Abstract

Experimental and theoretical studies on granular porous hexanitrostilbene (HNS) explosive have yielded an increased understanding of microstructural processes occurring during initiation by shock loading. Experiments give time-resolved pressure, hence chemical decomposition history at the impact interface following planar impact of HNS specimens onto fused-sil ica targets. The data are interpreted in terms of a quantitative two-temperature model which considers hot spots to be formed at pore sites as a result of the irreversible work accompanying the shock. Subsequently, decomposition completion is achieved by burn fronts which propagate radially out from each hot spot at a velocity which can be inferred from the bulk decomposition rate. Analysis of the data in the context of the model leads to several observations: 1) The delay times corresponding to hot-spot decomposition are shorter than expected, based on extrapolated low-temperature kinetics. 2) Contrary to interpretation of data on other explosives, the velocity of the burn front which propagates radially from each hot spot does not have a strong dependence upon the prevail ing pressure but is more nearly constant. 3) The inferred burn velocity has a very strong dependence upon the initial shock pressure. Introduction It is generally accepted that the passage of a shock wave through a granular porous explosive leads to Presented at the 8th ICOGER, Minsk, USSR, Aug. 23-26, 1981. Copyright © 1982 by the U.S. Dept. of Energy. Published by the American Institute of Aeronautics and Astronautics, Inc., with permission. Manager, Fluid and Thermal Science Department.

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