An internally consistent thermodynamic dataset with uncertainties and correlations: 2. Data and results
- 1 December 1985
- journal article
- Published by Wiley in Journal of Metamorphic Geology
- Vol. 3 (4) , 343-370
- https://doi.org/10.1111/j.1525-1314.1985.tb00325.x
Abstract
This, the second of two papers, represents the application of a least squares approach, discussed in the previous paper, to the generation of an internally consistent thermodynamic dataset involving 60 reactions among 43 phases, in the system K2O–Na2O–CaO–MgO–Al2O3–SiO2–H2O–CO2. We make the assumption that all the thermodynamic data, with the exception of enthalpies of formation of the phases, are well known, and solve for an internally consistent set of enthalpies which reproduces the 60, experimentally determined, phase equilibrium reactions. An important difference between our dataset and that of previous alternatives in the literature is that we are able to determine the uncertainties on, and correlations between, the enthalpies of formation for all phases in the set, and hence are able to apply simple error propagation techniques to determine the uncertainties in any phase equilibrium calculations performed using this dataset. Selection of reactions, for geothermometry and geobarometry, may be more readily made by choosing equilibria with small uncertainties in their thermodynamics. Our data are in reasonably close agreement with the high temperature molten oxide calorimetry results on silicate minerals where available, a fact which lends a degree of confidence to the results.Keywords
This publication has 59 references indexed in Scilit:
- An internally consistent thermodynamic dataset with uncertainties and correlations: 1. Methods and a worked exampleJournal of Metamorphic Geology, 1985
- Fe-free clinozoisite stability relative to zoisiteNature, 1983
- Slaty cleavage and related strain in Martinsburg Slate, Delaware Water Gap, New JerseyAmerican Journal of Science, 1978
- An experimental investigation of the system MgO-SiO 2 -H 2 O-CO 2American Journal of Science, 1969
- Experimental determination of kyanite-andalusite and andalusite-sillimanite equilibria; the aluminum silicate triple pointAmerican Journal of Science, 1969
- Kyanite-sillimanite equilibrium between 700 degrees and 1500 degrees CAmerican Journal of Science, 1968
- Kyanite-Andalusite Equilibrium from 700° to 800°CScience, 1966
- Kyanite-Sillimanite Equilibrium at 750°CScience, 1966
- Lawsonite equilibriaAmerican Journal of Science, 1965
- Studies in the system CaO-MgO-CO 2 ; Part 1, The thermal dissociation of calcite, dolomite and magnesiteAmerican Journal of Science, 1955