THERMOCHEMISTRY OF CARBONATE-PYROXENE EQUILIBRIA

The enthalpies of drop solution of calcite. magnesite, dolomite, wollastonite and diopside have been measured in a lead borate solvent at 977 K in a Calvet-type microcalorimeter. The carbonate calorimetry was done under flowing gas atmosphere. Both natural and synthetic samples were used. From these calorimetric data, the enthalpies of several reactions of carbonate with quartz were calculated. The enthalpies of these reactions (kJ/mol) at 298 K are: calcite + quartz --> wollastonite + CO2, 92.3 +/- 1.0; magnesite + quartz --> enstatite + CO2, 82.9 +/- 2.8; dolomite + quartz --> diopside + CO2, 163.0 +/- 1.9. These values generally are in agreement with those calculated from Robie et al., Helgeson et al.. Berman and Holland and Powell. The enthalpy of the dolomite-quartz reaction overlaps marginally with those from Berman and Holland and Powell. The enthalpy of formation of dolomite from magnesite and calcite ( - 11.1 +/- 2.5 kJ/mol) was also derived from the measured enthalpies, and this value is consistent with that from acid solution calorimetric measurements as shown by Navrotsky and Capobianco, but different from values in the earlier literature. These results support the premise that drop-solution of carbonates into molten lead borate results in a well-defined final state consisting of dissolved oxide and evolved CO2, This was also confirmed by weight change experiments. Thus, oxide melt calorimetry is applicable to carbonates.