Table 2
Initial volatile concentrations 
(ppm by mass) of CO2 and H2O in the mantle relative to a total mantle mass of 4.208 × 1024 kg.
| Case | Final outgassed | Initial abundance | ||
|---|---|---|---|---|
 |
 |
 |
 |
|
| (bar) | (ppm) | (ppm) | ||
| 1 | 0.1 | 25 | 63 | 234 |
| 2 | 0.13 | 32 | 79 | 227 |
| 3 | 0.25 | 74 | 160 | 197 |
| 4 | 0.33 | 110 | 221 | 181 |
| 5 | 0.5 | 220 | 380 | 155 |
| 6 | 0.66 | 441 | 666 | 136 |
| 7 | 0.75 | 662 | 941 | 128 |
| 8 | 0.83 | 1103 | 1483 | 121 |
| 9 | 0.9 | 1986 | 2558 | 116 |
Notes. Final volume mixing ratio and partial pressure of CO2 is 
and 
, respectively.All parameter combinations result in a 220 bar partial pressure atmosphere of H2O once solidification and hence outgassing is complete. A suffix of ‘v’ and ‘c’ to the case number denotes a variable and constant mixing length, respectively. An additional suffix of ‘s’ denotes that gravitational separation of the melt and solid phase is also included.
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