Soil erosion and sediment delivery in a mountain catchment under scenarios of land use change using a spatially distributed numerical model
Soil erosion and sediment yield are strongly affected by land use/land cover (LULC). Spatially distributed erosion models are of great interest to assess the expected effect of LULC changes on soil erosion and sediment yield. However, they can only be applied if spatially distributed data is availab...
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Format: | Article |
Language: | English |
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Copernicus Publications
2012-05-01
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Series: | Hydrology and Earth System Sciences |
Online Access: | http://www.hydrol-earth-syst-sci.net/16/1321/2012/hess-16-1321-2012.pdf |
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author | L. C. Alatorre S. Beguería N. Lana-Renault A. Navas J. M. García-Ruiz |
author_facet | L. C. Alatorre S. Beguería N. Lana-Renault A. Navas J. M. García-Ruiz |
author_sort | L. C. Alatorre |
collection | DOAJ |
description | Soil erosion and sediment yield are strongly affected by land use/land cover (LULC). Spatially distributed erosion models are of great interest to assess the expected effect of LULC changes on soil erosion and sediment yield. However, they can only be applied if spatially distributed data is available for their calibration. In this study the soil erosion and sediment delivery model WATEM/SEDEM was applied to a small (2.84 km<sup>2</sup>) experimental catchment in the Central Spanish Pyrenees. Model calibration was performed based on a dataset of soil redistribution rates derived from point <sup>137</sup>Cs inventories, allowing capture differences per land use in the main model parameters. Model calibration showed a good convergence to a global optimum in the parameter space, which was not possible to attain if only external (not spatially distributed) sediment yield data were available. Validation of the model results against seven years of recorded sediment yield at the catchment outlet was satisfactory. Two LULC scenarios were then modeled to reproduce land use at the beginning of the twentieth century and a hypothetic future scenario, and to compare the simulation results to the current LULC situation. The results show a reduction of about one order of magnitude in gross erosion (3180 to 350 Mg yr<sup>−1</sup>) and sediment delivery (11.2 to 1.2 Mg yr<sup>−1</sup> ha<sup>−1</sup>) during the last decades as a result of the abandonment of traditional land uses (mostly agriculture) and subsequent vegetation recolonization. The simulation also allowed assessing differences in the sediment sources and sinks within the catchment. |
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institution | Directory Open Access Journal |
issn | 1027-5606 1607-7938 |
language | English |
last_indexed | 2024-12-12T00:46:26Z |
publishDate | 2012-05-01 |
publisher | Copernicus Publications |
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series | Hydrology and Earth System Sciences |
spelling | doaj.art-a6569386d29843339a9ef1d117873bb22022-12-22T00:44:08ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382012-05-011651321133410.5194/hess-16-1321-2012Soil erosion and sediment delivery in a mountain catchment under scenarios of land use change using a spatially distributed numerical modelL. C. AlatorreS. BegueríaN. Lana-RenaultA. NavasJ. M. García-RuizSoil erosion and sediment yield are strongly affected by land use/land cover (LULC). Spatially distributed erosion models are of great interest to assess the expected effect of LULC changes on soil erosion and sediment yield. However, they can only be applied if spatially distributed data is available for their calibration. In this study the soil erosion and sediment delivery model WATEM/SEDEM was applied to a small (2.84 km<sup>2</sup>) experimental catchment in the Central Spanish Pyrenees. Model calibration was performed based on a dataset of soil redistribution rates derived from point <sup>137</sup>Cs inventories, allowing capture differences per land use in the main model parameters. Model calibration showed a good convergence to a global optimum in the parameter space, which was not possible to attain if only external (not spatially distributed) sediment yield data were available. Validation of the model results against seven years of recorded sediment yield at the catchment outlet was satisfactory. Two LULC scenarios were then modeled to reproduce land use at the beginning of the twentieth century and a hypothetic future scenario, and to compare the simulation results to the current LULC situation. The results show a reduction of about one order of magnitude in gross erosion (3180 to 350 Mg yr<sup>−1</sup>) and sediment delivery (11.2 to 1.2 Mg yr<sup>−1</sup> ha<sup>−1</sup>) during the last decades as a result of the abandonment of traditional land uses (mostly agriculture) and subsequent vegetation recolonization. The simulation also allowed assessing differences in the sediment sources and sinks within the catchment.http://www.hydrol-earth-syst-sci.net/16/1321/2012/hess-16-1321-2012.pdf |
spellingShingle | L. C. Alatorre S. Beguería N. Lana-Renault A. Navas J. M. García-Ruiz Soil erosion and sediment delivery in a mountain catchment under scenarios of land use change using a spatially distributed numerical model Hydrology and Earth System Sciences |
title | Soil erosion and sediment delivery in a mountain catchment under scenarios of land use change using a spatially distributed numerical model |
title_full | Soil erosion and sediment delivery in a mountain catchment under scenarios of land use change using a spatially distributed numerical model |
title_fullStr | Soil erosion and sediment delivery in a mountain catchment under scenarios of land use change using a spatially distributed numerical model |
title_full_unstemmed | Soil erosion and sediment delivery in a mountain catchment under scenarios of land use change using a spatially distributed numerical model |
title_short | Soil erosion and sediment delivery in a mountain catchment under scenarios of land use change using a spatially distributed numerical model |
title_sort | soil erosion and sediment delivery in a mountain catchment under scenarios of land use change using a spatially distributed numerical model |
url | http://www.hydrol-earth-syst-sci.net/16/1321/2012/hess-16-1321-2012.pdf |
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