Soil dry aggregate stability and wind erodible fraction in a semiarid environment of Argentina
The size and stability of soil aggregates are primary factors that affect the soil susceptibility to wind erosion. Relationships among several soil properties and both the wind erodible fraction (EF) and the dry aggregate stability (DAS) can allow the development of simple mathematical models which...
| Autores principales: | , |
|---|---|
| Formato: | Artículo |
| Lenguaje: | Inglés |
| Publicado: |
2018
|
| Materias: | |
| Acceso en línea: | https://www.sciencedirect.com/science/article/pii/S0016706110002272 http://hdl.handle.net/20.500.12123/2164 https://doi.org/10.1016/j.geoderma.2010.07.016 |
Ejemplares similares: Soil dry aggregate stability and wind erodible fraction in a semiarid environment of Argentina
- Comparing adjacent cultivated and “virgin” soils in wind erosion affected environments can lead to errors in measuring soil degradation
- Effect of temporal resolution of wind data on wind erosion prediction with the Revised Wind Erosion Equation (RWEQ) = Efecto de la resolución temporal de los datos de viento en la predicción de la erosión eólica con el modelo RWEQ
- The impact of agriculture on soil texture due to wind erosion
- Relative soil water content as a factor for wind erodibility in soils with different texture and aggregation
- RWEQ wind erosion predictions for variable soil roughness conditions
- Selección de indicadores de sustentabilidad relacionados con la erosión eólica para la región semiárida central argentina (RSCA)