High velocity oblique impact experiments result in both compression and shear shock waves. Behind the shear shock wave the particle velocity is transverse to the shock front. At large transverse particle velocities , dislocation kinetics can contribute a portion of the velocity. Based on a kinematic and thermodynamic model of dislocation kinetics, an analysis is made of the transverse strain and velocity behind a shear shock. Kinematics of dislocations in transverse motion behind the shock is formulated. A solution is given for an ideal case where the disloca-tion density function propagates as a pulse behind the shear shock.
CITATION STYLE
Stout, R. B., & Anderson, G. D. (1986). Dislocation Kinetics Behind Shear Shocks. In Shock Waves in Condensed Matter (pp. 293–297). Springer US. https://doi.org/10.1007/978-1-4613-2207-8_38
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