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Communication dans un congrès
Impact of soils surface characteristics on gully erosion in Sahel : development of a modeling approach at different scales
Abstract : Water erosion is a natural processes particularly developed in semi-arid and arid regions, where soils can be really vulnerable. Erosion is thus the first step to desertification. In Sahelian region, concentrated overland flow often leads to the formation of gullies. Although this phenomenon is widespread in those regions, research efforts are still needed to be able to model their spatial distribution and the role of the different parameters involved in this process. In this context, the objectives of the Biocrust project are twofold. The first step is to investigate to what extent the role of Sahelian soil surface crusts (biological and/or physical) on soil surface infiltrability and detachment affect the formation and development of gullies. The second step is to integrate the results of these investigations in a simple geomorphological model to predict gully location at the catchment scale using satellite imagery to produce the land use as well as the soil surfa ce characteristic maps. Results from an evaluation of the methodology on two catchments show that the integration of soil crusting is a key parameter to insure the quality and relevance of gully prediction. The model is able to distinguish between two types of gullies, those whose width range between 0.5m and 4m and those whose width exceeds 4m. The application of the model at the regional scale is however limited by the resolution of available regional digital elevation model (i.e. the 90m resolution SRTM DEM) which only permits the prediction of large gullies.
https://hal-brgm.archives-ouvertes.fr/hal-00790410
Contributeur : Jean-François Desprats <>
Soumis le : mercredi 20 février 2013 - 11:00:00
Dernière modification le : mardi 15 juin 2021 - 14:56:05
Contributeur : Jean-François Desprats <>
Soumis le : mercredi 20 février 2013 - 11:00:00
Dernière modification le : mardi 15 juin 2021 - 14:56:05