CaltechAUTHORS
  A Caltech Library Service

On the inversion of the density gradient at the fringe of the convection zone

Chitre, S. M. and Shaviv, G. (1967) On the inversion of the density gradient at the fringe of the convection zone. Proceedings of the National Academy of Sciences of the United States of America, 57 (3). pp. 573-579. ISSN 0027-8424. http://resolver.caltech.edu/CaltechAUTHORS:20120815-133043126

[img]
Preview
PDF - Published Version
See Usage Policy.

480Kb

Use this Persistent URL to link to this item: http://resolver.caltech.edu/CaltechAUTHORS:20120815-133043126

Abstract

Introduction. It is well known that the total pressure and the temperature increase as one goes inward from the surface to the center of a star. That the density, on the other hand, does not necessarily increase with depth below the surface was pointed out by Hoyle and Schwarzschild (1955) and was borne out quite clearly by the numerical integrations of the solar surface layers by Faulkner, Griffiths, and Hoyle (1963). The question was raised by Tayler and Gough (1963) as to whether the density gradient inversion was real or whether it was due to the particular model of convection adopted by Faulkner et al. It is the purpose of this note to show that the inversion is indeed genuine and results from the steep temperature gradient that exists in the outermost layers of the convection zone where convection is not fully efficient and carries only a fraction (<1/2) of the total energy flux. Also, the electron pressure-temperature plane can be divided into regions where dp/dT is negative and positive. The dividing line depends, in an insensitive manner, on the assumed model and efficiency of convection. In the case of the sun it is the hydrogen ionization at about 10^4 °K that causes the opacity to go up sharply and as a result the temperature gradient steepens there by inverting the density gradient. The inversion necessarily results in a Rayleigh-Taylor instability.


Item Type:Article
Related URLs:
URLURL TypeDescription
http://www.pnas.org/content/57/3.tocPublisherUNSPECIFIED
Additional Information:© 1967 National Academy of Sciences. Communicated by William A. Fowler, January 18, 1967. We wish to thank Professors William A. Fowler, F. Hoyle, and R. F. Christy for very illuminating discussions. Supported in part by the Office of Naval Research (Nonr-220(47)), and the National Science Foundation (GP-5391).
Funders:
Funding AgencyGrant Number
Office of Naval ResearchNonr-220(47))
NSFGP-5391
Record Number:CaltechAUTHORS:20120815-133043126
Persistent URL:http://resolver.caltech.edu/CaltechAUTHORS:20120815-133043126
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:33222
Collection:CaltechAUTHORS
Deposited By: Jason Perez
Deposited On:15 Aug 2012 23:19
Last Modified:14 Nov 2014 19:21

Repository Staff Only: item control page