“…This is due to the fact that the silicate melt structure undergoes radical atomic arrangement from four‐ to six‐fold Si‐O coordination (SI, Figure S6a): While the nearest neighbor O‐H distance represented by the principal peak position in g HO ( r ) (SI, Figure S6b) remains at virtually the same distance, the second neighbor O‐H distances are shifted to considerably lower r with increasing P , reflected in the decrease of with P . By contrast, the average interatomic distance between Fe and H in the metallic melts remains constant over the same P ‐range (SI, Figure S6d), similar to the results reported in a previous DFT‐MD study (Posner & Steinle‐Neumann, 2019). At higher P , differences are Δ r V/ = −16% (40 GPa, 4,000 K) and −12% (130 GPa, 4,000 K), and they contribute more significantly to G by a P Δ r V energy component due to large P : The P Δ r V term increases from −0.13 eV at 20 GPa and 2,500 K, to −0.54 eV at 40 GPa and 4,000 K, and −0.88 eV at 130 GPa and 4,000 K (Figures 2d – 2f; SI, Table S2).…”