Geostatic Initialization (Multi Stage) |
Description |
Here are described the Keywords and their corresponding parameters for defining a multi stage Geostatic initialization of a problem. This is done in ParaGeo via the Geostatic_control_data structure. Geostatic control facilities: •Multi-step geostatic initialization where in each step specific assumptions can be applied, particularly related to the material and contact models. •Specification of additional initialization options; e.g. re-initialisation of displacement and state variables after establishing geostatic equilibrium.
Geostatic control may be used for cases where the initial geostatic state cannot be fully defined a-priori or when additional initialization options are required. For example, when discrete contact surfaces are present two situations can arise: •The displacement associated with establishing contact stress results in horizontal stresses that differ significantly from the target values, in which case an additional initialization step can be used to improve these values •Undesirable plastic deformation is observed adjacent to the contact surfaces during initialization. This can be ameliorated by performing the initial geostatic step using an elastic material assumption then performing an additional step where there is a gradual transition to nonlinear response. •Undesirable slip or de-bonding occurs on the contact surfaces. In this case setting the contact model as elastic in the first step and then performing a subsequent step with a gradual transition to slip assumptions may be beneficial.
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GEOSTATIC CONTROL Definition of geostatic control options |
Usage |
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Description |
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It is used to create Parageo Geostatic_control_data structure. This data structure facilitates: •Multi-step geostatic initialization where in each step specific assumptions can be applied, particularly related to the material and contact models. •Specification of additional initialization options; e.g. re-initialisation of displacement and state variables after establishing geostatic equilibrium.
Examples
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