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Coupled wellbore erosion and stability analysis

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dc.contributor.author Stavropoulou, M en
dc.contributor.author Papanastasiou, P en
dc.contributor.author Vardoulakis, I en
dc.date.accessioned 2014-03-01T01:13:39Z
dc.date.available 2014-03-01T01:13:39Z
dc.date.issued 1998 en
dc.identifier.issn 0363-9061 en
dc.identifier.uri https://dspace.lib.ntua.gr/xmlui/handle/123456789/12635
dc.subject wellbore stability en
dc.subject sand erosion en
dc.subject sand production en
dc.subject sand prediction en
dc.subject radial flow en
dc.subject poroelasticity en
dc.subject.classification Engineering, Geological en
dc.subject.classification Materials Science, Multidisciplinary en
dc.subject.classification Mechanics en
dc.subject.other Elasticity en
dc.subject.other Erosion en
dc.subject.other Finite element method en
dc.subject.other Galerkin methods en
dc.subject.other Mathematical models en
dc.subject.other Mechanical permeability en
dc.subject.other Porosity en
dc.subject.other Radial flow en
dc.subject.other Stabilization en
dc.subject.other Poroelasticity en
dc.subject.other Sand erosion en
dc.subject.other Sand prediction en
dc.subject.other Sand production en
dc.subject.other Wellbore stability en
dc.subject.other Sand en
dc.subject.other erosion en
dc.subject.other hydrocarbon technology en
dc.subject.other sand en
dc.title Coupled wellbore erosion and stability analysis en
heal.type journalArticle en
heal.identifier.primary 10.1002/(SICI)1096-9853(199809)22:9<749::AID-NAG944>3.0.CO;2-K en
heal.identifier.secondary http://dx.doi.org/10.1002/(SICI)1096-9853(199809)22:9<749::AID-NAG944>3.0.CO;2-K en
heal.language English en
heal.publicationDate 1998 en
heal.abstract This paper extends earlier work on sand erosion and presents an attempt to couple sand erosion to mechanical damage of rock around a wellbore. Porosity which evolves in time and space as surface erosion progresses, is chosen as the coupling parameter. Both rock elasticity and strength (cohesion) are assumed to depend on porosity in such a way that the material becomes weaker with increasing porosity. The mathematical model, consists of erosion equations, mixture flow equations and stress equilibrium equations, is solved numerically by Galerkin finite element method. Numerical results suggest that erosion, resulting in sand production, is high close to the free surface. Erosion is accompanied by changes in porosity and a significant permeability increase. Erosion in the vicinity of the wellbore induces alterations in the mechanical behaviour of the medium. Weakening of rock stiffness leads to severe alteration of both effective stresses and pore pressure near the cavity. Since cohesion decreases with increasing porosity, one can also identify the time instant at which rock mechanical failure starts.This paper extends earlier work on sand erosion and presents an attempt couple sand erosion to mechanical damage of rock around a wellbore. Porosity which evolves m time and space as surface erosion progresses, is chosen as the coupling parameter. Both rock elasticity and strength (cohesion) are assumed to depend on porosity in such a way that the material becomes weaker with increasing porosity. The mathematical model, consists of erosion equations, mixture flow equations and stress equilibrium equations, is solved numerically by Galerkin finite element method. Numerical results suggest that erosion, resulting in sand production, is high close to the free surface. Erosion is accompanied by changes in porosity and a significant permeability increase. Erosion in the vicinity of the wellbore induces alterations in the mechanical behaviour of the medium. Weakening of rock stiffness leads to severe alteration of both effective stresses and pore pressure near the cavity. Since cohesion decreases with increasing porosity, one can also identify the time instant at which rock mechanical failure starts. en
heal.publisher John Wiley & Sons Ltd, Chichester, United Kingdom en
heal.journalName International Journal for Numerical and Analytical Methods in Geomechanics en
dc.identifier.doi 10.1002/(SICI)1096-9853(199809)22:9<749::AID-NAG944>3.0.CO;2-K en
dc.identifier.isi ISI:000075888600003 en
dc.identifier.volume 22 en
dc.identifier.issue 9 en
dc.identifier.spage 749 en
dc.identifier.epage 769 en


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