δ s at high pressure and dlnVs/dlnVp in the lower mantle

δ s , a measure of the sensitivity of the adiabatic bulk‐modulus to isobaric density changes, controls lateral variations of P‐wave velocities. To estimate the effect of pressure on δ s , we have performed lattice dynamic calculations of the cubic alkaline earth oxides. We used a many‐body parametric Hamiltonian that reproduces the available laboratory data on thermoelastic properties. The calculations were carried out for P‐T conditions that correspond to those of the lower mantle. We find that δ s decreases from 4±1 at standard conditions to ≤ 2 at lower mantle conditions. The latter value is consistent with D.L. Anderson's estimates based on geophysical data. With δ s ≤ 2, and a corresponding parameter for shear modulus not decreasing with compression, no partial melting is required to account for the observation that ΔlnV s /ΔlnV p ≥ 2 in the lower mantle. Although more data and calculations on additional minerals are needed to draw any firm conclusions, our results indicate that the relatively small lateral variations of lnV p , when compared to lnV s , are due entirely to compressional effects.