Analytic model of principal Hugoniot at all pressures

Abstract

We present the analytic form of the principal Hugoniot at all pressures. It is constructed by interpolating smoothly between three pressure [Formula: see text] regimes. Specifically, (i) the low-[Formula: see text] regime in which the Hugoniot is described by [Formula: see text], where [Formula: see text] and [Formula: see text] are particle and shock velocities, respectively, the values of [Formula: see text] and [Formula: see text] come from the experiment, and a small non-linearity ([Formula: see text] s/km) is added to the otherwise common linear form [Formula: see text] to match the next regime; (ii) the intermediate-[Formula: see text] regime where the Hugoniot is described by the quantum-statistical model of Kalitkin and Kuzmina, [Formula: see text], with the values of [Formula: see text], [Formula: see text], and [Formula: see text] determined virtually for all [Formula: see text]s ([Formula: see text] being the atomic number); and (iii) the high-[Formula: see text] regime in which the Hugoniot is described by the Debye–Hückel model developed by Johnson. We determine the analytic form of the Hugoniot in the high-[Formula: see text] regime and match it with those in the other two regimes. We show that no additional free parameter is required for the construction of the Hugoniot at all [Formula: see text] except the six mentioned above: [Formula: see text], [Formula: see text], [Formula: see text], [Formula: see text], [Formula: see text], and [Formula: see text]. Comparison of the new model to experimental and/or theoretical data on aluminum, iron, silicon, and lithium fluoride, the four materials for which such data exist to very high [Formula: see text], demonstrates excellent agreement. Our approach applies to both elemental substances and complex materials (compounds and alloys) and can be used to predict the analytic forms of the yet unknown Hugoniots as well as to validate experimental results and theoretical calculations. The new model can be adopted for the description of the principal Hugoniots of porous substances and can be generalized for radiation-dominated (strong) shocks.