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Modeling Water and Soil Redistribution in a Dynamic Landscape Context

J. M. Schoorl*, A. Veldkamp and J. Bouma

Laboratory of Soil Science and Geology, Department of Environmental Sciences, Wageningen University, P.O. Box 37, 6700 AA Wageningen, The Netherlands



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Fig. 1. Study area in the lower Guadalhorce River basin with (a) DEM of the area with contour line interval 50 m, (b) major soil units according to parent material: river terraces (RI), gneiss (GN), molasse (MO), marls (MA), limestone (LM), phylites (PL), and serpentinite (SP), and (c) initial soil depth map.

 


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Fig. 2. Water redistribution with (a) run-off patterns of annual rainfall excess under Scenario A, (b) changes in run-off between Scenario A and B using multiple flow direction routing (MF) instead of steepest descent flow routing (SD), (c) detailed area indicated in (a) with SD, (d) detailed area with MF and (e) changes in run-off between Scenario B and C.

 


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Fig. 3. Annual soil redistribution in the landscape for Scenario D showing: (a) erosion and (b) sedimentation.

 


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Fig. 4. Changes in soil erosion patterns, shown with 5% decreasing or increasing threshold for (a) Scenario A to B, (b) Scenario B to C, (c) Scenario C to D and (d) total change from Scenario A to D.

 


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Fig. 5. Changes in sedimentation patterns, shown with 5% decreasing or increasing threshold for (a) Scenario A to B, (b) Scenario B to C, (c) Scenario C to D and (d) total change from Scenario A to D.

 


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Fig. 6. Changes in available water storage capacity for Scenario D compared with Scenario A.

 





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Copyright © 2002 by the Soil Science Society of America.