Visco-hypoplasticity and observational method for soft ground
Identifieur interne : 001763 ( Main/Exploration ); précédent : 001762; suivant : 001764Visco-hypoplasticity and observational method for soft ground
Auteurs : G. Gudehus [Allemagne]Source :
Descripteurs français
- Pascal (Inist)
English descriptors
- KwdEn :
Abstract
For soils with soft particles, in particular clays, a visco-hypoplastic relation is introduced by numerical element tests. With a single set of equations for effective stress rates depending on strain rates, the known behaviour is obtained for oedometric compression and creep, undrained and drained shearing. OCR = pe/p' with an equivalent pressure pc depending on e and stress ratio is decisive. Only five key parameters are needed and can easily be determined. The natural consolidation of a soft layer can thus be followed up, and its subsequent consolidation and creep under a fill, including spreading and localization. The method is also realistic for a braced excavation in soft clay. This enables an enhanced observational method
Affiliations:
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Le document en format XML
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<sourceDesc><biblStruct><analytic><title xml:lang="en" level="a">Visco-hypoplasticity and observational method for soft ground</title>
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<profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>constitutive equation</term>
<term>displacements</term>
<term>engineering supports</term>
<term>excavations</term>
<term>soft clays</term>
<term>soft soils</term>
</keywords>
<keywords scheme="Pascal" xml:lang="fr"><term>Sol mou</term>
<term>Equation constitutive</term>
<term>Déplacement</term>
<term>Excavation</term>
<term>Argile molle</term>
<term>Soutènement</term>
<term>Hypoplasticité</term>
<term>Remplissage barrage</term>
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<front><div type="abstract" xml:lang="en">For soils with soft particles, in particular clays, a visco-hypoplastic relation is introduced by numerical element tests. With a single set of equations for effective stress rates depending on strain rates, the known behaviour is obtained for oedometric compression and creep, undrained and drained shearing. OCR = p<sub>e</sub>
/p' with an equivalent pressure p<sub>c</sub>
depending on e and stress ratio is decisive. Only five key parameters are needed and can easily be determined. The natural consolidation of a soft layer can thus be followed up, and its subsequent consolidation and creep under a fill, including spreading and localization. The method is also realistic for a braced excavation in soft clay. This enables an enhanced observational method</div>
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<affiliations><list><country><li>Allemagne</li>
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