Two-zone Hugoniot for porous materials

A. D. Resnyansky
Phys. Rev. B 93, 054103 – Published 1 February 2016

Abstract

By decoupling thermal equilibrium conditions in shock loaded porous materials, two regimes resulting in two-zone Hugoniot are revealed, specifically, a stable low-pressure regime characterized by achieving interphase temperature equilibrium and a metastable high-pressure regime. Porous materials, represented as two-phase mixtures, are analyzed with an analytically constructed Hugoniot employing a constant Grüneisen parameter of condensed phase. Results of the analysis agree well with experiments for various porous materials over a wide range of porosities, which confirms the consistency of this interpretation. The two-zone consideration discovers a limitation on the high-temperature states of solid materials accessible via the shock loading of porous materials and suggests that the two-phase nature of porous materials needs to be reflected in the use of Hugoniot data of powders when constructing equations of state for the corresponding condensed materials.

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  • Received 13 April 2015
  • Revised 3 November 2015

DOI:https://doi.org/10.1103/PhysRevB.93.054103

Published by the American Physical Society

Physics Subject Headings (PhySH)

Condensed Matter, Materials & Applied Physics

Authors & Affiliations

A. D. Resnyansky*

  • WCSD, Defence Science and Technology Organisation, P.O. Box 1500, Edinburgh SA 5111, Australia

  • *anatoly.resnyansky@dsto.defence.gov.au

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Issue

Vol. 93, Iss. 5 — 1 February 2016

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