Fig. 16From: Mass transfer in the Earth’s interior: fluid-melt interaction in aluminosilicate–C–O–H–N systems at high pressure and temperature under oxidizing conditionsPartition coefficient between fluid and melt of N2, KN2f/m, as a function of temperature. The least squares straight line fit is, KH2Of/m = −1.9 ± 0.5 + 2356 ± 450/T, r2 = 0.90Back to article page
