Spatial Estimation of Soil Erosion Risk by Land-cover Change in the Andes OF Southern Ecuador

被引:111
|
作者
Ochoa-Cueva, Pablo [1 ]
Fries, Andreas [2 ,3 ]
Montesinos, Pilar [4 ]
Rodriguez-Diaz, Juan A. [4 ]
Boll, Jan [5 ]
机构
[1] Univ Tecn Particular Loja, Dept Ciencias Agr & Alimentos, Loja 1101608, Ecuador
[2] Univ Tecn Particular Loja, Unidad Ingn Civil & Geol UCG, Loja 1101608, Ecuador
[3] Univ Marburg, Fac Geog FOG, LCRS, D-35032 Marburg, Germany
[4] Univ Cordoba, Dept Agron, E-14071 Cordoba, Spain
[5] Univ Idaho, Dept Biol & Agr Engn, Moscow, ID 83844 USA
关键词
soil erosion; RUSLE; land-cover change; future scenarios; C-factor; Ecuadorian Andes; VEGETATION COVER; ERODIBILITY; ECOSYSTEM; PRECIPITATION; VARIABILITY;
D O I
10.1002/ldr.2219
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Ecuador has the highest deforestation rate in South America, causing large-scale soil erosion. Inter-Andean watersheds are especially affected by a rapid increase of the population leading to the conversion of large areas of montane forest into pasture and cropland. In this study, we estimate soil erosion risk in a small mixed land-use watershed in the southern Andes of Ecuador. Soil loss was estimated at a spatial resolution of 30m, using the Revised Universal Soil Loss Equation (RUSLE) where the RUSLE factors were estimated on the basis of limited public available data. Land-cover maps for 1976, 2008 and 2040 were created assuming increasing deforestation rates over the ensuing decades. Greater erosion rates are estimated for succession areas with agricultural cropland and pasture with maximum values of 936Mgha(-1)y(-1), where slopes and precipitation amounts are the greatest. Under natural forest vegetation, the estimated soil erosion rates are negligible (15 to 40Mgha(-1)y(-1)) even at steep slopes and higher elevations where rainfall amounts and intensities are generally higher. When the entire watershed has undergone substantial deforestation in 2040, erosion values may reach 2,021Mgha(-1)y(-1). Vegetation cover is the most important factor for potential soil erosion. Secondary factors are related to rainfall (R-factor) and topography (LS factors). Although the spatial predictions of potential soil erosion have only limited meaning for erosion risk, this method provides an important screening tool for land management and assessment of land-cover change. Copyright (c) 2013 John Wiley & Sons, Ltd.
引用
收藏
页码:565 / 573
页数:9
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