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. Author manuscript; available in PMC: 2021 Dec 1.
Published in final edited form as: Nat Geosci. 2021 May 10;14:369–376. doi: 10.1038/s41561-021-00733-0

Extended Data Fig. 5. DNalloy/silicate as a function of oxygen fugacity and (a) silicon content in the alloy and (b) temperature.

Extended Data Fig. 5

a) In addition to the effect of fO2, when Si content in the alloy melt and FeO content in the silicate melt are coupled to each other, incorporation of Si into the alloy melt on its own has a strong negative effect on N content in the alloy at a similar logfO2 (~IW–4; here shown by grey rectangle). A similar effect has been observed in a previous study11 albeit at a higher logfO2 (~IW–2.5) because in graphite-saturated alloys, Si expels N from the alloy melt even at lower concentrations (as low as 0.1 wt.% Si). b) In contrast to the observations of previous studies11,12 in graphite-saturated conditions, temperature does not have any discernible effect on DNalloy/silicate in the limited temperature range explored in this study. Error bars represent ±1-σ deviation obtained by propagation of ±1-σ deviation on N content in the alloy and silicate melts; where absent, the error bars are smaller than the symbol size.