Boussinesq’s problem of viscoelasticity

dc.contributor.authorWolf, Detlefde
dc.date.accessioned2010-02-08de
dc.date.accessioned2016-03-31T11:42:03Z
dc.date.available2010-02-08de
dc.date.available2016-03-31T11:42:03Z
dc.date.issued1991de
dc.description.abstractWe consider an isochemical, isentropic, incompressible fluid half-space and study quasistatic viscoelastic perturbations, induced by two-dimensional (2D) surface loads, of a hydrostatic initial state. In view of the regional or local scale required for deformations of planets to be amenable to the half-space approximation, the model is assumed to be externally gravitating. We derive analytic solutions for the displacement and incremental stress components and study several approximations to the expressions. Particular emphasis is placed on discriminating between the material and local incremental stresses. Based on this distinction, deeper insight is gained into the physical significance of the solution.en
dc.identifier.other321391306de
dc.identifier.urihttp://nbn-resolving.de/urn:nbn:de:bsz:93-opus-50912de
dc.identifier.urihttp://elib.uni-stuttgart.de/handle/11682/7153
dc.identifier.urihttp://dx.doi.org/10.18419/opus-7136
dc.language.isoende
dc.rightsinfo:eu-repo/semantics/openAccessde
dc.subject.classificationBoussinesq-Approximation , Viskoelastizitätde
dc.subject.ddc550de
dc.titleBoussinesq’s problem of viscoelasticityen
dc.typearticlede
ubs.fakultaetFakultätsübergreifend / Sonstige Einrichtungde
ubs.institutSonstige Einrichtungde
ubs.opusid5091de
ubs.publikation.sourceTerra Nova 3 (1991), S. 401-407. URL http://dx.doi.org./10.1111/j.1365-3121.1991.tb00169.xde
ubs.publikation.typZeitschriftenartikelde

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