Pa. Rock et al., A NEW METHOD FOR DETERMINING GIBBS ENERGIES OF FORMATION OF METAL-CARBONATE SOLID-SOLUTIONS .1. THE CAXCD1-XCO3(S) SYSTEM AT 298-K AND 1-BAR, Geochimica et cosmochimica acta, 58(20), 1994, pp. 4281-4291
New thermodynamic data are presented for mixing of calcite (CaCO3(s))
and otavite (CdCO3(s)) to form Ca(x)Cd1-xCO3(s) solutions. A reversibl
e equilibrium was achieved between the aqueous solution and the metast
able solid solution using electrochemical double cells and a new elect
rode of the third kind. Evidence that the cell reactions are reversibl
e includes demonstration of Nernstian response to changes in electroly
te composition and an absence of significant hysteresis in cell curren
t-voltage and current-temperature (10-35-degrees-C) plots. We observe
negative excess Gibbs energies for mixing on the order of 0 to -6.6 kJ
.mol-1; these magnitudes are sensitive to uncertainties in the estimat
es of DELTAG(f)o[CdCO3(s)]. The double-cell method is potentially usef
ul in other systems where, through incorporation of impurities, the ac
tivity of the CaCO3(s) is not unity relative to the standard state of
the pure, well-crystallized, endmember mineral. It remains to be seen
whether the double cell method is equally useful for systems, such as
the Ca(x)Mg1-xCO3(s) or Ca(x)Sr1-xCO3(s) solid solutions, that have va
riable and positive excess Gibbs energies, but some of the same advant
ages would apply.