The investigation of RMI at an air/solid interface using Pagosa
ORAL
Abstract
Richtmyer-Meshkov instability (RMI) occurs when there has a baroclinic generation of vorticity resulting from the misalignment of density and pressure gradients on a density-stratified interface. Accelerated by the incident shock, the interface becomes unstable, fingers grow to form bubbles of light fluid, while spikes are formed in heavy fluid. RMI is a key problem in many fields, such as deflagration-to-detonation transition (DDT) as well as inertial confinement fusion (ICF) and supernovae explosions. Therefore, its research is of scientific and engineering significance. This work will investigate the Richtmyer-Meshkov instability at a solid/air interface using a hydrocode Pagosa. We first verify the ability of Pagosa to handle the Rayleigh-Taylor instability (RTI) and the RMI at an air/SF6 interface. Subsequently, we explore the RMI at a solid/air interface. The ultimate goal is to assess the effect of the initial perturbation (including the wavenumber, the amplitude etc) , the initial solid-gas ratio, the solid-material yield stress on the interface behavior.
*This work was supported by the U.S. Department of Energy through the Los Alamos National Laboratory. Los Alamos National Laboratory is operated by Triad National Security, LLC, for the National Nuclear Security Administration of U.S. Department of Energy (Contract No. 89233218CNA000001). The authors are grateful for the Advanced Simulation and Computing Program (ASC)'s support of this work.
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Publication: Computers & Mathematics with Applications
Presenters
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Xia Ma
- Los Alamos National Laboratory