CSIRO Publishing Books Journals About Us Shopping Cart You are here: Journals > PASA   
PASA
  Publications of the Astronomical Society of Australia
 
Search
 
 
  Advanced Search
   

Journal Home
About the Journal
Editorial Board
Contacts
Content
Online Early
Current Issue
Just Accepted
All Issues
Special Issues
Sample Issue
Call for Proposals
For Authors
General Information
Instructions to Authors
Submit Article
Open Access
For Referees
General Information
Review Article
For Subscribers
Subscription Prices
Customer Service

 Early Alert
Subscribe to our email Early Alert or RSS feeds for the latest journal papers.

 Connect with us
facebook   youtube

Training

Publication Workshops


 

Article << Previous     |         Contents Vol 19(2)

Effects of Lower Boundary Conditions on the Stability of Radiative Shocks

Curtis J. Saxton

Publications of the Astronomical Society of Australia 19(2) 282 - 292

Abstract

Thermal instabilities can cause a radiative shock to oscillate, thereby modulating the emission from the post-shock region. The mode frequencies are approximately quantised in analogy to those of a vibrating pipe. The stability properties depend on the cooling processes, the electron–ion energy exchange, and the boundary conditions. This paper considers the effects of the lower boundary condition on the post-shock flow, both ideally and for some specific physical models. Specific cases include constant perturbed velocity, pressure, density, flow rate, or temperature at the lower boundary, and the situation with nonzero stationary flow velocity at the lower boundary. It is found that for cases with zero terminal stationary velocity, the stability properties are insensitive to the perturbed hydrodynamic variables at the lower boundary. The luminosity responses are generally dependent on the lower boundary condition.

Keywords: accretion — shock waves — binaries: close — white dwarfs



Full text doi:10.1071/AS02004

© CSIRO 2002

 
 PDF (249 KB)
 Export Citation
 Print
  
  
    


 
Top  Email this page
 
Legal & Privacy | Contact Us | Help

CSIRO

© CSIRO 1996-2012