The effect of soil type, meteorological forcing and slope gradient on the simulation of internal erosion processes at the local scale.

作者: Guillaume Nord , Michel Esteves

DOI: 10.1002/HYP.7613

关键词:

摘要: Numerical simulation experiments of water erosion at the local scale (20 × 5 m) using a process-based model [Plot Soil Erosion Model_2D (PSEM_2D)] were carried out to test effects various environmental factors (soil type, meteorological forcing and slope gradient) on runoff response determine dominant processes that control sediment yield lengths. The selected corresponded conditions for which had been fully tested beforehand. use Green Ampt infiltration explained role played by rainfall intensity in response. Sediment outlet simulated area was correlated positively with gradient, but less sensitive soil type. relationship between loss per unit area) length greatly influenced all factors, there general tendency towards higher when longer. Contribution gross surfaces lengths ranging from 4 20 m. highest yields cases where flow activated. An increase gradient resulted detachment starting upstream. exported came predominantly zone located near outlet. microrelief helped development rill network controlled both ratio length. Copyright © 2010 John Wiley & Sons, Ltd.

参考文章(49)
杨明义, 薛亚洲, 刘普灵, 宋炜, Using REE Tracers to Measure Sheet Erosion Changing to Rill Erosion 中国稀土学报:英文版. ,vol. 21, pp. 587- 590 ,(2003)
Brian R. Zurbuchen, Vitaly A. Zlotnik, James J. Butler, Dynamic interpretation of slug tests in highly permeable aquifers Water Resources Research. ,vol. 38, pp. 7- 1 ,(2002) , 10.1029/2001WR000354
Olivier Cerdan, Jean Poesen, Gérard Govers, Nicolas Saby, Yves Le Bissonnais, Anne Gobin, Andrea Vacca, John Quinton, Karl Auerswald, Andreas Klik, Frantz FPM Kwaad, MJ Roxo, Bureau de Recherches Géologiques et Minières, Physical and Regional Geography Research Group, Sheet and Rill Erosion John Wiley & Sons, Ltd. pp. 501- 513 ,(2006) , 10.1002/0470859202.CH38
John Wainwright, Anthony J. Parsons, The effect of temporal variations in rainfall on scale dependency in runoff coefficients Water Resources Research. ,vol. 38, pp. 7- 1 ,(2002) , 10.1029/2000WR000188
BC Peter Heng, Graham C Sander, Cecil F Scott, None, Modeling overland flow and soil erosion on nonuniform hillslopes: a finite volume scheme. Water Resources Research. ,vol. 45, ,(2009) , 10.1029/2008WR007502
Peter B. Hairsine, Laurent Beuselinck, Graham C. Sander, Sediment transport through an area of net deposition Water Resources Research. ,vol. 38, pp. 22- 1 ,(2002) , 10.1029/2001WR000265
G. C. Sander, J.-Y. Parlange, D. A. Barry, M. B. Parlange, W. L. Hogarth, Limitation of the transport capacity approach in sediment transport modeling Water Resources Research. ,vol. 43, ,(2007) , 10.1029/2006WR005177
Guillaume Nord, Michel Esteves, PSEM_2D: A physically based model of erosion processes at the plot scale Water Resources Research. ,vol. 41, pp. 08407- ,(2005) , 10.1029/2004WR003690
K. Van Oost, G. Govers, O. Cerdan, D. Thauré, A. Van Rompaey, A. Steegen, J. Nachtergaele, I. Takken, J. Poesen, Spatially distributed data for erosion model calibration and validation: The Ganspoel and Kinderveld datasets Catena. ,vol. 61, pp. 105- 121 ,(2005) , 10.1016/J.CATENA.2005.03.001