PARTITION OF SULFUR BETWEEN SODALITE AND HYDROTHERMAL FLUID - AN EXPERIMENTAL-STUDY

Citation
Ar. Kotelnikov et al., PARTITION OF SULFUR BETWEEN SODALITE AND HYDROTHERMAL FLUID - AN EXPERIMENTAL-STUDY, Geohimia, (11), 1996, pp. 1082-1087
Citations number
13
Categorie Soggetti
Geochemitry & Geophysics
Journal title
ISSN journal
00167525
Issue
11
Year of publication
1996
Pages
1082 - 1087
Database
ISI
SICI code
0016-7525(1996):11<1082:POSBSA>2.0.ZU;2-#
Abstract
The partition of sulfur between sodalite and the fluid at temperatures of 600-800 degrees C and 3 kbar pressure was studied experimentally. Sulfur enriches sodalite relative to the fluid over the entire composi tional range of sodalite. The sulfur partition between sodalite and th e fluid is not ideal. The partition coefficients do not depend on temp erature. The experimental data are used to obtain a relation between t he sulfur mole fraction in the fluid [X(S)(fl) = S/(S + Cl)] and the s odalite composition:(sic).