Figure 3
From: The influence of δ-(Al,Fe)OOH on seismic heterogeneities in Earth’s lower mantle

The elastic wave velocities of the δ-Fe13 samples computed using the natural abundance of Fe: (a), vP, (b), vS, (c) vΦ. Elastic wave velocities of other end-membered hydrous phases: δ-AlOOH20,21,26, δ-(Al0.956Fe0.044)OOH (δ-Fe4)23, and ε-FeOOH with low spin state of Fe3+26 are also shown. PREM is shown by gray lines36. The values indicated by solid and open symbols were obtained from room temperature experiments and calculations at 0 K, respectively. Abrupt reductions of vP and vΦ for the δ-Fe13 samples at 32 GPa and 37.1 GPa are due to the spin transition of Fe3+22. The numerical values for the data of δ-Fe13 samples in this figure are available in Table S2.