General properties of a multilayer stratified fluids system
Journal Article
·
· Physics of Fluids A; (United States)
- Department of Applied Mathematics and Statistics, State University of New York, Stony Brook, New York 11794 (United States)
Linearized Euler equations of a general stationary multiple layer stratified system for both compressible and incompressible inviscid fluids are analyzed. The main result is that many features of a multilayer system are universal, in the sense they do not depend on such details as the number of layers, their thicknesses, equations of state for the fluids, and equilibrium density distributions. Necessary and sufficient conditions of stability are determined. For compressible fluids, it is possible for the system to be unstable even if there is no density inversion anywhere. It is shown that a compressible system is always more unstable than the corresponding incompressible one. A universal upper bound for the growth rate for a given perturbation wave number is given. General Rayleigh--Taylor unstable modes are characterized, and the range of unstable wave numbers is determined. Properties of stable modes are discussed. Numerical algorithms for solving the eigenvalue problem of the set of linearized Euler equations are given.
- DOE Contract Number:
- FG02-90ER25084
- OSTI ID:
- 6943224
- Journal Information:
- Physics of Fluids A; (United States), Journal Name: Physics of Fluids A; (United States) Vol. 5:5; ISSN PFADEB; ISSN 0899-8213
- Country of Publication:
- United States
- Language:
- English
Similar Records
Multiple linear instability of layered stratified shear flow
Hydromagnetic Rayleigh--Taylor instability of a rotating stratified fluid
Streamwise vortices in heated boundary layers. Final Report
Journal Article
·
Fri Dec 31 23:00:00 EST 1993
· Journal of Fluid Mechanics
·
OSTI ID:85464
Hydromagnetic Rayleigh--Taylor instability of a rotating stratified fluid
Journal Article
·
Sat May 01 00:00:00 EDT 1982
· Phys. Fluids; (United States)
·
OSTI ID:5525328
Streamwise vortices in heated boundary layers. Final Report
Technical Report
·
Mon Jun 01 00:00:00 EDT 1992
·
OSTI ID:7252621