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Stabilized finite element methods fo...
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Stanford University.
Stabilized finite element methods for coupled flow and geomechanics.
紀錄類型:
書目-電子資源 : Monograph/item
正題名/作者:
Stabilized finite element methods for coupled flow and geomechanics.
作者:
White, Joshua A.
面頁冊數:
96 p.
附註:
Source: Dissertation Abstracts International, Volume: 70-10, Section: B, page: .
附註:
Adviser: Ronaldo I. Borja.
Contained By:
Dissertation Abstracts International70-10B.
標題:
Geotechnology.
電子資源:
http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=3382958
ISBN:
9781109450446
Stabilized finite element methods for coupled flow and geomechanics.
White, Joshua A.
Stabilized finite element methods for coupled flow and geomechanics.
- 96 p.
Source: Dissertation Abstracts International, Volume: 70-10, Section: B, page: .
Thesis (Ph.D.)--Stanford University, 2009.
In this work, we present a finite element formulation for variably-saturated porous geomaterials undergoing elastoplastic deformations. The deforming body is treated as a multiphase continuum, and the governing mass and momentum balance equations are solved in a fully- coupled manner. It is well-known, however, that mixed formulations of the type examined here may lead to unstable approximations unless the spaces chosen for the pressure and displacement interpolation satisfy stringent stability restrictions. Failure to choose a stable pair typically leads to spurious pressure oscillations and poor convergence behavior. Unfortunately, many seemingly natural combinations---including equal-order interpolation for all field variables---do not satisfy the necessary requirements. In this work, we propose a stabilized formulation, based on a minor modification of the variational equations, which allows one to circumvent these restrictions and employ equal-order mixed elements. Several numerical examples are used to demonstrate the computationally appealing features of this alternative formulation.
ISBN: 9781109450446Subjects--Topical Terms:
227307
Geotechnology.
Stabilized finite element methods for coupled flow and geomechanics.
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Stabilized finite element methods for coupled flow and geomechanics.
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Source: Dissertation Abstracts International, Volume: 70-10, Section: B, page: .
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Adviser: Ronaldo I. Borja.
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Thesis (Ph.D.)--Stanford University, 2009.
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In this work, we present a finite element formulation for variably-saturated porous geomaterials undergoing elastoplastic deformations. The deforming body is treated as a multiphase continuum, and the governing mass and momentum balance equations are solved in a fully- coupled manner. It is well-known, however, that mixed formulations of the type examined here may lead to unstable approximations unless the spaces chosen for the pressure and displacement interpolation satisfy stringent stability restrictions. Failure to choose a stable pair typically leads to spurious pressure oscillations and poor convergence behavior. Unfortunately, many seemingly natural combinations---including equal-order interpolation for all field variables---do not satisfy the necessary requirements. In this work, we propose a stabilized formulation, based on a minor modification of the variational equations, which allows one to circumvent these restrictions and employ equal-order mixed elements. Several numerical examples are used to demonstrate the computationally appealing features of this alternative formulation.
520
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The resulting implicit, nonlinear algebraic systems are then solved using an inexact Newton algorithm. We discuss methods for solving the linearized systems using memory-efficient iterative solvers, both on serial and parallel computing platforms. In order to deal with inherent ill-conditioning, we propose a block-structured, multilevel preconditioner that both accelerates the convergence of the Krylov solver and exhibits excellent scaling properties as the number of unknowns and number of processors increase.
520
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To demonstrate the effectiveness of these approaches, the analysis framework is applied to modeling hydrologically-driven slope failure. This analysis is motivated by a recent landslide that occurred at a steep experimental catchment (CB1) near Coos Bay, Oregon. Simulations are used to quantify the rainfall-induced slope deformation and assess the failure potential. Results of parametric studies suggest that for a steep hillside slope underlain by shallow bedrock similar to the CB1 site, failure would occur by a multiple slide block mechanism, with progressive failure surfaces forming at the bedrock interface and then propagating to the slope surface. A key observation is that significant computational resources are required to capture these complex solid/fluid interaction mechanisms at sufficient resolution, further justifying the use of the proposed approaches over conventional methods.
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