The dynamic compression of natural uranium of normal and lower initial
density in the ranges of porosity of 1-4.8 and pressure of 20-200 GPa
is experimentally investigated. The method of barriers is used to reg
ister the run of four release isentropes for shock-compressed porous s
amples in a wide range of thermodynamic parameters-from the states on
shock adiabats under pressures from 70 to 350 GPa to near-critical sta
tes under pressures of several tens of MPa. The experimental data are
compared with the results of calculations performed by the wide-range
equation of state for uranium, including for the effects of high-tempe
rature melting and evaporation.