Soil loss estimation using RUSLE model, GIS and remote sensing techniques: A case study from the Dembecha Watershed, Northwestern Ethiopia

被引:70
|
作者
Ostovari, Yaser [1 ]
Ghorbani-Dashtaki, Shoja [1 ]
Bahrami, Hossein-Ali [2 ]
Naderi, Mehdi [1 ]
Melo Dematte, Jose Alexandre [3 ]
机构
[1] Shahrekord Univ, Dept Soil Sci, Coll Agr, POX 115, Shahrekord, Iran
[2] Tarbiat Modares Univ, Dept Soil Sci, Coll Agr, Tehran, Iran
[3] Univ Sao Paulo, Dept Soil Sci, Luiz de Queiroz Coll Agr, Av Padua Dias 11, BR-13418260 Piracicaba, SP, Brazil
关键词
Erodibility; Erosivity; Landsat; 8; NDVI; Inceptisols; Entisols;
D O I
10.1016/j.geodrs.2017.06.003
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Soil loss is a major cause of land degradation worldwide, especially in large areas of arid and semi-arid regions. With advent of new software and technologies such as remote sensing (RS) and GIS, there is a necessity to integrate them to achieve important information in a faster manner. The aims of present study were to evaluate soil erodibility (K-factor) using standard plots under natural rainfall and prediction of soil loss by integrating RUSLE, GIS and RS in Fars Iran. The RUSLE factors were evaluated as following: the R-factor was calculated using modified Fournier index; K-factor was measured in the field using erosion plots and estimated by the USLE equation; the C-factor map was created using the NDVI; the LS-factor map was generated from digital elevation model with 10 m resolution, and the P-factor map was assumed as 1. Spatial distribution of annual soil loss in the Simakan watershed was obtained by multiplying these factors in GIS. The average of the measured K was 0.014 th MJ(-1) mm(-1) and 2.08 times less than the average of the estimated K (0.030 th MJ(-1) mm(-1)). The performance of RUSLE was highly influenced by the K, because the annual soil loss predicted using estimated K (11.0 th(-1) ya(-1)) was about twice as much as the measured K (5.7 th(-1) ya(-1)). The spatial distribution of soil loss classes predicted was: 73.64% very low, 14.79% low, 10.19% moderate and 1.25% severe. Areas of severe soil loss are situated in the northern portion of the study area, which needs suitable conservation practices.
引用
收藏
页码:28 / 36
页数:9
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