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Fig. 4

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Condensation temperatures (TC) of the rock-forming elements Mg, Si, Ca, and Al, plotted against the molar C/O ratio in disks, based on stellar ϵC/ϵO values (top). Solar C/O = 0.55 (Asplund et al. 2009) is indicated as a vertical dashed line. All elements show a transition from high TC at low C/O to lower TC at higher C/O. For Mg, colouring condensation temperature by the disk Mg/O (= ϵMg / ϵO; bottom) reveals that the C/O value at which this transition occurs depends on Mg/O. Condensation temperatures are derived from condensation sequence calculations at P = 10−4 bar.

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