Phase equilibria in the system CaO-CoO-SiO2 and gibbs energies of formation of the quaternary oxides CaCoSi2O6, Ca2CoSi2O7 and CaCoSiO4

Mukhopadhyay, Sukanya ; Jacob, K. T. (1996) Phase equilibria in the system CaO-CoO-SiO2 and gibbs energies of formation of the quaternary oxides CaCoSi2O6, Ca2CoSi2O7 and CaCoSiO4 American Mineralogist, 81 (7-8). pp. 963-972. ISSN 0003-004X

Full text not available from this repository.

Official URL: http://ammin.geoscienceworld.org/content/81/7-8/96...

Abstract

Phase relations in the pseudoternary system CaO-CoO-Si02 have been established at 1323 K. Three quaternary oxides were found to be stable: CaCoSi206 with clinopyroxene (Cpx), Ca2CoSi207 with melilite (Mel), and CaCoSi04 with olivine (01) structures. The Gibbs energies of formation of the quaternary oxides from their component binary oxides were measured using solid-state galvanic cells incorporating yttria-stabilized zirconia as the solid electrolyte in the temperature range of 1000-1324 K. The results can be summarized as follows: CoO (rs) + CaO (rs) + 2Si02 (Qtz)→CaCoSi206 (Cpx), ΔG°f = -117920 + 11.26T (:t 150) J/mol CoO (rs) + 2CaO (rs) + 2Si02 (Qtz)→Ca2CoSi207(Mel), ΔG°f = -192690 + 2.38T(:t130) J/mol CoO (rs) + CaO (rs) + Si02 (Qtz)→CaCoSi04 (01), ΔG°f = -100325 + 2.55T (:t 100) J/mol where rs = rock salt (NaCl) structure and Qtz = quartz. The uncertainty limits correspond to twice the standard error estimate. The experimentally observed miscibility gaps along the joins CaO-CoO and CaCoSi04-C02Si04 were used to calculate the excess free energies of mixing for the solid solutions CaXCo1-XO and (CayCo1-y)CoSi04:ΔGE = X(l - X)[31975X + 26736(1 - X)] J/mol and ΔGE = 23100 (±250) Y(l - Y)J/mol. A T-X phase diagram for the binary CaO-CoO was computed from the thermodynamic information; the diagram agrees with information available in the literature. The computed miscibility gap along the CaCoSi04-C02Si04 join is associated with a critical temperature of 1389 (±15) K. Stability fields for the various solid solutions and the quaternary compounds are depicted on chemical-potential diagrams for Si02, CaO, and CoO at 1323 K.

Item Type:Article
Source:Copyright of this article belongs to Mineralogical Society of America.
Keywords:Slag; Mineralogy; Disequilibrium; Smelting; Cu Ores; Archeometallurgy
ID Code:94961
Deposited On:10 Oct 2012 07:22
Last Modified:10 Oct 2012 07:22

Repository Staff Only: item control page