Systematic approach to using isentropic stress reverberation techniques in approximating equation of state.

Rev Sci Instrum

Mechanical Engineering, University of Rhode Island, 92 Upper College Rd., Kingston, Rhode Island 02881, USA.

Published: March 2015

AI Article Synopsis

  • Isentropic stress reverberations allow researchers to extract multiple Hugoniot states from a single plate impact experiment by using a layered plate setup, with a low impedance inner layer within a high impedance bulk.
  • The technique relies on the Rankine-Hugoniot equations for impedance matching, requiring a known Hugoniot for the bulk material and considering various factors like wave velocities and layer thickness to influence the number of states obtained.
  • Experimental results using materials like 6061 aluminum and A572 grade 50 structural steel showed successful generation of six and ten Hugoniot states for polycarbonate respectively, while the method is confined to low to moderate stress regions where Hugoniot representations align closely with isentropic representations.

Article Abstract

Isentropic stress reverberations are used to obtain multiple Hugoniot states from a single plate impact experiment using a layered plate geometry, where a low impedance inner layer is embedded within a high impedance bulk structure. The mathematical framework used in this technique uses the classical Rankine-Hugoniot equations in the method of impedance matching, where the bulk material is required to have a known Hugoniot. Factors including the wave velocities in the materials, input pulse duration, inner layer thickness, and diameter of the test samples affect the number of states that can be generated from a single experiment. Experiments using 6061 aluminum and polycarbonate, respectively, as the bulk material and inner layer, accurately generated six Hugoniot states for the polycarbonate. Experiments using A572 grade 50 structural steel as the bulk material accurately generated ten Hugoniot states for the polycarbonate. For each experiment, the method can be used to generate a Hugoniot equation defining the material response of the inner layer within the domain encompassed by the specific test. The method is also confined to the low to moderate stress regions, within which Hugoniot and isentropic representations of the material are almost identical.

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http://dx.doi.org/10.1063/1.4914023DOI Listing

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