| Titre de série : |
U.S Geological Survey Water-Supply Paper, 2349 |
| Titre : |
The significance of sediment transport in Arroyo development |
| Type de document : |
texte imprimé |
| Auteurs : |
Meyer, D.F. |
| Mention d'édition : |
United States Government Printing office |
| Editeur : |
United States Government Printing Office |
| Année de publication : |
1989 |
| ISBN/ISSN/EAN : |
CI-06668 |
| Note générale : |
Arroyo widening dominantes postineisional arroyo development, and the monner of widenig is dependent on the grain size of bed material transported by the channel. When bed material is predominantly gravel, subaqueous bars the alternate from one side of the channel to the other form during high flows in initially narrow, often straight, arroyos. These alternate bars grow and became coarse-grained point bars. Moderate and flows cannot rework these coarse bars, and the channel meanders around them-Arroyo walls opposite the bars are undercut and eroded. |
| Langues : |
Anglais (eng) |
| Mots-clés : |
Géologie Hydrologie Transport de sédiment Méthode d'analyse Relation expérimentale |
| Index. décimale : |
551.48 Hydrologie : |
| Résumé : |
Arroyo widening dominantes postineisional arroyo development, and the monner of widenig is dependent on the grain size of bed material transported by the channel. When bed material is predominantly gravel, subaqueous bars the alternate from one side of the channel to the other form during high flows in initially narrow, often straight, arroyos. These alternate bars grow and became coarse-grained point bars. Moderate and flows cannot rework these coarse bars, and the channel meanders around them-Arroyo walls opposite the bars are undercut and eroded. |
| Note de contenu : |
Arroyo widening dominantes postineisional arroyo development, and the monner of widenig is dependent on the grain size of bed material transported by the channel. When bed material is predominantly gravel, subaqueous bars the alternate from one side of the channel to the other form during high flows in initially narrow, often straight, arroyos. These alternate bars grow and became coarse-grained point bars. Moderate and flows cannot rework these coarse bars, and the channel meanders around them-Arroyo walls opposite the bars are undercut and eroded. |
U.S Geological Survey Water-Supply Paper, 2349. The significance of sediment transport in Arroyo development [texte imprimé] / Meyer, D.F. . - United States Government Printing office . - United States Government Printing Office, 1989. ISSN : CI-06668 Arroyo widening dominantes postineisional arroyo development, and the monner of widenig is dependent on the grain size of bed material transported by the channel. When bed material is predominantly gravel, subaqueous bars the alternate from one side of the channel to the other form during high flows in initially narrow, often straight, arroyos. These alternate bars grow and became coarse-grained point bars. Moderate and flows cannot rework these coarse bars, and the channel meanders around them-Arroyo walls opposite the bars are undercut and eroded. Langues : Anglais ( eng)
| Mots-clés : |
Géologie Hydrologie Transport de sédiment Méthode d'analyse Relation expérimentale |
| Index. décimale : |
551.48 Hydrologie : |
| Résumé : |
Arroyo widening dominantes postineisional arroyo development, and the monner of widenig is dependent on the grain size of bed material transported by the channel. When bed material is predominantly gravel, subaqueous bars the alternate from one side of the channel to the other form during high flows in initially narrow, often straight, arroyos. These alternate bars grow and became coarse-grained point bars. Moderate and flows cannot rework these coarse bars, and the channel meanders around them-Arroyo walls opposite the bars are undercut and eroded. |
| Note de contenu : |
Arroyo widening dominantes postineisional arroyo development, and the monner of widenig is dependent on the grain size of bed material transported by the channel. When bed material is predominantly gravel, subaqueous bars the alternate from one side of the channel to the other form during high flows in initially narrow, often straight, arroyos. These alternate bars grow and became coarse-grained point bars. Moderate and flows cannot rework these coarse bars, and the channel meanders around them-Arroyo walls opposite the bars are undercut and eroded. |
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