A Study of Chaos and Mixing in Rayleigh-Taylor and Richtmyer-Meshkov Unstable Interfaces.

Abstract

Instabilities of fluid interfaces give rise to entrainment and to a chaotic mixing layer. This report has three purposes. The authors discuss the general features of such chaotic mixing layers, formulate a scientific program for their study and report on their recent progress in carrying out portions of this program. The Rayleigh-Taylor instability is driven by an inertial or gravitational force accelerating an interface between fluids of differing densities. Thus with the heavy fluid above the lighter fluid a flat (horizontal) interface in a gravitational field is in a position of unstable equilibrium. Small disturbances grow, producing bubbles of light fluid rising in the heavy fluid and spikes - or droplets of heavy fluid falling in the light fluid. The Richtmyer-Meshkov instability is produced by a shock wave hiring an interface (a contact discontinuity or material boundary) separating fluids of differing densities. Assuming a planar shock wave normally incident on an interface slightly perturbed from planar, the initial disturbances in the interface are again unstable, and grow with time.

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Document Details

Document Type
Technical Report
Publication Date
Apr 01, 1987
Accession Number
ADA184751

Entities

People

  • C. L. Gardner
  • J. Glimm
  • J. Grove
  • O. Mcbryan
  • R. Menikoff

Organizations

  • New York University

Tags

Communities of Interest

  • C4I
  • Energy and Power Technologies

DTIC Thesaurus Topics

  • Classification
  • Computational Fluid Dynamics
  • Computations
  • Equations
  • Equations Of State
  • Governments
  • Hypervelocity Flow
  • Law
  • Mathematics
  • New York
  • Numerical Analysis
  • Rayleigh Taylor Instability
  • Security
  • Shock Waves
  • Simulations
  • United States
  • United States Government

Readers

  • Atmospheric Science / Meteorology, specifically Wind Wave Turbulence.
  • Economics
  • Plasma Physics / Magnetohydrodynamics