NONUNIQUE DYNAMIC EQUILIBRIUM CONSTITUTIVE RELATION OF METAL-POWDER DEPENDING ON ITS MICROSTRUCTURE

Citation
Y. Sano et al., NONUNIQUE DYNAMIC EQUILIBRIUM CONSTITUTIVE RELATION OF METAL-POWDER DEPENDING ON ITS MICROSTRUCTURE, Journal of engineering materials and technology, 118(1), 1996, pp. 12-18
Citations number
20
Categorie Soggetti
Engineering, Mechanical","Material Science
ISSN journal
00944289
Volume
118
Issue
1
Year of publication
1996
Pages
12 - 18
Database
ISI
SICI code
0094-4289(1996)118:1<12:NDECRO>2.0.ZU;2-O
Abstract
If was observed in an earlier work by Morimoto et al. [Inst. Phys, Con f: Ser. No. 70, Oxford 1984, p. 427] that the dynamic compact of an al uminium powder medium had greater flakiness and contiguity ratio than the static compact of the same density. This observed difference in mi crostructure is used to explain their result that the dynamic pressure of the medium is higher than the static pressure for a given density: the degree of rotation of particles during compaction is assumed to d ecrease for higher strain rates because of the shorter time available, causing an increase in plastic particle deformation in the compaction direction, and increased resistance to the compaction. The normal Hug oniot equation derived, in which the mean strain rate averaged over a single steady wavefront is introduced indicates that a rise of the nor mal Hugoniot with an increase in the strain rare results macroscopical ly from the increase in the propagation velocity of the wavefront, The multiwave Hugoniot equation is found to depend on the strain rate his tory of a given material. in compactions of a metal powder medium by p unch impact, the wavefronts passing through the medium are approximate ly steady if the punch mass is sufficiently larger than the medium mas s. Bur both the number of wavefronts arising during the compaction and the amplitudes of the strain waves, and hence the strain rate histori es, vary with compaction conditions such as punch mass and initial pun ch velocity. This implies that a dynamic equilibrium constitutive rela tion for the medium will depend on the compaction conditions, and ther efore cannot be determined uniquely for any two compactions.