“…The EoS are derived from the standard decomposition of the Helmholtz free energy of a crystal, F ( V , T ) = F c ( V ) + F i o n ( V , T ) into a static lattice energy, or cold curve, F c ( V ), that depends only on specific volume, and the thermal ionic contribution, F ion ( V , T ), that depends on the set of vibrational normal modes of the crystal . Whereas the Rose–Vinet function was used to represent the cold curve in our earlier EoS for RDX, HMX, and PETN, − in this study we have used the MACAW reference curve of Lozano and Aslam. , One motivation for the development of the MACAW reference curve was to eliminate regions with negative bulk moduli when the material is put into tension, V > V 0 , where V 0 is the equilibrium volume of the crystal. While real materials cannot support large tensile stresses, the presence of regions of negative bulk modulus in expansion, which may occur in the popular Burch–Murnaghan or Rose–Vinet forms, leads to severe numerical instabilities in hydrocodes and finite element simulations that are circumvented by the use of the MACAW form .…”