Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
European Journal of Mineralogy Don't get GSW? Talk to your librarian.
JOURNAL HOME HELP FEEDBACK/COMMNET SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

European Journal of Mineralogy; August 1999; v. 11; no. 4; p. 709-719
This Article
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Harlov, D. E.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Thermochemistry of Ag-Cu exchange equilibria between proustite, sinnerite, and pearceite; constraints on Ag-Cu and As-Sb mixing in pyrargyrite-proustite

Daniel E. Harlov

GeoForschungsZentrum Potsdam, Potsdam, Federal Republic of Germany

Experimental Ag-Cu exchange equilibria (evacuated silica tubes; variable mass ratio) involving proustite (Ag,Cu) 3 AsS 3 , smithite AgAsS 2 , pearceite (Ag,Cu) 16 As 2 S 11 , lautite CuAsS, and sinnerite Cu 6 As 4 S 9 are reported over the temperature range 150-350 degrees C. Lautite and sinnerite are found to take in negligible amounts of Ag (below the detection limit of the microprobe), even at 350 degrees C. Similarly smithite is found to take in <1% Cu. Utilizing new Ag-Cu exchange data between proustite and pearceite and previously published As-Sb exchange data between pyrargyrite-proustite (Ag,Cu) 3 (Sb,As)S 3 and polybasite-pearceite (Ag,Cu) 16 (Sb,As) 2 S 11 , a model is calibrated which reflects both the Ag-Cu and As-Sb mixing properties of the pyrargyrite-proustite solid solution over the temperature range 120-400 degrees C. Explicit provision for site distortion in proustite resulting from the Cu+ for Ag+ substitution (or Ag+ for Cu+ substitution) is made by assuming that the standard state properties of the Ag-proustite and Cu-proustite end members are linearly dependent on the Cu/(Cu+Ag) ratio. Cu substitution in pyrargyrite-proustite is both asymmetric and substantially non-ideal (W (super Pyr-Prs) CuAg = 21.0; W (super Pyr-Prs) AgCu = 11+ or -0.5 kJ/gfw) as opposed to As-Sb mixing along the proustite-pyrargyrite join, which has been found to be both more symmetric and more ideal (W (super Pyr-Prs) AsSb = 6.00+ or -0.60 kJ/gfw). The reciprocal energy, Delta G rec , between proustite and pyrargyrite is found to approximate 0. Ag-Cu exchange experiments between pearceite grains and equimolar powder mixtures of proustite and sinnerite are used to define equilibrium compositions for a three-phase region involving proustite, pearceite and sinnerite over the temperature range 150-350 degrees C.

This record provided courtesy of AGI/GeoRef.







JOURNAL HOME HELP FEEDBACK/COMMNET SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2010 by E. Schweizerbart'sche Verlagsbuchhandlung Science Publishers