Published January 1, 1978
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Journal Article
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The relation between the shock-induced free-surface velocity and the postshock specific volume of solids
- Creators
- Lyzenga, Gregory A.
- Ahrens, Thomas J.
Chicago
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Abstract
The release of solids from a state of shock compression at a free surface is examined. For isentropic release, the postshock specific volume V[prime]0 is shown to be constrained by V[prime]0? (Ufs–Up)2/P1+V1, where (P1,V1) is the pressure-volume Hugoniot state of shock compression and Ufs and Up are the free-surface and shock particle velocities, respectively. When a sudden phase change occurs during the release process, this lower bound is increased, subject to simplifying assumptions about the phase transition.
Additional Information
Copyright © 1978 American Institute of Physics. (Received 15 March 1977; accepted for publication 19 August 1977) [G.A.L. was] [s]upported by the Fannie and John Hertz Foundation and also the National Science Foundation Grant No. DES75-15006. Contribution No. 2858, Division of Geological and Planetary Sciences, California Institute of Technology.Files
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Additional details
- Eprint ID
- 11031
- Resolver ID
- CaltechAUTHORS:LYZjap78
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2008-06-23Created from EPrint's datestamp field
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