Abstract
High-temperature oxide melt solution calorimetry with molten 2PbO.B2O3 as a solvent can be used for determining enthalpies of formation of carbonates and hydrous silicates. Under conditions of gas flow at 1-2 cm3/s, all H2O and CO2 is expelled from the solvent, leading to a reproducible final thermodynamic state. Both analytical data and a number of thermodynamics cycles show that, under these conditions, the volatiles neither dissolve in nor interact energetically with the melt. -Authors
| Original language | English (US) |
|---|---|
| Pages (from-to) | 1099-1109 |
| Number of pages | 11 |
| Journal | American Mineralogist |
| Volume | 79 |
| Issue number | 11-12 |
| State | Published - 1994 |
| Externally published | Yes |
ASJC Scopus subject areas
- Geophysics
- Geochemistry and Petrology