1992
DOI: 10.1016/0167-6636(92)90014-5
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A constitutive model for inelastic flow and damage evolution in solids under triaxial compression

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Cited by 79 publications
(42 citation statements)
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“…Van Sambeek et al (1993) referred to the disturbed zone which forms upon mining as the initial DRZ and the subsequent disturbed zone which forms as a result of creep deformation and stress redistribution as the secondary D E . Both the magnitude and extent of damage in the Salado DRZ are time-dependent because the micromechanical deformation mechanism governing the dilatant inelastic deformation of the salt is a timedependent micro-fracturing mechanism (Chan et al, 1992). This mechanism is operable only under a limited range of stress states, specifically high stress difference relative to low mean stress.…”
Section: Description Of the Drzmentioning
confidence: 99%
“…Van Sambeek et al (1993) referred to the disturbed zone which forms upon mining as the initial DRZ and the subsequent disturbed zone which forms as a result of creep deformation and stress redistribution as the secondary D E . Both the magnitude and extent of damage in the Salado DRZ are time-dependent because the micromechanical deformation mechanism governing the dilatant inelastic deformation of the salt is a timedependent micro-fracturing mechanism (Chan et al, 1992). This mechanism is operable only under a limited range of stress states, specifically high stress difference relative to low mean stress.…”
Section: Description Of the Drzmentioning
confidence: 99%
“…While the MD model is relatively advanced in comparison to some creep models, it lacks other features that are important for more-advanced modeling of salt response. A descendant of the MD model that incorporates a few more advanced features is the Multi-mechanism Deformation Creep Fracture (MDCF) Model (Chan et al, 1992). At a minimum, this model needs to be incorporated into the code.…”
Section: Other Unique Featuresmentioning
confidence: 99%
“…See references for more detailed descriptions of each model. The three constitutive models reviewed are the multimechanism deformation coupled fracture model (Chan et al, 1992;Chan et al, 1994;Munson, 1993), representing the state of the art creep model developed through the mid-90s and used at SNL, the composite dilatancy model (Hampsel, 2007), and a rock salt model that describes transient, stationary, and accelerated creep and dilatancy (Salzer et al, 2006;Gunter and Salzer, 2007). The latter two models represent state of the art constitutive models developed in the last decade.…”
Section: B30 Constitutive Modelsmentioning
confidence: 99%
“…1 is the difference in principal stresses given by 101 -021, or the Tresca maximum shear stress criterion. The second term in the right-hand-side of Under normal conditions, the strong influence of the lithostatic pressure, expressed through the complicated second term on the right-hand-side of Eq.…”
Section: Conceptual Model Of Fracture and Spall Formationmentioning
confidence: 99%