New European Slope Length and Steepness Factor (LS-Factor) for Modeling Soil Erosion by Water

被引:264
作者
Panagos, Panos [1 ]
Borrelli, Pasquale [1 ]
Meusburger, Katrin [2 ]
机构
[1] Inst Environm & Sustainabil, European Commiss Joint Res Ctr, Via Enrico Fermi 2749, I-21027 Ispra, Italy
[2] Univ Basel, Environm Geosci, CH-4056 Basel, Switzerland
关键词
soil erosion; Revised Universal Soil Loss Equation (RUSLE); LS-factor; System for Automated Geoscientific Analyses (SAGA); Digital Elevation Model (DEM); Europe;
D O I
10.3390/geosciences5020117
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The Universal Soil Loss Equation (USLE) model is the most frequently used model for soil erosion risk estimation. Among the six input layers, the combined slope length and slope angle (LS-factor) has the greatest influence on soil loss at the European scale. The S-factor measures the effect of slope steepness, and the L-factor defines the impact of slope length. The combined LS-factor describes the effect of topography on soil erosion. The European Soil Data Centre (ESDAC) developed a new pan-European high-resolution soil erosion assessment to achieve a better understanding of the spatial and temporal patterns of soil erosion in Europe. The LS-calculation was performed using the original equation proposed by Desmet and Govers (1996) and implemented using the System for Automated Geoscientific Analyses (SAGA), which incorporates a multiple flow algorithm and contributes to a precise estimation of flow accumulation. The LS-factor dataset was calculated using a high-resolution (25 m) Digital Elevation Model (DEM) for the whole European Union, resulting in an improved delineation of areas at risk of soil erosion as compared to lower-resolution datasets. This combined approach of using GIS software tools with high-resolution DEMs has been successfully applied in regional assessments in the past, and is now being applied for first time at the European scale.
引用
收藏
页码:117 / 126
页数:10
相关论文
共 35 条
[1]  
[Anonymous], 1997, PREDICTING SOIL EROS
[2]  
Baoyuan L., 2002, P 12 ISCO C SUSTAINA, V2, P21
[3]   Modeling soil erosion and river sediment yield for an intermountain drainage basin of the Central Apennines, Italy [J].
Borrelli, Pasquale ;
Maerker, Michael ;
Panagos, Panos ;
Schuett, Brigitta .
CATENA, 2014, 114 :45-58
[4]  
Bosco C, 2015, NAT HAZARD EARTH SYS, V15, P225, DOI 10.5194/nhess-15-225-2015
[5]   Modelling topographic potential for erosion and deposition using GIS - Comment [J].
Desmet, PJJ ;
Govers, G .
INTERNATIONAL JOURNAL OF GEOGRAPHICAL INFORMATION SCIENCE, 1997, 11 (06) :603-610
[6]  
Desmet PJJ, 1996, J SOIL WATER CONSERV, V51, P427
[7]  
FOSTER GR, 1974, T ASAE, V17, P305
[8]  
GRIFFIN ML, 1988, J SOIL WATER CONSERV, V43, P326
[9]  
Hickey R., 2000, CARTOGRAPHY, V29, P1, DOI [DOI 10.1080/00690805.2000.9714334, 10.1080/00690805.2000.9714334]
[10]   Slope length effects on soil loss for steep slopes [J].
Liu, BY ;
Nearing, MA ;
Shi, PJ ;
Jia, ZW .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 2000, 64 (05) :1759-1763