Aeolian sediment mass fluxes on a sandy soil in Central Patagonia

• Autores: Sterk, Geert; Parigiani, Jacopo; Cittadini, Eduardo Daniel; Peters, Piet; Scholberg, Johannes; Peri, Pablo Luis
• Año de publicación: 2012
• Idioma: inglés
• Tipo de recurso: artículo
• Fuente: Catena 95: 112-123. (August 2012)
• Materia: Soil; Wind Erosion; Windbreaks; Semiarid Zones; Degradation; Suelo; Erosión de Suelo; Cortavientos; Zonas Semiáridas; Degradación; Chubut (Argentina); Eolian Dust; Sediment Transport Equation; Polvo Eólico; Ecuación de Transporte de Sedimentos; Región Patagónica
• Institución: Instituto Nacional de Tecnología Agropecuaria

The climate of Patagonia is semi-arid and characterised by frequent strong winds. Wind erosion is potentially a serious soil degradation process that impacts long-term sustainability of local agricultural systems, but the conditions and the rates of wind erosion in this region have not been studied extensively. The aim of this study was to quantify windblown mass transport on a sandy soil in Central Patagonia. Aeolian mass fluxes were measured in the valley of Sarmiento (Chubut province, Argentina) using two saltiphones and 24 Modified Wilson and Cooke (MWAC) sediment catchers. The latter were installed along three transects: (1) a control on a bare strip of land cleared of its natural vegetation, to measure the maximum wind erosion; (2) a similar transect protected by an artificial windbreak with an optical porosity of 50%; and (3) a transect in a cherry orchard protected with the same type of windbreak. Nine windstorms were recorded throughout the experimental period. Storms with wind speed peaks of 20 m s−1 caused a total soil loss of 248 Mg ha− 1 in the control strip and heavily depleted the soil of its erodible fraction. The artificial windbreak reduced the soil loss by 51.0% on average, while no erosion was recorded in the cherry orchard. Measured maximum mass transport values were used to fit five sediment transport equations in order to select the best equation to integrate into a GIS-based wind erosion prediction system. The Kawamura (1964) equation showed the highest model efficiency and was considered to be the best sediment transport equation for the Patagonia conditions. It expresses total mass transport as a function of two empirical constants: the threshold friction velocity (u*t), and an erodibility coefficient CKa. It is concluded that wind erosion in Central Patagonia poses a serious risk of soil degradation once the natural vegetation is removed due to overgrazing or other anthropogenic activities.
EEA Santa Cruz
Fil: Sterk, Geert. Utrecht University. Department of Physical Geography; Países Bajos
Fil: Parigiani, Jacopo. Green Resources; Tanzania.
Fil: Cittadini, Eduardo Daniel. Instituto Nacional de Tecnología Agropecuaria (INTA). Estación Experimental Agropecuaria Chubut; Argentina.
Fil: Peters, Piet. Wageningen University. Land Degradation & Development group; Países Bajos
Fil: Scholberg, Johannes. Wageningen University. Biological Farming Systems; Países Bajos
Fil: Peri, Pablo Luis. Instituto Nacional de Tecnología Agropecuaria (INTA). Estación Experimental Agropecuaria Santa Cruz; Argentina.
Fil: Peri, Pablo Luis. Universidad Nacional de la Patagonia Austral; Argentina.
Fil: Peri, Pablo Luis. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina.