2008
DOI: 10.1016/j.geomorph.2007.05.013
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A sapping erosion susceptibility model for the southern Cantabrian Range, North Spain

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Cited by 4 publications
(3 citation statements)
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“…Although models developed for gully erosion commonly deal with the estimation of erosion rates (Knisel, 1980;Merkel et al, 1988;Knisel, 1993;Flanagan and Nearing, 1995;Sidorchuk, 1999), only a few authors focused on gully erosion susceptibility (Meyers and Martínez-Casasnovas, 1999;Bou Kheir et al, 2007;Conoscenti et al, 2008;Fernández et al, 2008;Gómez Gutiérrez et al, 2009;Krishna Bahadur, 2009;Pike et al, 2009;Conforti et al, 2011). Conversely, it is possible to find many studies in literature for landslide susceptibility and hazard mapping.…”
Section: Introductionmentioning
confidence: 99%
“…Although models developed for gully erosion commonly deal with the estimation of erosion rates (Knisel, 1980;Merkel et al, 1988;Knisel, 1993;Flanagan and Nearing, 1995;Sidorchuk, 1999), only a few authors focused on gully erosion susceptibility (Meyers and Martínez-Casasnovas, 1999;Bou Kheir et al, 2007;Conoscenti et al, 2008;Fernández et al, 2008;Gómez Gutiérrez et al, 2009;Krishna Bahadur, 2009;Pike et al, 2009;Conforti et al, 2011). Conversely, it is possible to find many studies in literature for landslide susceptibility and hazard mapping.…”
Section: Introductionmentioning
confidence: 99%
“…The static CFs have been identified to trigger soil erosion and applied by many researchers in susceptibility studies. For instance, drainage density [8,[24][25][26], lineament density [8,27,28], LS-factor [9,[29][30][31][32][33], K-factor [34][35][36], and NDVI [25,28,37] were implemented in those studies. However, some dynamic CFs such as R-factor, LST and SMI are rarely considered despite their roles in the soil erosion process.…”
Section: Erosion Cfs In Susceptibility Assessmentmentioning
confidence: 99%
“…En estas regiones semiá-ridas la actividad de las cárcavas está limitada en el tiempo a la aparición de eventos de lluvia erosiva que ocurren unas pocas veces al año. En menor medida y de modo más reciente aparecen trabajos sobre el desarrollo y evolución de las cárcavas en zonas subhúmedas y húmedas peninsulares, como las que tienen lugar sobre las formaciones margosas y arenosas del flysch eoceno del Pirineo oscense (Nadal-Romero et al, 2008), sobre los regolitos de la Cordillera Cantábrica (Menéndez-Duarte et al, 2007), los conglomerados poco consolidados del sector septentrional de la Cuenca Terciaria del Duero (Fernández et al, 2008) o sobre las margas de la Depresión Terciaria del Penedés (Martínez-Casasnovas et al, 2003).…”
Section: Introductionunclassified