Ab initio simulations on metal-silicate partitioning of phosphorus during Earth’s core formation

Table S1 contains the fitted parameters of a local third-order finite strain expression, corresponding a Birch-Murnaghan equation-of-state for the metallic and silicate system at 10-135 GPa and 3000-5000 K. Table S2-S3 show the detailed data of two-phase coexistence simulations. Table S4 shows the detailed data. Table S5 shows the raw data of thermodynamic integration calculations. Table S6 shows the compilation of dataset from previous experiments.