Measurement of elastic velocities of MgO under shock compression to 500 kilobars
Author(s) -
Davies Geoffrey F.,
Ahrens Thomas J.
Publication year - 1973
Publication title -
journal of geophysical research
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/jb078i032p07596
Subject(s) - rarefaction (ecology) , shock (circulatory) , shock front , shock wave , mechanics , front (military) , compression (physics) , moving shock , physics , geology , thermodynamics , meteorology , medicine , paleontology , species richness
The velocities of rarefaction waves in shock‐compressed MgO have been measured by observing the reduction of the shock front velocity near the sample edges due to the rarefaction waves propagating from the edges. The extent of this ‘edge effect’ is difficult to determine accurately because of its emergent nature. Arrangements sensitive to differences in shock front velocity yielded rarefaction wave velocities close to predicted longitudinal velocities in the high‐pressure shock state. Velocities closer to the hydrodynamic sound speed in the shock state were obtained from less sensitive arrangements. These results can be interpreted in terms of a two‐stage elastoplastic model of the decompression. The longitudinal velocities measured in shock states up to 528 kb imply second pressure derivatives of the elastic moduli c ij ″, given by K 0 c ij ″ = −1 ± 15, where K is the bulk modulus.
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