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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

Figure 3: γNalloy melt and DNalloy/silicate as a function of oxygen fugacity and carbon content in the alloy melt.

Figure 3:

a) γNalloy melt in C-poor and Si-free alloy melts in this study is ~1 while Nalloy melt is ~3-4 at similar fO2 for graphite-saturated alloys. This is due to non-ideal interactions between C and N occupying similar octahedral voids in the alloy melt. Higher γNalloy melt for C-poor and Si-bearing alloys results from repulsive interactions between Si and N. b) In agreement with previous studies in graphite-saturated conditions1013,25,29, DNalloy/silicate decreases with decreasing fO2 in graphite-undersaturated conditions. At any given fO2, DNalloy/silicate in graphite-undersaturated conditions is almost an order of magnitude higher relative to graphite-saturated conditions. γNalloy melt was calculated using the ‘Online Metal Activity Calculator’ (http://norris.org.au/expet/metalact/) which uses ε approach via Wagner equations. Error bars for DNalloy/silicate 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.