390
M. Gonzales and N. N. Thadhani
Fig. 13 The P-V Hugoniot for Ti/Al/B with the P-α prediction and Ballotechnic. The Wu-Jing
EOS approaches the Mie-Grüneisen porous Hugoniot. Many data points lie along the Ballotechnic,
hinting at a potential shock-induced chemical reaction
Fig. 14 The simulated stresses measured at each individual tracer point show a wide variability
in both arrival-time signature and stress level. Averaging the stresses naturally leads to the
observed characteristic “hump,” which was reproduced by simulations. This is captured due to
the inhomogeneous loading of the PVDF gage
M. Gonzales and N. N. Thadhani
Fig. 13 The P-V Hugoniot for Ti/Al/B with the P-α prediction and Ballotechnic. The Wu-Jing
EOS approaches the Mie-Grüneisen porous Hugoniot. Many data points lie along the Ballotechnic,
hinting at a potential shock-induced chemical reaction
Fig. 14 The simulated stresses measured at each individual tracer point show a wide variability
in both arrival-time signature and stress level. Averaging the stresses naturally leads to the
observed characteristic “hump,” which was reproduced by simulations. This is captured due to
the inhomogeneous loading of the PVDF gage