The use of models of mixture for analysis of shock-wave experiments with incomplete phase transformation

Abstract

It is suggested to use the known models of mixture for determining phase concentrations and temperature by the data of shock-wave experiments with incomplete phase transformation. Calculation results are given for the case of some known experiments involving graphite and C60 fullerite, and the dependence of the accuracy of calculation on the error of measurement is studied. The possibility is discussed of using the obtained degree of phase transformation in shock wave for constructing hydrodynamic models of kinetics of phase transitions at high pressures and temperatures, which adequately fit the experiment.