Abstract
The chemical potential of oxygen defined by the equilibrium: {Mathematical expression} has been measured between 850 and 1250 K via an electrochemical method using calcia-stabilized zirconia electrolytes and either Ni+NiO or Cu+Cu2O as the reference electrode. The results are: {Mathematical expression} where μO2 is in J·mol-1, T in kelvins, and the reference pressure for O2 is 1 bar (105 Pa). (Values in terms of log- {Mathematical expression}may be obtained from the above expression by dividing by R Tln10, where R=8.31441 J.K-1·mol-1). The standard enthalpy of formation of ReO2 is-444.350±0.400 (1σ) kJ·mol-1, requiring a significant modification to previously published estimates. These results were checked in hydrothermal experiments using the double capsule method with NiO+Ni-Pd alloy as an oxygen sensor. Reversals at P=1 kbar over the T range 823 to 1073 K are in good agreement with the electrochemical measurements. These latter results also serve to demonstrate: (1) the usefulness of the "redox sensor" method; (2) the viability of using Re+ReO2 as a buffer in hydrothermal experiments. Re+ReO2 lies nearly midway between the Ni+NiO and Fe3O4+Fe2O3 buffers in μO2-T space, and thus fills a petrologically important gap in the range of μO2s which can be covered by accurately calibrated oxygen buffers.
Original language | English |
---|---|
Pages (from-to) | 130-137 |
Number of pages | 8 |
Journal | Contributions of Mineralogy and Petrology |
Volume | 118 |
Issue number | 2 |
DOIs | |
Publication status | Published - Jun 1994 |
Externally published | Yes |