http://www.cnr.it/ontology/cnr/individuo/prodotto/ID137625
Soil Erodibility Assessment for Applications at Watershed Scale. (Contributo in volume (capitolo o saggio))
- Type
- Label
- Soil Erodibility Assessment for Applications at Watershed Scale. (Contributo in volume (capitolo o saggio)) (literal)
- Anno
- 2009-01-01T00:00:00+01:00 (literal)
- Alternative label
BORSELLI L., CASSI P., SALVADOR SANCHIS P. (2009)
Soil Erodibility Assessment for Applications at Watershed Scale.
Springer, New York (Stati Uniti d'America) in Manual of methods for soil and land evaluation, 2009
(literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- BORSELLI L., CASSI P., SALVADOR SANCHIS P. (literal)
- Pagina inizio
- Pagina fine
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#citta
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#titoloVolume
- Manual of methods for soil and land evaluation (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#pagineTotali
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
- BORSELLI L., CASSI P., SALVADOR SANCHIS P. (CNR-IRPI- sede di Firenze) (literal)
- Titolo
- Soil Erodibility Assessment for Applications at Watershed Scale. (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#inCollana
- E.A.C. Costantini (Ed.). Manual of Methods for Soil and Land Evaluation, Science Publishers,U.S., ISBN 978-1-57808-571-2 , 600pp (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#isbn
- 978-1-57808-571-2 (literal)
- Abstract
- The term \"soil erodibility\" indicates the aptitude of a soil, based on its properties, to be eroded
by the following processes and exogenous agents: rainfall, runoff, mass movements and wind.
The concept of erodibility gained in importance during the last 50 years in the field of
soil erosion modelling and applications of soil conservation. However, erodibility is a concept
borrowed from geomorphological literature that was developed and adopted up to the
beginning of the 20th century.
In this context, the concept of erodibility was often used to give a qualitative assessment
of the effectiveness of various forms of erosion caused by exogenous agents such as water, ice
and wind (Davis, 1909). It was used mainly by geologists and geographers for a long time and
related to the processes most effective in the characterization of landform dynamics (Taylor
and Eggleton, 2001; Turkington et al., 2005). It is easy to associate varying rates of erodibility
to compactness of igneous and metamorphic rock masses compared to marls and clay shale,
deeply eroded by gullies. Indeed, the effectiveness of different processes and geomorphic
agents is directly linked to the characteristics of the bedrock in its state of weathering. (literal)
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