AN EQUATION OF STATE FOR ROEDDERITES, (K,NA)(2)MG-5[SI12O30] BASED ONKNUDSEN CELL MASS-SPECTROMETRY AND SYNTHESIS OF EIFELITE-ROEDDERITE CRYSTALLINE SOLUTIONS
P. Bruckmann et al., AN EQUATION OF STATE FOR ROEDDERITES, (K,NA)(2)MG-5[SI12O30] BASED ONKNUDSEN CELL MASS-SPECTROMETRY AND SYNTHESIS OF EIFELITE-ROEDDERITE CRYSTALLINE SOLUTIONS, Physics and chemistry of minerals, 20(5), 1993, pp. 362-368
Knudsen cell mass spectrometry has been applied to obtain activity (a(
i)) vs composition (X(i)) data for 18 synthetic roedderites. (K, Na)(2
)Mg5Si12O30, at temperatures between 800 degrees and 1100 degrees C. T
he samples were synthesized at 800 degrees C and 1 kbar P-H2O and char
acterized by X-ray powder diffractometry (XRD) and electron probe micr
oanalysis (EPMA) prior to mass spectrometric activity measurement. The
experimental a(i)-X(i) data have been smoothed, assuming for now the
simplest possible model of a two-site K-Na mixing for this binary crys
talline solution. Using the Margules formalism, and expressing the res
ults in terms of one atom of K-Na mixing, the tentative equation of st
ate is: W-G [J/mol] =-8704-0.0067.P, with P given in bar. The temperat
ure-dependence of W-G could not be resolved due to its large uncertain
ty on the order of 2.8 kJ/mol. A more rigorous thermodynamic model for
roedderites will have to be deferred until information on temperature
-dependent K-Na disordering becomes available. Besides roedderites, si
ngle-phase eifelite-roedderite crystalline solutions have also been sn
ythesized for the first time. They show a symmetric positive excess vo
lume of mixing,with W-V [J/bar.mol]=0.1064+/-0.0021.