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• W2095066341 startingPage "5125" @default.
• W2095066341 abstract "Because of the relatively large surface energy of liquid basalt, the nuclcation of CO 2 bubbles in mid‐ocean ridge basalts (MORB) requires degrees of supersaturation, which vary from 1.5 to 7, depending on the pressure. This pressure sensitivity is a direct consequence of the increase in the molar volume of gaseous CO 2 when the pressure decreases. This causes the surface area of stable nuclei with a constant number of carbon dioxide molecules to become larger with decreasing pressure. Of the major igneous gases, CO 2 is the most abundant in uncontaminated MORB, but has the smallest solubility. Therefore bubbles in MORB at P > 100 bar are CO 2 dominated. The recently discovered CO 2 supersaturation in MORB [Dixon et al., 1988; Fine and Stolper, 1986] can be explained as being due to the difficulty of bubble nucleation at low pressure." @default.
• W2095066341 created "2016-06-24" @default.
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• W2095066341 date "1990-04-10" @default.
• W2095066341 modified "2023-10-13" @default.
• W2095066341 title "Mid‐ocean ridge basalt degassing: Bubble nucleation" @default.
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• W2095066341 doi "https://doi.org/10.1029/jb095ib04p05125" @default.
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