Modeling soil and landscape evolution – the effect of rainfall and land-use change on soil and landscape patterns

<p>Humans have substantially altered soil and landscape patterns and properties due to agricultural use, with severe impacts on biodiversity, carbon sequestration and food security. These impacts are difficult to quantify, because we lack data on long-term changes in soils in natural and agric...

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Main Authors: W. M. van der Meij, A. J. A. M. Temme, J. Wallinga, M. Sommer
Format: Article
Language:English
Published: Copernicus Publications 2020-08-01
Series:SOIL
Online Access:https://soil.copernicus.org/articles/6/337/2020/soil-6-337-2020.pdf
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spelling doaj-c7505e9d76614204aa13b39d345c868a2020-11-25T02:55:12ZengCopernicus PublicationsSOIL2199-39712199-398X2020-08-01633735810.5194/soil-6-337-2020Modeling soil and landscape evolution – the effect of rainfall and land-use change on soil and landscape patternsW. M. van der Meij0W. M. van der Meij1A. J. A. M. Temme2A. J. A. M. Temme3J. Wallinga4M. Sommer5M. Sommer6Soil Geography and Landscape Group, Wageningen University and Research, P.O. Box 47, 6700 AA, Wageningen, the NetherlandsResearch Area Landscape Functioning, Working Group Landscape Pedology, Leibniz-Centre for Agricultural Landscape Research ZALF, Eberswalder Straße 84, 15374 Müncheberg, GermanyDepartment of Geography, Kansas State University, 920 N17th Street, Manhattan, KS 66506, USAInstitute of Arctic and Alpine Research, University of Colorado, Campus, P.O. Box 450, Boulder, CO 80309-0450, USASoil Geography and Landscape Group, Wageningen University and Research, P.O. Box 47, 6700 AA, Wageningen, the NetherlandsResearch Area Landscape Functioning, Working Group Landscape Pedology, Leibniz-Centre for Agricultural Landscape Research ZALF, Eberswalder Straße 84, 15374 Müncheberg, GermanyInstitute of Environmental Science & Geography, University of Potsdam, Karl-Liebknecht-Straße 24–25, 14476 Potsdam, Germany<p>Humans have substantially altered soil and landscape patterns and properties due to agricultural use, with severe impacts on biodiversity, carbon sequestration and food security. These impacts are difficult to quantify, because we lack data on long-term changes in soils in natural and agricultural settings and available simulation methods are not suitable for reliably predicting future development of soils under projected changes in climate and land management. To help overcome these challenges, we developed the HydroLorica soil–landscape evolution model that simulates soil development by explicitly modeling the spatial water balance as a driver of soil- and landscape-forming processes. We simulated 14&thinsp;500 years of soil formation under natural conditions for three scenarios of different rainfall inputs. For each scenario we added a 500-year period of intensive agricultural land use, where we introduced tillage erosion and changed vegetation type.</p> <p>Our results show substantial differences between natural soil patterns under different rainfall input. With higher rainfall, soil patterns become more heterogeneous due to increased tree throw and water erosion. Agricultural patterns differ substantially from the natural patterns, with higher variation of soil properties over larger distances and larger correlations with terrain position. In the natural system, rainfall is the dominant factor influencing soil variation, while for agricultural soil patterns landform explains most of the variation simulated. The cultivation of soils thus changed the dominant factors and processes influencing soil formation and thereby also increased predictability of soil patterns. Our study highlights the potential of soil–landscape evolution modeling for simulating past and future developments of soil and landscape patterns. Our results confirm that humans have become the dominant soil-forming factor in agricultural landscapes.</p>https://soil.copernicus.org/articles/6/337/2020/soil-6-337-2020.pdf
collection DOAJ
language English
format Article
sources DOAJ
author W. M. van der Meij
W. M. van der Meij
A. J. A. M. Temme
A. J. A. M. Temme
J. Wallinga
M. Sommer
M. Sommer
spellingShingle W. M. van der Meij
W. M. van der Meij
A. J. A. M. Temme
A. J. A. M. Temme
J. Wallinga
M. Sommer
M. Sommer
Modeling soil and landscape evolution – the effect of rainfall and land-use change on soil and landscape patterns
SOIL
author_facet W. M. van der Meij
W. M. van der Meij
A. J. A. M. Temme
A. J. A. M. Temme
J. Wallinga
M. Sommer
M. Sommer
author_sort W. M. van der Meij
title Modeling soil and landscape evolution – the effect of rainfall and land-use change on soil and landscape patterns
title_short Modeling soil and landscape evolution – the effect of rainfall and land-use change on soil and landscape patterns
title_full Modeling soil and landscape evolution – the effect of rainfall and land-use change on soil and landscape patterns
title_fullStr Modeling soil and landscape evolution – the effect of rainfall and land-use change on soil and landscape patterns
title_full_unstemmed Modeling soil and landscape evolution – the effect of rainfall and land-use change on soil and landscape patterns
title_sort modeling soil and landscape evolution – the effect of rainfall and land-use change on soil and landscape patterns
publisher Copernicus Publications
series SOIL
issn 2199-3971
2199-398X
publishDate 2020-08-01
description <p>Humans have substantially altered soil and landscape patterns and properties due to agricultural use, with severe impacts on biodiversity, carbon sequestration and food security. These impacts are difficult to quantify, because we lack data on long-term changes in soils in natural and agricultural settings and available simulation methods are not suitable for reliably predicting future development of soils under projected changes in climate and land management. To help overcome these challenges, we developed the HydroLorica soil–landscape evolution model that simulates soil development by explicitly modeling the spatial water balance as a driver of soil- and landscape-forming processes. We simulated 14&thinsp;500 years of soil formation under natural conditions for three scenarios of different rainfall inputs. For each scenario we added a 500-year period of intensive agricultural land use, where we introduced tillage erosion and changed vegetation type.</p> <p>Our results show substantial differences between natural soil patterns under different rainfall input. With higher rainfall, soil patterns become more heterogeneous due to increased tree throw and water erosion. Agricultural patterns differ substantially from the natural patterns, with higher variation of soil properties over larger distances and larger correlations with terrain position. In the natural system, rainfall is the dominant factor influencing soil variation, while for agricultural soil patterns landform explains most of the variation simulated. The cultivation of soils thus changed the dominant factors and processes influencing soil formation and thereby also increased predictability of soil patterns. Our study highlights the potential of soil–landscape evolution modeling for simulating past and future developments of soil and landscape patterns. Our results confirm that humans have become the dominant soil-forming factor in agricultural landscapes.</p>
url https://soil.copernicus.org/articles/6/337/2020/soil-6-337-2020.pdf
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