Fig. 4 | Nature Communications

Fig. 4

From: Valence and spin states of iron are invisible in Earth’s lower mantle

Fig. 4

Variation of observable seismic properties of bridgmanite as a function of iron content at 80 GPa and 300 K. EoS results from this study and previous work summarized in ref. 19 demonstrate that a density b bulk modulus, and c bulk sound velocity exhibit different dependence on Fe2+ and Fe3+ content. The red solid lines are linear interpolations between MgSiO3-Bdg and end members for high-spin (HS) Fe3+-Bdg and the red dashed lines are those for B-site low-spin (LS) Fe3+ Bdg. The black lines are linear fits for Fe2+-Bdg summarized in ref.19. The Fe3+-Bdg end member is from this study, and the open and solid circles are for HS and B-site LS Fe3+ Bdg, respectively. Differences between21 (red triangles) and solid red line trend for bulk modulus and sound velocity may be caused by compositional changes during Bdg synthesis from glass in the laser heated diamond anvil cell. The purple symbols are for Fe3+, Al-bearing Bdg samples22,70, and the green symbols are for Fe3+, Fe2+-bearing Bdg samples with Fe3+/ΣFe <50%41

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