Abstract Title
Finite Element Modeling of Phase Transition in Zirconia Using MOOSE
Additional Funding Sources
The project described was supported by the National Science Foundation via the Research Experience for Undergraduates Site: Materials for Society at Boise State University (Award No. DMR 1658076).
Abstract
MOOSE (Multiphysics Object Oriented Simulation Environment) is a finite element framework software developed by the Idaho National Laboratory. Its open source and parallelization capabilities make it powerful and easily accessible to use for mesoscale computational modeling and upscaling to larger domains. MOOSE modules allow for easy implementation of various physics modeling conditions. We utilize MOOSE’s phase field module to model the tetragonal to monoclinic (t→m) phase transition in zirconia, a material known for its strength, fracture toughness, and low thermal conductivity. t→m transition is the mechanism underlying the zirconia self-healing against crack propagation. In this work we applied the time-dependent Ginzburg-Landau equations to evaluate the temporal and spatial evolution of t→m. Phase field modeling is an extremely powerful method in model mesoscale phenomenon and it has been shown to accurately model the t→m martensitic phase transformation in zirconia. A minimization technique is used to track all energies within a system, making it possible to calculate surface energies and increase stability of the system. We present preliminary results of using the phase field method to model the t→m transformation with MOOSE.
Finite Element Modeling of Phase Transition in Zirconia Using MOOSE
MOOSE (Multiphysics Object Oriented Simulation Environment) is a finite element framework software developed by the Idaho National Laboratory. Its open source and parallelization capabilities make it powerful and easily accessible to use for mesoscale computational modeling and upscaling to larger domains. MOOSE modules allow for easy implementation of various physics modeling conditions. We utilize MOOSE’s phase field module to model the tetragonal to monoclinic (t→m) phase transition in zirconia, a material known for its strength, fracture toughness, and low thermal conductivity. t→m transition is the mechanism underlying the zirconia self-healing against crack propagation. In this work we applied the time-dependent Ginzburg-Landau equations to evaluate the temporal and spatial evolution of t→m. Phase field modeling is an extremely powerful method in model mesoscale phenomenon and it has been shown to accurately model the t→m martensitic phase transformation in zirconia. A minimization technique is used to track all energies within a system, making it possible to calculate surface energies and increase stability of the system. We present preliminary results of using the phase field method to model the t→m transformation with MOOSE.
Comments
W75