THE SYSTEM C-O IN EQUILIBRIUM WITH GRAPHITE AT HIGH-PRESSURE AND TEMPERATURE - AN EXPERIMENTAL-STUDY

Citation
S. Jakobsson et N. Oskarsson, THE SYSTEM C-O IN EQUILIBRIUM WITH GRAPHITE AT HIGH-PRESSURE AND TEMPERATURE - AN EXPERIMENTAL-STUDY, Geochimica et cosmochimica acta, 58(1), 1994, pp. 9-17
Citations number
33
Categorie Soggetti
Geosciences, Interdisciplinary
ISSN journal
00167037
Volume
58
Issue
1
Year of publication
1994
Pages
9 - 17
Database
ISI
SICI code
0016-7037(1994)58:1<9:TSCIEW>2.0.ZU;2-8
Abstract
The fluid system C-O has been studied experimentally in equilibrium wi th graphite at 7.5 to 20 kbars and 1100 to 1500-degrees-C. The results are compared to calculated results from the Redlich-Kwong equation of state and the Saxena and Fei corresponding states equation and are al so fitted to a virial equation of state to obtain interaction paramete rs and a new equation to calculate the oxygen fugacity of the graphite -oxygen (CCO) buffer. Experimental results were found to be lower in C O than calculated values, especially at high pressures and temperature s. Several experiments performed at different quench rates showed decr easing CO with increased quench time suggesting that CO reacts during the quench to form CO2. The data obtained from the quench experiments allow determination of the rate constant, k, for the quench reaction a t different P and T and calculation of zero-time concentrations.