Open Access

Table A.1

Species-specific gas solubility laws (above the line) and graphite/diamond and sulfide saturation parameterizations (below the line).

Species Reference Temperature [°C] Pressure [bar] O2 fugacity [-] Composition
H2 Hirschmann (2012) 1400-1450 7000-30000 IW basalt, andesite
H2O Sossi et al. (2023) 1900 1 IW–1.9-IW+6 peridotite
CH4 Hirschmann (2016) 1400-1800 350-32000 IW–3.6-IW+2.3 basalt
CO Hirschmann (2016) 1400-1800 350-32000 IW–3.6-IW+2.3 basalt
CO2 Hirschmann (2016) 1200-1625 100-25000 IW–l-FMQ+2 basalt
N2 Dasgupta et al. (2022) 1050-2327 1-82000 IW–8.3-IW+8.7 basalt
NH3a
HCNa
SH2a
S2 Gaillard et al. (2022) 800-1350 1-2000 IW–8.3-IW+5 basalt, dacite
SO2a$\[\mathrm{SO}_2^a\]$

CO Yoshioka et al. (2019) 1200-1600 2000-30000 NAb MORB, andesite, rhyolite
CO2 Eguchi & Dasgupta (2018) 950-1600 500-30000 FMQ–6-FMQ+1.5 foidite, rhyolite

aDissolution of these species has been neglected.

bNot Available.

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