Do stones modify the spatial distribution of fire induced soil water repellency? Preliminary data

Water repellency is a property of many fire-affected soils that contributes to delayed wetting rates and shows many hydrological and geomorphological consequences. Fire-induced soil water repellency (SWR) may be modulated by pre-fire soil and vegetation properties. Many studies have been carried out...

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Detalles Bibliográficos
Autores: García Moreno, Jorge, Gordillo Rivero, Ángel J., Gil Torres, Juan, Jiménez Morillo, Nicasio T., Mataix Solera, Jorge, González Peñaloza, Félix Ángel, Pascual Granged, Arturo José, Bárcenas Moreno, G., Jiménez Pinilla, Patricia, Lozano Guardiola, Elena, Jordán López, Antonio, Martínez Zavala, Lorena María
Tipo de recurso: artículo
Estado:Versión publicada
Fecha de publicación:2013
País:España
Institución:Universidad de Sevilla (US)
Repositorio:idUS. Depósito de Investigación de la Universidad de Sevilla
OAI Identifier:oai:idus.us.es:11441/50626
Acceso en línea:http://hdl.handle.net/11441/50626
Access Level:acceso abierto
Palabra clave:Experimental burn Soil structure Subritical soil water repellency Surface stones
Experimental burn
Soil structure
Subritical soil
water repellency
Surface stones
Descripción
Sumario:Water repellency is a property of many fire-affected soils that contributes to delayed wetting rates and shows many hydrological and geomorphological consequences. Fire-induced soil water repellency (SWR) may be modulated by pre-fire soil and vegetation properties. Many studies have been carried out to investigate the relationship between SWR and these properties. But, to our knowledge, no studies have considered the effect of surface stones in the spatial distribution of fire-induced SWR. In this research, we study the occurrence and spatial and vertical distribution of SWR and its consequences on soil structure after experimental burning in a previously wettable soil under different stone covers (0, 15, 30, 45 and 60%). In our experiment, burning induced critical or subcritical SWR in the upper millimetres of previously wettable soil. Fire-induced SWR did not vary with stone cover, but critical SWR was reached in inter-stone soil areas. At stone-covered soil areas, SWR was increased, but WDPTs remained mostly below the 5 s threshold