Abstract
To assess the long-term safety of radioactive waste disposal systems, validation of predictive models is essential and large efforts should be given to barriers, particularly geologic barriers. This work appears in the form of four volumes, the subject of the first part is described below. Soils and rocks erosion depends upon climate, relief, lithology and human activities (deforesting). In the world, mechanical erosion is evaluated from 5 to 8 cm per 1000 years (mean denudation ratio). Rocks weathering solubilize chemical elements in the running water and rocks fracturation becomes more easily under erosion effects. Alteration front progress is 0.3-3 cm per 1000 years in temperate zones and 4-7 cm per 1000 years in tropical zones. 5 figs., 14 tabs., 80 refs.
Afzali, H;
Fourniguet, J;
Peaudecerf, P
[1]
- Bureau de Recherches Geologiques et Minieres (BRGM), 45 - Orleans (France)
Citation Formats
Afzali, H, Fourniguet, J, and Peaudecerf, P.
Development of modelling and forecasting in geology. (Volume 1). Evaluation of weathering and erosion velocity in different media; Geoprospective: developpement de la modelisation. Volume 1. Evaluation des vitesses d`alteration et d`erosion dans divers contextes.
France: N. p.,
1990.
Web.
Afzali, H, Fourniguet, J, & Peaudecerf, P.
Development of modelling and forecasting in geology. (Volume 1). Evaluation of weathering and erosion velocity in different media; Geoprospective: developpement de la modelisation. Volume 1. Evaluation des vitesses d`alteration et d`erosion dans divers contextes.
France.
Afzali, H, Fourniguet, J, and Peaudecerf, P.
1990.
"Development of modelling and forecasting in geology. (Volume 1). Evaluation of weathering and erosion velocity in different media; Geoprospective: developpement de la modelisation. Volume 1. Evaluation des vitesses d`alteration et d`erosion dans divers contextes."
France.
@misc{etde_10116522,
title = {Development of modelling and forecasting in geology. (Volume 1). Evaluation of weathering and erosion velocity in different media; Geoprospective: developpement de la modelisation. Volume 1. Evaluation des vitesses d`alteration et d`erosion dans divers contextes}
author = {Afzali, H, Fourniguet, J, and Peaudecerf, P}
abstractNote = {To assess the long-term safety of radioactive waste disposal systems, validation of predictive models is essential and large efforts should be given to barriers, particularly geologic barriers. This work appears in the form of four volumes, the subject of the first part is described below. Soils and rocks erosion depends upon climate, relief, lithology and human activities (deforesting). In the world, mechanical erosion is evaluated from 5 to 8 cm per 1000 years (mean denudation ratio). Rocks weathering solubilize chemical elements in the running water and rocks fracturation becomes more easily under erosion effects. Alteration front progress is 0.3-3 cm per 1000 years in temperate zones and 4-7 cm per 1000 years in tropical zones. 5 figs., 14 tabs., 80 refs.}
place = {France}
year = {1990}
month = {Dec}
}
title = {Development of modelling and forecasting in geology. (Volume 1). Evaluation of weathering and erosion velocity in different media; Geoprospective: developpement de la modelisation. Volume 1. Evaluation des vitesses d`alteration et d`erosion dans divers contextes}
author = {Afzali, H, Fourniguet, J, and Peaudecerf, P}
abstractNote = {To assess the long-term safety of radioactive waste disposal systems, validation of predictive models is essential and large efforts should be given to barriers, particularly geologic barriers. This work appears in the form of four volumes, the subject of the first part is described below. Soils and rocks erosion depends upon climate, relief, lithology and human activities (deforesting). In the world, mechanical erosion is evaluated from 5 to 8 cm per 1000 years (mean denudation ratio). Rocks weathering solubilize chemical elements in the running water and rocks fracturation becomes more easily under erosion effects. Alteration front progress is 0.3-3 cm per 1000 years in temperate zones and 4-7 cm per 1000 years in tropical zones. 5 figs., 14 tabs., 80 refs.}
place = {France}
year = {1990}
month = {Dec}
}