Thermal-induced cracks in explosive
crystals could hinder heat
conduction, generate hot spots, and ultimately induce detonation,
posing safety hazards for the storage and transportation of explosives
and impacting their performance. The thermotropic phase transition
occurring below decomposition and detonation temperature complicate
the evolution and mechanism of the cracks during heating for some
explosives. In this work, the generation and evolution of cracks induced
by the heating at both 180 and 185 °C above the phase transition
temperature were investigated for the classical energetic crystal
HMX. Three types of cracks, fast cracks, slow cracks, and small cracks, were observed
and the corresponding formation mechanisms and distribution characteristics
were systematically studied by optical microscopy, scanning electron
microscopy, 3D X-ray computed tomography, X-ray diffraction, and Raman
spectroscopy. The results indicate that fast cracks form due to thermal expansion, tending to be perpendicular to the
lattice b-direction. Slow cracks arise from the (101) (or (1̅10)) plane slipping and exist
only in the subsurface. Small cracks originate from
the β–δ phase transition of HMX, are denser and
more disordered, and mainly occur close to the heated surface. These
findings provide further insight into the relationship between thermal
damage and the heat conduction characteristics of HMX crystals.