1996
DOI: 10.1080/026937996137918
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Modelling topographic potential for erosion and deposition using GIS

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Cited by 142 publications
(206 citation statements)
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“…Direct measurement of slope gradient and slope length is feasible for small plots and parcels (Wischmeier and Smith 1978); however at the catchment scale the use of a Digital Elevation Model (DEM) is more suited (Mitasova et al 1996). DEMs of the three catchment sites were constructed by (1) digitizing all contours (20 m interval) from the official 1:50,000 maps of Claveria of the National Mapping and Resource Information Authority of the Philippines, and (2) interpolating a raster DEM from the digital contour data using spline interpolation.…”
Section: Study Areasmentioning
confidence: 99%
“…Direct measurement of slope gradient and slope length is feasible for small plots and parcels (Wischmeier and Smith 1978); however at the catchment scale the use of a Digital Elevation Model (DEM) is more suited (Mitasova et al 1996). DEMs of the three catchment sites were constructed by (1) digitizing all contours (20 m interval) from the official 1:50,000 maps of Claveria of the National Mapping and Resource Information Authority of the Philippines, and (2) interpolating a raster DEM from the digital contour data using spline interpolation.…”
Section: Study Areasmentioning
confidence: 99%
“…The ground slope data can be used to generate an erosion risk map of the bare soil areas (Nobrega et al 2006). By using Geographical Information Systems (GIS) techniques, a slope data can be produced accurately and quickly based on topographic maps and DEM (Mitasova et al 1996). Sazbo et al (1998) andBojie et al (1995) indicated that the GIS techniques can be successfully used to develop erosion risk maps based on DEM, slope, aspect, and land use data.…”
Section: Introductionmentioning
confidence: 98%
“…Huang and Cai (2007) conducted a study where GIS based stochastic model was developed to simulate land use change in Shiqian County, Southwestern China. In a more recent study, Zhijun et al (2009) RS technology and GIS techniques can be efficiently used to provide the spatial distributions of soil erosion, which is very important to determine the areas with high erosion risks and to prevent soil erosion incidents in such areas (Mitasova et al 1996). In this study, remotely sensed data and elevation data were used to extract and classify bare soil erosion risk areas for a study area selected from Hatila Valley Natural Protected Area in northeastern Turkey.…”
Section: Introductionmentioning
confidence: 99%
“…The spatial differences in the levels of soil erosion in Taita Hills by using mean annual rainfall to compute the rainfall intensities with intensity (Knijft et al, 1999) and a thresholds of 40mm and above was deemed erosive in the computation, soil erodibility (Harison et al, 2012); a combine of soil texture, available water content and gravel, study area population (KNBS 2010). The slope generated from DEM as detailed in (Morgan R.P.C, 1978& Mitasova et al, 1996 as the determinants used in the modeling. The slope factor was a combine of slope length and steepness; LS factor, (Mitasova et al, 1996) and the vegetation index derived from the NDVI and the land use for the study area.…”
Section: V) Soil Erosion Mappingmentioning
confidence: 99%
“…The slope generated from DEM as detailed in (Morgan R.P.C, 1978& Mitasova et al, 1996 as the determinants used in the modeling. The slope factor was a combine of slope length and steepness; LS factor, (Mitasova et al, 1996) and the vegetation index derived from the NDVI and the land use for the study area.…”
Section: V) Soil Erosion Mappingmentioning
confidence: 99%