Abstract:
The nucleation and evolution of damage in annealed coarsely crystalline M1-type copper subjected to fast loading to a pressure $P\sim$ 32 GPa, followed by the action of tensile stresses $\sigma_p$ with an intensity of $\approx$ -2.0 GPa for a time $t\approx$ 0.3–1.5 $\mu$s, have been investigated numerically and experimentally. It has been shown that, at a specific combination of amplitude-time characteristics of the tensile stress pulse, damage localization in some cases at $t <$ 1 $\mu$s has been observed in zones ($\sim$10–14 mm in size) alternating with “dead” zones ($\sim$3–5 mm in size) containing no visible damages. Pores are connected by “yield streamlets”. The existing multistage models of fracture kinetics have neither explained nor predicted the formation of a “band” damage structure or the presence of “yield streamlets” in specimens.