Granular flow of comminuted ceramics governs the resistance for penetr
ation of ceramic armor under impact. To understand the mechanism of th
e granular flow, silicon carbide was subjected to high-strain, high-st
rain-rate deformation by radial symmetric collapse of a thick-walled c
ylinder by explosive. The deformation, under compressive stresses, was
carried out in two stages: the first stage prefractured the ceramic,
while a large deformation was accomplished in the second stage. The to
tal tangential strain (-0.23) was accommodated by both homogeneous def
ormation (-0.10) and shear localization (-0.13). Three microstructures
, produced by different processing methods, were investigated. The mic
rostructural differences affected the microcrack propagation: either i
ntergranular or transgranular fracture was observed, depending on the
processing conditions. Nevertheless, the spacing between shear bands a
nd the shear displacement within the shear bands were not significantl
y affected by the microstructure. Within the shear bands, the phenomen
on of comminution occurred, and the thickness of the shear bands incre
ased gradually with the shear strain. A bimodal distribution of fragme
nts developed inside the shear bands. The comminution proceeded throug
h the incorporation of fragments from the shear-band interfaces and th
e erosion of fragments inside the shear band. Outside the shear bands,
an additional comminution mechanism was identified: localized bending
generated comminution fronts, which transformed the fractured materia
l into the comminuted material. The observed features of high-strain-r
ate deformation of comminuted SiC can be used for validation of comput
er models for penetration process. (C) 1998 American Institute of Phys
ics.