FIGURE 2. Theoretical fractionation of silicon isotopes between silicate and metal as a function of temperature.

From the following article:

Silicon in the Earth's core

R. Bastian Georg, Alex N. Halliday, Edwin A. Schauble & Ben C. Reynolds

Nature 447, 1102-1106(28 June 2007)

doi:10.1038/nature05927

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Equilibrium 30Si/28Si fractionation (epsilon = 1,000 lnalphasilicate-metal) between silicate and metal is estimated from lattice-dynamics modelling of Mg2SiO4-olivine and body-centred cubic Fe3Si. The lower (black) curve is calculated assuming Si-atom vibration at 10 THz in the Fe3Si structure. The upper (grey) curve assumes Si-atom vibration at 7.5 THz in Fe3Si. The dashed curves at temperatures above 1,200 °C (1,473 K) indicate extrapolation beyond the 1 atm melting point of Fe3Si.

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