Hostname: page-component-84b7d79bbc-fnpn6 Total loading time: 0 Render date: 2024-08-01T13:14:05.201Z Has data issue: false hasContentIssue false

Boundary shock waves

Published online by Cambridge University Press:  28 March 2006

E. Dale Martin
Affiliation:
Ames Research Center, NASA, Moffett Field, California

Abstract

The possible occurrence of a viscous region near a surface from which there is rapid efflux of gas, accompanied by large heat transfer, is postulated and investigated theoretically. Such a viscous region, denoted as a boundary shock wave, may occur in the case of a large high-speed meteor entering the earth's atmosphere, when a very high rate of vaporization induces translational non-equilibrium. The conditions across a boundary shock wave and its structure are calculated from the appropriate macroscopic equations reduced to closed-form expressions under the restrictions of a perfect gas, flowing at constant total enthalpy.

Type
Research Article
Copyright
© 1967 Cambridge University Press

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Allen, H. J. & James, N. A. 1964 NASA TN D-2069.
Friedrichs, K. O. 1955 Bull. Amer. Math. Soc. 61, 485504.
Hayes, W. D. 1960 Gasdynamic Discontinuities. Princeton Aeronautical Paperbacks, no. 3. Princeton University Press.
Liepmann, H. W., Narasimha, R. & Chahine, M. T. 1962 Phys. Fluids 5, 13131324.
Liepmann, H. W. & Roshko, A. 1957 Elements of Gasdynamics. New York: Wiley.
Lighthill, M. J. 1956 In Surveys in Mechanics (ed. by G. K. Batchelor & R. M. Davies), pp. 250351. Cambridge University Press.
Martin, E. D. 1966 NASA TN D-3195.
öpik, E. J. 1958 Physics of Meteor Flight in the Atmosphere. New York: Interscience.
Vincenti, W. G. & Kruger, C. H. 1965 Introduction to Physical Gasdynamics. New York: Wiley.