A simple thermodynamic model for calculating the high-pressure and high-temperature properties of MgO consistently is presented. The model explains experimental equation of state (EOS) to ∼220 GPa at room temperature and shock-wave EOS to ∼200 GPa very well. The calculated Hugoniot temperature amounts to 3400 K at 200 GPa. The input parameters are the volume of the unit cell, V 0, bulk modulus, K 0, its pressure derivative, K 0′, Debye temperature, Θ 0, and a parameter relating to the shear modulus, f 44, all in the static lattice at zero pressure which are estimated from experimental data at room temperature and zero pressure. The calculated thermal expansivity, α, and Anderson–Grüneisen parameters, δ T and δ S , at zero pressure are in agreement with experimental data to 1000–1250 K and those to 1800 K, respectively. Our model explains also experimental velocities v p and v s of compressional and shear waves to 1800 K at zero pressure very well. The pressure-dependence of α, v p and v s at room temperature agree reasonably with experimental data to 36 GPa at room temperature. Applying our model to magnesiowüstite, we have calculated the thermal EOS and shock-wave EOS in agreement with experimental data. The implication of our result together with our previous one of magnesium-silicate perovskite for the composition of the lower mantle is briefly discussed.
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