2012
DOI: 10.1007/s12517-012-0730-3
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Estimation of soil losses by USLE model using GIS at Mashhad plain, Northeast of Iran

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Cited by 55 publications
(36 citation statements)
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“…In terms of practicality, Desmet & Govers (1996) have reported studies of this method applied at a watershed scale with the disadvantages of it being time-consuming. Studies in Iran and the Philippines have implemented the R/USLE methods within a GIS environment by calculating the LS-factor for each raster cell in a DEM, essentially treating each pixel as its own segment of uniform slope (Bagherzadeh, 2014;Schmitt, 2009). …”
Section: Slope Length (L) and Steepness (S) Factormentioning
confidence: 99%
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“…In terms of practicality, Desmet & Govers (1996) have reported studies of this method applied at a watershed scale with the disadvantages of it being time-consuming. Studies in Iran and the Philippines have implemented the R/USLE methods within a GIS environment by calculating the LS-factor for each raster cell in a DEM, essentially treating each pixel as its own segment of uniform slope (Bagherzadeh, 2014;Schmitt, 2009). …”
Section: Slope Length (L) and Steepness (S) Factormentioning
confidence: 99%
“…The P-factor accounts for management practices that affect soil erosion through modifying the flow pattern, such as contouring, strip-cropping, or terracing (Renard et al, 1997). The more effective the conservation practice is at mitigating soil erosion, the lower the P-5 factor (Bagherzadeh, 2014). Like the C-factor, values for P-factors can be taken from literature and if there are no support practices observed, the P-factor is 1.0 (Adornado et al, 2009).…”
Section: Support Practice Factor (P)mentioning
confidence: 99%
“…"P i " is monthly average of rainfall for month i (mm) and "P" represents the annual average of rainfall (mm) (Bagherzadeh 2012;Demirci & Karaburun 2011;Pradhan et al 2012).…”
Section: Preparation Of Usle Layersmentioning
confidence: 99%
“…Recently, due to population and industrial growth, massive development in hilly areas can be observed especially in Penang Island and Kuala Lumpur city . Therefore, many hilly areas are under heavy pressure from agricultural and urban development (Akgun et al 2011;2012;Pradhan 2010b;2012;Pradhan et al 2012).…”
Section: Introductionmentioning
confidence: 99%
“…One of the most important characteristics of precipitation in arid and semi-arid regions as the case of the study area is thunderstorm which causes huge runoff in a short time which resulted in massive amount of soil losses. In an investigation by Bagherzadeh (2014) for estimating soil losses in Mashhad-Chenaran Plain, the values of soil losses varied between 0 and 0.25 t ha -1 yr -1 alongside the kashaf-rud river in the middle of the plain and 2-10 t ha -1 yr -1 at the edges of the plain. Conventional down-slope cultivation on 1-2% slopes of silty loam soils accelerated the erosion process and adversely influenced soil structure (Kurothe et al, 2014).…”
Section: Introductionmentioning
confidence: 99%