Titre : |
Characteristics and problems of collapsible soils |
Type de document : |
texte imprimé |
Auteurs : |
Knodel, P. C. |
Mention d'édition : |
U.S. Department of the Interior |
Editeur : |
U.S. Department of the Interior |
Année de publication : |
1992 |
ISBN/ISSN/EAN : |
CI-08667 |
Note générale : |
In designing and construsting water ressources projects, the bureau of reclamation has encountered collapsing soil in several different parts of the united states. Collapsible soil are defined as any unsaturated soil that es thraugh a radiocal reanangement of particles and great decreape in volume upon wetting, additional loading, or both. Collapsible soils are found thraug haut the world in soil deposits, that are eolian, loessial, subaerial, mudflows, alluvial, residual, or are manmade fills . |
Langues : |
Anglais (eng) |
Mots-clés : |
Sol Typologie Pédologie Méthodologie Hydrocompaction |
Index. décimale : |
631.4 Pédologie, science et préservation des sols : chimie, physique, fertilité |
Résumé : |
In designing and construsting water ressources projects, the bureau of reclamation has encountered collapsing soil in several different parts of the united states. Collapsible soil are defined as any unsaturated soil that es thraugh a radiocal reanangement of particles and great decreape in volume upon wetting, additional loading, or both. Collapsible soils are found thraug haut the world in soil deposits, that are eolian, loessial, subaerial, mudflows, alluvial, residual, or are manmade fills . |
Note de contenu : |
In designing and construsting water ressources projects, the bureau of reclamation has encountered collapsing soil in several different parts of the united states. Collapsible soil are defined as any unsaturated soil that es thraugh a radiocal reanangement of particles and great decreape in volume upon wetting, additional loading, or both. Collapsible soils are found thraug haut the world in soil deposits, that are eolian, loessial, subaerial, mudflows, alluvial, residual, or are manmade fills . |
Characteristics and problems of collapsible soils [texte imprimé] / Knodel, P. C. . - U.S. Department of the Interior . - U.S. Department of the Interior, 1992. ISSN : CI-08667 In designing and construsting water ressources projects, the bureau of reclamation has encountered collapsing soil in several different parts of the united states. Collapsible soil are defined as any unsaturated soil that es thraugh a radiocal reanangement of particles and great decreape in volume upon wetting, additional loading, or both. Collapsible soils are found thraug haut the world in soil deposits, that are eolian, loessial, subaerial, mudflows, alluvial, residual, or are manmade fills . Langues : Anglais ( eng)
Mots-clés : |
Sol Typologie Pédologie Méthodologie Hydrocompaction |
Index. décimale : |
631.4 Pédologie, science et préservation des sols : chimie, physique, fertilité |
Résumé : |
In designing and construsting water ressources projects, the bureau of reclamation has encountered collapsing soil in several different parts of the united states. Collapsible soil are defined as any unsaturated soil that es thraugh a radiocal reanangement of particles and great decreape in volume upon wetting, additional loading, or both. Collapsible soils are found thraug haut the world in soil deposits, that are eolian, loessial, subaerial, mudflows, alluvial, residual, or are manmade fills . |
Note de contenu : |
In designing and construsting water ressources projects, the bureau of reclamation has encountered collapsing soil in several different parts of the united states. Collapsible soil are defined as any unsaturated soil that es thraugh a radiocal reanangement of particles and great decreape in volume upon wetting, additional loading, or both. Collapsible soils are found thraug haut the world in soil deposits, that are eolian, loessial, subaerial, mudflows, alluvial, residual, or are manmade fills . |
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