Abstract
Soil erosion by gullies in Ethiopia is causing environmental and socioeconomic problems. A sound soil and water management plan requires accurately predicted gully erosion hotspot areas. Hence, this study develops a gully erosion susceptibility map (GESM) using frequency ratio (FR) and random forest (RF) algorithms. A total of 56 gullies were surveyed, and their extents were derived by digitizing Google Earth imagery. Literature review and a multicollinearity test resulted in 14 environmental variables for the final analysis. Model prediction potential was evaluated using the area under the curve (AUC) method. Results showed that the best prediction accuracy using the FR and RF models was obtained by using the top four most important gully predictor factors: drainage density, elevation, land use, and groundwater table. The notion that the groundwater table is one of the most important gully predictor factors in Ethiopia is a novel and significant quantifiable finding and is critical to the design of effective watershed management plans. Results from separate variable importance analyses showed land cover for Nitisols and drainage density for Vertisols as leading factors determining gully locations. Factors such as texture, stream power index, convergence index, slope length, and plan and profile curvatures were found to have little significance for gully formation in the studied catchment.
Highlights
IntroductionErosion lowers the groundwater table [3] and increases the susceptibility of soils to drought, causing crop yield reduction [4]
Its altitude ranges from (Ethiopia) and covers a drainage area of km rainfall of 1480 mm, of which more than 90% falls between May and October
The multicollinearity test showed that the variance inflation factor (VIF) ranges from 1.04 to 7.8, while the TOL, which is the reciprocal of the VIF, varies from 0.13 to 0.96 (Table 3)
Summary
Erosion lowers the groundwater table [3] and increases the susceptibility of soils to drought, causing crop yield reduction [4]. Gullies increase landscape connectivity by providing efficient paths for the transport of water, sediment, and other materials from the source to the sink [5,6]. This affects flooding and reservoir siltation [7]. Soil erosion studies worldwide have shown that sediment in rivers mainly originates from gully erosion [8]. In Ethiopia, severe gully erosion has been a major
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