The volume equations of state for MgO and ε Fe determined under calibrated static pressure conditions to 1 Mbar are given by V/V0 = [1 + 2.85(3)P (Mbar)]−0.219(3) (for MgO) where V0 = 11.25(2) cm3/mol and V(cm3/mol) = 6.74(3)[1 + 3.4(3)P(Mbar)]−0.185(7) (for ε Fe). The random error of V is 0.3%, and the maximum systematic error of V (caused by the uncertainty of the pressure scale) is 1%. These equations can be employed in geophysical models of the mantle‐core boundary.
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Mao et al. (1979) studied this question.
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