. Chamberlain, Tony Reimann, Harm Smeenge, Annika van Oorschot, and Jakob Wallinga
SOIL, 10, 567–586, https://doi.org/10.5194/soil-10-567-2024, https://doi.org/10.5194/soil-10-567-2024, 2024
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This research applies luminescence dating methods to a plaggic anthrosol in the eastern Netherlands to understand the formation history of the soil. To achieve this, we combined both quartz and feldspar luminescence dating methods. We developed a new method for feldspar to largely avoid the problem occurring from poorly bleached grains by examining two different signals from a single grain. Through our research, we were able to reconstruct the timing and processes of plaggic anthrosol formation.
Adrian Dahlmann, Mathias Hoffmann, Gernot Verch, Marten Schmidt, Michael Sommer, Jürgen Augustin, and Maren Dubbert
Hydrol. Earth Syst. Sci., 27, 3851–3873, https://doi.org/10.5194/hess-27-3851-2023, https://doi.org/10.5194/hess-27-3851-2023, 2023
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Evapotranspiration (ET) plays a pivotal role in terrestrial water cycling, returning up to 90 % of precipitation to the atmosphere. We studied impacts of soil type and management on an agroecosystem using an automated system with modern modeling approaches. We modeled ET at high spatial and temporal resolution to highlight differences in heterogeneous soils on an hourly basis. Our results show significant differences in yield and smaller differences in ET overall, impacting water use efficiency.
W. Marijn van der Meij, Arnaud J. A. M. Temme, Steven A. Binnie, and Tony Reimann
Geochronology, 5, 241–261, https://doi.org/10.5194/gchron-5-241-2023, https://doi.org/10.5194/gchron-5-241-2023, 2023
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We present our model ChronoLorica. We coupled the original Lorica model, which simulates soil and landscape evolution, with a geochronological module that traces cosmogenic nuclide inventories and particle ages through simulations. These properties are often measured in the field to determine rates of landscape change. The coupling enables calibration of the model and the study of how soil, landscapes and geochronometers change under complex boundary conditions such as intensive land management.
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Earth Syst. Sci. Data, 15, 1059–1075, https://doi.org/10.5194/essd-15-1059-2023, https://doi.org/10.5194/essd-15-1059-2023, 2023
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Arctic soils store large amounts of carbon and nutrients. The availability of nutrients, such as silicon, calcium, iron, aluminum, phosphorus, and amorphous silica, is crucial to understand future carbon fluxes in the Arctic. Here, we provide, for the first time, a unique dataset of the availability of the abovementioned nutrients for the different soil layers, including the currently frozen permafrost layer. We relate these data to several geographical and geological parameters.
Cindy Quik, Ype van der Velde, Jasper H. J. Candel, Luc Steinbuch, Roy van Beek, and Jakob Wallinga
Biogeosciences, 20, 695–718, https://doi.org/10.5194/bg-20-695-2023, https://doi.org/10.5194/bg-20-695-2023, 2023
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In NW Europe only parts of former peatlands remain. When these peatlands formed is not well known but relevant for questions on landscape, climate and archaeology. We investigated the age of Fochteloërveen, using radiocarbon dating and modelling. Results show that peat initiated at several sites 11 000–7000 years ago and expanded rapidly 5000 years ago. Our approach may ultimately be applied to model peat ages outside current remnants and provide a view of these lost landscapes.
W. Marijn van der Meij
SOIL, 8, 381–389, https://doi.org/10.5194/soil-8-381-2022, https://doi.org/10.5194/soil-8-381-2022, 2022
Short summary
Short summary
The development of soils and landscapes can be complex due to changes in climate and land use. Computer models are required to simulate this complex development. This research presents a new method to analyze and visualize the results of these models. This is done with the use of evolutionary pathways (EPs), which describe how soil properties change in space and through time. I illustrate the EPs with examples from the field and give recommendations for further use of EPs in soil model studies.
Marc Wehrhan, Daniel Puppe, Danuta Kaczorek, and Michael Sommer
Biogeosciences, 18, 5163–5183, https://doi.org/10.5194/bg-18-5163-2021, https://doi.org/10.5194/bg-18-5163-2021, 2021
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UAS remote sensing provides a promising tool for new insights into Si biogeochemistry at catchment scale. Our study on an artificial catchment shows surprisingly high silicon stocks in the biomass of two grass species (C. epigejos, 7 g m−2; P. australis, 27 g m−2). The distribution of initial sediment properties (clay, Tiron-extractable Si, nitrogen, plant-available potassium) controlled the spatial distribution of C. epigejos. Soil wetness determined the occurrence of P. australis.
Cited articles
Alewell, C., Egli, M., and Meusburger, K.: An attempt to estimate tolerable
soil erosion rates by matching soil formation with denudation in Alpine
grasslands, J. Soil. Sediment., 15, 1383–1399, 2015.
Allen, R. G., Pereira, L. S., Raes, D., and Smith, M.: Crop
evapotranspiration-Guidelines for computing crop water requirements,
Irrigation and drainage paper 56, FAO, Rome, 1998.
Amundson, R. and Jenny, H.: The place of humans in the state factor theory
of ecosystems and their soils, Soil Sci., 151, 99–109, 1991.
Amundson, R., Berhe, A. A., Hopmans, J. W., Olson, C., Sztein, A. E., and
Sparks, D. L.: Soil and human security in the 21st century, Science, 348,
1261071, https://doi.org/10.1126/science.1261071, 2015.
Angelini, M. E., Heuvelink, G. B. M., Kempen, B., and Morrás, H. J. M.:
Mapping the soils of an Argentine Pampas region using structural equation
modelling, Geoderma, 281, 102–118, 2016.
Bai, Z. G., Dent, D. L., Olsson, L., and Schaepman, M. E.: Proxy global
assessment of land degradation, Soil Use Manage., 24, 223–234, 2008.
Bajard, M., Poulenard, J., Sabatier, P., Develle, A.-L., Giguet-Covex, C.,
Jacob, J., Crouzet, C., David, F., Pignol, C., and Arnaud, F.: Progressive
and regressive soil evolution phases in the Anthropocene, CATENA, 150,
39–52, 2017.
Barnhart, K. R., Glade, R. C., Shobe, C. M., and Tucker, G. E.: Terrainbento 1.0: a Python package for multi-model analysis in long-term drainage basin evolution, Geosci. Model Dev., 12, 1267–1297, https://doi.org/10.5194/gmd-12-1267-2019, 2019.
Berhe, A. A., Barnes, R. T., Six, J., and Marín-Spiotta, E.: Role of
Soil Erosion in Biogeochemical Cycling of Essential Elements: Carbon,
Nitrogen, and Phosphorus, Annu. Rev. Earth Pl. Sc., 46,
521–548, 2018.
Bibby, J. S. and Mackney, D.: Land use capability classification, Rothamsted
Experimental Station, Harpenden, England, 27 pp., 1969.
Bouma, J.: Soil science contributions towards sustainable development goals
and their implementation: linking soil functions with ecosystem services,
J. Plant Nutr. Soil. Sc., 177, 111–120, 2014.
Brubaker, S. C., Holzhey, C. S., and Brasher, B. R.: Estimating the
water-dispersible clay content of soils, Soil Sci. Soc. Am.
J., 56, 1226–1232, 1992.
Budyko, M. I. and Miller, D. H.: Climate and life, Academic press, New York, 507 pp.,
1974.
Catt, J. A.: The agricultural importance of loess, Earth-Sci. Rev.,
54, 213–229, 2001.
Chappell, A., Baldock, J., and Sanderman, J.: The global significance of
omitting soil erosion from soil organic carbon cycling schemes, Nat.
Clim. Change, 6, 187–191, 2015.
Chen, S., Richer-de-Forges, A. C., Saby, N. P. A., Martin, M. P., Walter,
C., and Arrouays, D.: Building a pedotransfer function for soil bulk density
on regional dataset and testing its validity over a larger area, Geoderma,
312, 52–63, 2018.
Christakos, G.: Modern spatiotemporal geostatistics, Oxford University
Press, Oxford, 312 pp., 2000.
Cowie, A. L., Orr, B. J., Castillo Sanchez, V. M., Chasek, P., Crossman, N.
D., Erlewein, A., Louwagie, G., Maron, M., Metternicht, G. I., Minelli, S.,
Tengberg, A. E., Walter, S., and Welton, S.: Land in balance: The scientific
conceptual framework for Land Degradation Neutrality, Environ. Sci.
Pol. 79, 25–35, 2018.
De Alba, S., Lindstrom, M., Schumacher, T. E., and Malo, D. D.: Soil
landscape evolution due to soil redistribution by tillage: a new conceptual
model of soil catena evolution in agricultural landscapes, CATENA, 58,
77–100, 2004.
De Vos, B., Cools, N., Ilvesniemi, H., Vesterdal, L., Vanguelova, E., and
Carnicelli, S.: Benchmark values for forest soil carbon stocks in Europe:
Results from a large scale forest soil survey, Geoderma, 251/252, 33–46,
2015.
Doetterl, S., Six, J., Van Wesemael, B., and Van Oost, K.: Carbon cycling in
eroding landscapes: geomorphic controls on soil organic C pool composition
and C stabilization, Glob. Change Biol., 18, 2218–2232, 2012.
Doetterl, S., Berhe, A. A., Nadeu, E., Wang, Z., Sommer, M., and Fiener, P.:
Erosion, deposition and soil carbon: A review of process-level controls,
experimental tools and models to address C cycling in dynamic landscapes,
Earth-Sci. Rev., 154, 102–122, 2016.
Dominati, E., Patterson, M., and Mackay, A.: A framework for classifying and
quantifying the natural capital and ecosystem services of soils, Ecol.
Econ., 69, 1858–1868, 2010.
Dotterweich, M.: The history of soil erosion and fluvial deposits in small
catchments of central Europe: Deciphering the long-term interaction between
humans and the environment – A review, Geomorphology, 101, 192–208, 2008.
Dudal, R.: The sixth factor of soil formation, Euras. Soil Sci., 38, S60–S65, 2005.
Dürr, H. H., Meybeck, M., and Dürr, S. H.: Lithologic composition of the Earth's continental surfaces derived from a new digital map emphasizing riverine material transfer, Global Biogeochem. Cy., 19, GB4S10, https://doi.org/10.1029/2005GB002515, 2005.
DWD Climate Data Center (CDC): Historical daily station observations
(temperature, pressure, precipitation, sunshine duration, etc.) for Germany,
version v006, available at: https://opendata.dwd.de/climate_environment/...air_temperature/, 2018a.
DWD Climate Data Center (CDC): Historical hourly station observations of
precipitation for Germany, version v006, available at: https://opendata.dwd.de/climate_environment/...precipitation/, 2018b.
Egli, M., Wernli, M., Kneisel, C., and Haeberli, W.: Melting glaciers and
soil development in the proglacial area Morteratsch (Swiss Alps): I. Soil
type chronosequence, Arct. Antarct. Alp. Res., 38, 499–509,
2006.
Ellis, B. and Foth, H.: Soil fertility, CRC Press, Boca Raton, Florida, 290 pp.,
1996.
Fick, S. E. and Hijmans, R. J.: WorldClim 2: new 1-km spatial resolution
climate surfaces for global land areas, Int. J.
Climatol., 37, 4302–4315, 2017.
Finke, P. A.: Modeling the genesis of luvisols as a function of topographic
position in loess parent material, Quaternary Int., 265, 3–17,
2012.
Finke, P. A., Vanwalleghem, T., Opolot, E., Poesen, J., and Deckers, J.:
Estimating the effect of tree uprooting on variation of soil horizon depth
by confronting pedogenetic simulations to measurements in a Belgian loess
area, J. Geophys. Re.-Earth Sur., 118, 2124–2139, 2013.
Follain, S., Minasny, B., McBratney, A. B., and Walter, C.: Simulation of
soil thickness evolution in a complex agricultural landscape at fine spatial
and temporal scales, Geoderma, 133, 71–86, 2006.
Gabet, E. J., Reichman, O. J., and Seabloom, E. W.: The effects of
bioturbation on soil processes and sediment transport, Annu. Rev.
Earth Pl. Sc., 31, 249–273, 2003.
Gallaway, J. M., Martin, Y. E., and Johnson, E. A.: Sediment transport due
to tree root throw: integrating tree population dynamics, wildfire and
geomorphic response, Earth Surf. Proc. Land., 34, 1255–1269,
2009.
Gasch, C. K., Hengl, T., Gräler, B., Meyer, H., Magney, T. S., and
Brown, D. J.: Spatio-temporal interpolation of soil water, temperature, and
electrical conductivity in 3D + T: The Cook Agronomy Farm data set,
Spat. Stat.-Neth., 14, 70–90, 2015.
Gessler, P. E., Chadwick, O. A., Chamran, F., Althouse, L., and Holmes, K.:
Modeling Soil–Landscape and Ecosystem Properties Using Terrain Attributes,
Soil Sci. Soc. Am. J., 64, 2046–2056, 2000.
Greiner, L., Keller, A., Grêt-Regamey, A., and Papritz, A.: Soil
function assessment: review of methods for quantifying the contributions of
soils to ecosystem services, Land Use Policy, 69, 224–237, 2017.
Grunwald, S.: Multi-criteria characterization of recent digital soil mapping
and modeling approaches, Geoderma, 152, 195–207, 2009.
Guo, L. B. and Gifford, R. M.: Soil carbon stocks and land use change: a
meta analysis, Glob. Change Biol., 8, 345–360, 2002.
Harden, J. W.: Genetic interpretations of elemental and chemical differences
in a soil chronosequence, California, Geoderma, 43, 179–193, 1988.
Harden, J. W., Sharpe, J. M., Parton, W. J., Ojima, D. S., Fries, T. L.,
Huntington, T. G., and Dabney, S. M.: Dynamic replacement and loss of soil
carbon on eroding cropland, Global Biogeochem. Cy., 13, 885–901, 1999.
Hargreaves, G. H. and Samani, Z. A.: Reference crop evapotranspiration from
temperature, Appl. Eng. Agr., 1, 96–99, 1985.
Heuvelink, G. B. M. and Webster, R.: Modelling soil variation: past,
present, and future, Geoderma, 100, 269–301, 2001.
Holmgren, P.: Multiple flow direction algorithms for runoff modelling in
grid based elevation models: An empirical evaluation, Hydrol.
Process., 8, 327–334, 1994.
Hunter, N. M., Bates, P. D., Horritt, M. S., and Wilson, M. D.: Simple
spatially-distributed models for predicting flood inundation: A review,
Geomorphology, 90, 208–225, 2007.
IPCC: Climate Change and Land: an IPCC special report on climate change,
desertification, land degradation, sustainable land management, food
security, and greenhouse gas fluxes in terrestrial ecosystems, IPCC, 896 pp., 2019.
Jagercikova, M., Cornu, S., Bourlès, D., Evrard, O., Hatté, C., and
Balesdent, J.: Quantification of vertical solid matter transfers in soils
during pedogenesis by a multi-tracer approach, J. Soil.
Sediment., 17, 408–422, 2017.
Jenny, H.: Factors of soil formation: a system of quantitative pedology,
McGraw-Hill, New York, 320 pp., 1941.
Johnson, D. L. and Watson-Stegner, D.: Evolution model of pedogenesis, Soil
Sci., 143, 349–366, 1987.
Keesstra, S., Mol, G., De Leeuw, J., Okx, J., De Cleen, M., and Visser, S.:
Soil-related sustainable development goals: Four concepts to make land
degradation neutrality and restoration work, Land, 7, 133, 2018.
Keyvanshokouhi, S., Cornu, S., Samouelian, A., and Finke, P.: Evaluating
SoilGen2 as a tool for projecting soil evolution induced by global change,
Sci. Total Environ., 571, 110–123, 2016.
Kirkby, M. J.: A conceptual model for physical and chemical soil profile
evolution, Geoderma, 331, 121–130, 2018.
Kust, G., Andreeva, O., and Cowie, A.: Land Degradation Neutrality: Concept
development, practical applications and assessment, J. Environ.
Manage., 195, 16–24, 2017.
Lal, R.: Accelerated Soil erosion as a source of atmospheric CO2, Soil
Till. Res., 188, 35–40, 2019.
Leopold, M. and Völkel, J.: Colluvium: Definition, differentiation, and
possible suitability for reconstructing Holocene climate data, Quaternary
Int., 162/163, 133–140, 2007.
Liu, Z., Shao, M. A., and Wang, Y.: Effect of environmental factors on
regional soil organic carbon stocks across the Loess Plateau region, China,
Agr. Ecosyst. Environ., 142, 184–194, 2011.
Lugato, E., Smith, P., Borrelli, P., Panagos, P., Ballabio, C., Orgiazzi,
A., Fernandez-Ugalde, O., Montanarella, L., and Jones, A.: Soil erosion is
unlikely to drive a future carbon sink in Europe, Sci. Adv., 4,
eaau3523, https://doi.org/10.1126/sciadv.aau3523, 2018.
Marschmann, G. L., Pagel, H., Kügler, P., and Streck, T.: Equifinality,
sloppiness, and emergent structures of mechanistic soil biogeochemical
models, Environ. Model. Softw., 122, 104518, https://doi.org/10.1016/j.envsoft.2019.104518, 2019.
McBratney, A. B., Santos, M. M., and Minasny, B.: On digital soil mapping,
Geoderma, 117, 3–52, 2003.
Metzen, D., Sheridan, G. J., Benyon, R. G., Bolstad, P. V., Griebel, A., and
Lane, P. N. J.: Spatio-temporal transpiration patterns reflect vegetation
structure in complex upland terrain, Sci. Total Environ., 694,
133551, https://doi.org/10.1016/j.scitotenv.2019.07.357, 2019.
Minasny, B., McBratney, A. B., and Salvador-Blanes, S.: Quantitative models
for pedogenesis – A review, Geoderma, 144, 140–157, 2008.
Minasny, B., Finke, P. A., Stockmann, U., Vanwalleghem, T., and McBratney,
A. B.: Resolving the integral connection between pedogenesis and landscape
evolution, Earth-Sci. Rev., 150, 102–120, 2015.
Minasny, B., Malone, B. P., McBratney, A. B., Angers, D. A., Arrouays, D.,
Chambers, A., Chaplot, V., Chen, Z.-S., Cheng, K., Das, B. S., Field, D. J.,
Gimona, A., Hedley, C. B., Hong, S. Y., Mandal, B., Marchant, B. P., Martin,
M., McConkey, B. G., Mulder, V. L., O'Rourke, S., Richer-de-Forges, A. C.,
Odeh, I., Padarian, J., Paustian, K., Pan, G., Poggio, L., Savin, I.,
Stolbovoy, V., Stockmann, U., Sulaeman, Y., Tsui, C.-C., Vågen, T.-G.,
Van Wesemael, B., and Winowiecki, L.: Soil carbon 4 per mille, Geoderma,
292, 59–86, 2017.
Montagne, D., Cornu, S., Le Forestier, L., Hardy, M., Josière, O.,
Caner, L., and Cousin, I.: Impact of drainage on soil-forming mechanisms in
a French Albeluvisol: Input of mineralogical data in mass-balance modelling,
Geoderma, 145, 426–438, 2008.
Montanarella, L., Pennock, D. J., McKenzie, N., Badraoui, M., Chude, V., Baptista, I., Mamo, T., Yemefack, M., Singh Aulakh, M., Yagi, K., Young Hong, S., Vijarnsorn, P., Zhang, G.-L., Arrouays, D., Black, H., Krasilnikov, P., Sobocká, J., Alegre, J., Henriquez, C. R., de Lourdes Mendonça-Santos, M., Taboada, M., Espinosa-Victoria, D., AlShankiti, A., AlaviPanah, S. K., Elsheikh, E. A. E. M., Hempel, J., Camps Arbestain, M., Nachtergaele, F., and Vargas, R.: World's soils are under threat, SOIL, 2, 79–82, https://doi.org/10.5194/soil-2-79-2016, 2016.
Morbidelli, R., Saltalippi, C., Flammini, A., and Govindaraju, R. S.: Role
of slope on infiltration: a review, J. Hydrol., 557, 878–886,
2018.
Muhs, D. R.: Loess deposits, origins and properties, in: Encyclopedia of
Quaternary Science, 1405–1418, 2007.
Nearing, M. A., Pruski, F. F., and O'Neal, M. R.: Expected climate change
impacts on soil erosion rates: A review, J. Soil Water
Conserv., 59, 43–50, 2004.
Opolot, E., Yu, Y. Y., and Finke, P. A.: Modeling soil genesis at pedon and
landscape scales: Achievements and problems, Quaternary Int., 376,
34–46, 2015.
Pawlik, Ł. and Šamonil, P.: Soil creep: The driving factors, evidence
and significance for biogeomorphic and pedogenic domains and systems – A
critical literature review, Earth-Sci. Rev., 178, 257–278, 2018.
Pebesma, E. J.: Multivariable geostatistics in S: the gstat package,
Comput. Geosci., 30, 683–691, 2004.
Pécsi, M.: Loess is not just the accumulation of dust, Quaternary
Int., 7/8, 1–21, 1990.
Peukert, S., Griffith, B. A., Murray, P. J., Macleod, C. J. A., and Brazier,
R. E.: Spatial variation in soil properties and diffuse losses between and
within grassland fields with similar short-term management, Europ. J. Soil Sci., 67, 386–396, 2016.
Phillips, J. D.: The convenient fiction of steady-state soil thickness,
Geoderma, 156, 389–398, 2010.
Phillips, J. D., Gares, P. A., and Slattery, M. C.: Agricultural soil
redistribution and landscape complexity, Landscape Ecol., 14, 197–211,
1999.
Phillips, J. D., Šamonil, P., Pawlik, Ł., Trochta, J., and Daněk, P.: Domination of hillslope denudation by tree uprooting in an old-growth
forest, Geomorphology, 276, 27–36, 2017.
Pistocchi, A., Bouraoui, F., and Bittelli, M.: A simplified parameterization
of the monthly topsoil water budget, Water Resour. Res., 44, https://doi.org/10.1029/2007WR006603, 2008.
Poesen, J.: Challenges in gully erosion research, Landform Analysis, 17,
5–9, 2011.
Pongratz, J., Reick, C., Raddatz, T., and Claussen, M.: A reconstruction of
global agricultural areas and land cover for the last millennium, Global
Biogeochem. Cy., 22, https://doi.org/10.1029/2007GB003153, 2008.
Ramcharan, A., Hengl, T., Beaudette, D., and Wills, S.: A Soil Bulk Density
Pedotransfer Function Based on Machine Learning: A Case Study with the NCSS
Soil Characterization Database, Soil Sci. Soc. Am. J., 81,
1279–1287, 2017.
Regmi, N. R., McDonald, E. V., and Rasmussen, C.: Hillslope response under
variable microclimate, Earth Surf. Proc. Land., 44, 2615–2627, https://doi.org/10.1002/esp.4686, 2019.
Richter, D. d., Bacon, A. R., Brecheisen, Z., and Mobley, M. L.: Soil in the
Anthropocene, 25, 2015.
Roering, J. J., Almond, P., Tonkin, P., and McKean, J.: Soil transport
driven by biological processes over millennial time scales, Geology, 30,
1115–1118, 2002.
Román-Sánchez, A., Laguna, A., Reimann, T., Giraldez, J., Peña,
A., and Vanwalleghem, T.: Bioturbation and erosion rates along the
soil-hillslope conveyor belt, Part 2: quantification using an analytical
solution of the diffusion-advection equation, Earth Surf. Proc.
Land., 44, 2066–2080, https://doi.org/10.1002/esp.4626,2019.
Rozas, V.: Tree age estimates in Fagus sylvatica and Quercus robur: testing
previous and improved methods, Plant Ecol., 167, 193–212, 2003.
Saco, P. M., Willgoose, G. R., and Hancock, G. R.: Spatial organization of
soil depths using a landform evolution model, J. Geophys.
Res.-Earth, 111, F02016,
https://doi.org/10.1029/2005JF000351, 2006.
Šamonil, P., Daněk, P., Schaetzl, R., Vašíčková,
I., and Valtera, M.: Soil mixing and genesis as affected by tree uprooting
in three temperate forests, Europ. J. Soil Sci., 66, 589–603,
2015.
Šamonil, P., Daněk, P., Schaetzl, R. J., Tejnecký, V., and
Drábek, O.: Converse pathways of soil evolution caused by tree
uprooting: A synthesis from three regions with varying soil formation
processes, CATENA, 161, 122–136, 2018.
Sauer, D.: Pedological concepts to be considered in soil chronosequence
studies, Soil Res., 53, 577–591, 2015.
Schoorl, J. M., Veldkamp, A., and Bouma, J.: Modeling Water and Soil
Redistribution in a Dynamic Landscape Context, Soil Sci. Soc.
Am. J., 66, 1610–1619, 2002.
Schuur, E. A. G., McGuire, A. D., Schädel, C., Grosse, G., Harden, J.
W., Hayes, D. J., Hugelius, G., Koven, C. D., Kuhry, P., and Lawrence, D.
M.: Climate change and the permafrost carbon feedback, Nature, 520, 171–179,
2015.
Shepard, C., Schaap, M. G., Pelletier, J. D., and Rasmussen, C.: A probabilistic approach to quantifying soil physical properties via time-integrated energy and mass input, SOIL, 3, 67–82, https://doi.org/10.5194/soil-3-67-2017, 2017.
Shouse, M. and Phillips, J. D.: Soil deepening by trees and the effects of
parent material, Geomorphology, 269, 1–7, 2016.
Smetanová, A.: Bright patches on Chernozems and their relationship to
relief, Geografický Časopis, 61, 215–227, 2009.
Snowden, T. J., Van der Graaf, P. H., and Tindall, M. J.: Methods of Model
Reduction for Large-Scale Biological Systems: A Survey of Current Methods
and Trends, B. Math. Biol., 79, 1449–1486, 2017.
Sommer, M., Gerke, H. H., and Deumlich, D.: Modelling soil landscape genesis
– A “time split” approach for hummocky agricultural landscapes,
Geoderma, 145, 480–493, 2008.
Stockmann, U., Salvador-Blanes, S., Vanwalleghem, T., Minasny, B., and
McBratney, A. B.: One-, Two- and Three-Dimensional Pedogenetic Models, in:
Pedometrics, Edited by: McBratney, A. B., Minasny, B., and Stockmann, U.,
Springer International Publishing, Cham, 555–593, 2018.
Swanson, F. J. and Swanston, D. N.: Complex mass-movement terrains in the
western Cascade Range, Oregon, in: Reviews in Engineering Geology, edited
by: Coates, D. R., Geol. Soc. Am., 113–124, 1977.
Swift Jr., L. W.: Algorithm for solar radiation on mountain slopes, Water
Resour. Res., 12, 108–112, 1976.
Temme, A. J. A. M.: The Uncalm Development of Proglacial Soils in the
European Alps Since 1850, in: Geomorphology of Proglacial Systems: Landform
and Sediment Dynamics in Recently Deglaciated Alpine Landscapes,
Springer International Publishing, Cham, 315–326, 2019.
Temme, A. J. A. M. and Lange, K.: Pro-glacial soil variability and
geomorphic activity – the case of three Swiss valleys, Earth Surf.
Proc. Land., 39, 1492–1499, 2014.
Temme, A. J. A. M. and Vanwalleghem, T.: LORICA – A new model for linking
landscape and soil profile evolution: development and sensitivity analysis,
Comput. Geosci., 90, 131–143, 2016.
Temme, A. J. A. M., Claessens, L., Veldkamp, A., and Schoorl, J. M.:
Evaluating choices in multi-process landscape evolution models,
Geomorphology, 125, 271–281, 2011.
Temme, A. J. A. M., Armitage, J., Attal, M., Van Gorp, W., Coulthard, T. J.,
and Schoorl, J. M.: Developing, choosing and using landscape evolution
models to inform field-based landscape reconstruction studies, Earth Surf.
Proc. Land., 42, 2167–2183, 2017.
Thompson, S. E., Harman, C. J., Heine, P., and Katul, G. G.:
Vegetation-infiltration relationships across climatic and soil type
gradients, J. Geophys. Res.-Biogeo., 115, G02023,
https://doi.org/10.1029/2009JG001134, 2010.
Tranter, G., Minasny, B., McBratney, A. B., Murphy, B., McKenzie, N. J.,
Grundy, M., and Brough, D.: Building and testing conceptual and empirical
models for predicting soil bulk density, Soil Use Manage., 23,
437–443, 2007.
Tscharntke, T., Clough, Y., Wanger, T. C., Jackson, L., Motzke, I.,
Perfecto, I., Vandermeer, J., and Whitbread, A.: Global food security,
biodiversity conservation and the future of agricultural intensification,
Biol. Conserv., 151, 53–59, 2012.
Van der Meij, W. M., Temme, A. J. A. M., Wallinga, J., Hierold, W., and
Sommer, M.: Topography reconstruction of eroding landscapes – A case study
from a hummocky ground moraine (CarboZALF-D), Geomorphology, 295, 758–772,
2017.
Van der Meij, W. M., Temme, A. J. A. M., Lin, H. S., Gerke, H. H., and
Sommer, M.: On the role of hydrologic processes in soil and landscape
evolution modeling: concepts, complications and partial solutions,
Earth-Sci. Rev., 185, 1088–1106, 2018.
Van der Meij, W. M., Reimann, T., Vornehm, V. K., Temme, A. J. A. M.,
Wallinga, J., Van Beek, R., and Sommer, M.: Reconstructing rates and
patterns of colluvial soil redistribution in agrarian (hummocky) landscapes,
Earth Surf. Proc. Land., 44, 2408–2422, https://doi.org/10.1002/esp.4671, 2019.
Van Oost, K., Van Muysen, W., Govers, G., Deckers, J., and Quine, T. A.:
From water to tillage erosion dominated landform evolution, Geomorphology,
72, 193–203, 2005.
Van Oost, K., Quine, T. A., Govers, G., De Gryze, S., Six, J., Harden, J.
W., Ritchie, J. C., McCarty, G. W., Heckrath, G., and Kosmas, C.: The impact
of agricultural soil erosion on the global carbon cycle, Science, 318,
626–629, 2007.
Vanwalleghem, T., Poesen, J., McBratney, A., and Deckers, J.: Spatial
variability of soil horizon depth in natural loess-derived soils, Geoderma,
157, 37–45, 2010.
Vanwalleghem, T., Stockmann, U., Minasny, B., and McBratney, A. B.: A
quantitative model for integrating landscape evolution and soil formation,
J. Geophys. Res.-Earth, 118, 331–347, 2013.
Vanwalleghem, T., Gómez, J. A., Infante Amate, J., González de
Molina, M., Vanderlinden, K., Guzmán, G., Laguna, A., and Giráldez,
J. V.: Impact of historical land use and soil management change on soil
erosion and agricultural sustainability during the Anthropocene,
Anthropocene, 17, 13–29, 2017.
Vereecken, H., Schnepf, A., Hopmans, J., Javaux, M., Or, D., Roose, T.,
Vanderborght, J., Young, M., Amelung, W., and Aitkenhead, M.: Modeling soil
processes: Review, key challenges, and new perspectives, Vadose Zone
J., 15, 1–57, 2016.
Wang, Z., Hoffmann, T., Six, J., Kaplan, J. O., Govers, G., Doetterl, S.,
and Van Oost, K.: Human-induced erosion has offset one-third of carbon
emissions from land cover change, Nat. Clim. Change, 7, 345–349, 2017.
West, N., Kirby, E., Bierman, P., Slingerland, R., Ma, L., Rood, D., and
Brantley, S.: Regolith production and transport at the Susquehanna Shale
Hills Critical Zone Observatory, Part 2: insights from meteoric 10Be,
J. Geophys. Res.-Earth, 118, 1877–1896, 2013.
Wiesmeier, M., Spörlein, P., Geuß, U., Hangen, E., Haug, S.,
Reischl, A., Schilling, B., von Lützow, M., and Kögel-Knabner, I.:
Soil organic carbon stocks in southeast Germany (Bavaria) as affected by
land use, soil type and sampling depth, Glob. Change Biol., 18,
2233–2245, 2012.
Wilkinson, B. H.: Humans as geologic agents: A deep-time perspective,
Geology, 33, 161–164, 2005.
Willgoose, G.: Principles of Soilscape and Landscape Evolution, University
Press, Cambridge, 334 pp., 2018.
Wolff, E.: Entwurf zur Bodenanalyse, Z. Anal. Chem.,
3, 85–115, 1864.
Wösten, J. H. M., Pachepsky, Y. A., and Rawls, W. J.: Pedotransfer
functions: bridging the gap between available basic soil data and missing
soil hydraulic characteristics, J. Hydrol., 251, 123–150, 2001.
Yemefack, M., Rossiter, D. G., and Njomgang, R.: Multi-scale
characterization of soil variability within an agricultural landscape mosaic
system in southern Cameroon, Geoderma, 125, 117–143, 2005.
Yoo, K., Amundson, R., Heimsath, A. M., and Dietrich, W. E.: Spatial
patterns of soil organic carbon on hillslopes: Integrating geomorphic
processes and the biological C cycle, Geoderma, 130, 47–65, 2006.
Yoo, K., Ji, J., Aufdenkampe, A., and Klaminder, J.: Rates of soil mixing
and associated carbon fluxes in a forest versus tilled agricultural field:
Implications for modeling the soil carbon cycle, J. Geophys.
Res.-Biogeo., 116, G01014,
https://doi.org/10.1029/2010JG001304, 2011.
Zádorová, T. and Pení žek, V.: Formation, morphology and
classification of colluvial soils: a review, Europ. J. Soil
Sci., 69, 577–591, 2018.
Zhao, G., Mu, X., Wen, Z., Wang, F., and Gao, P.: Soil erosion,
conservation, and eco-environment changes in the loess plateau of China,
Land. Degrad. Dev., 24, 499–510, 2013.
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Short summary
We developed a model to simulate long-term development of soils and landscapes under varying rainfall and land-use conditions to quantify the temporal variation of soil patterns. In natural landscapes, rainfall amount was the dominant factor influencing soil variation, while for agricultural landscapes, landscape position became the dominant factor due to tillage erosion. Our model shows potential for simulating past and future developments of soils in various landscapes and climates.
We developed a model to simulate long-term development of soils and landscapes under varying...