Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
American Mineralogist Signup for GSW Email News
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

American Mineralogist; January 2007; v. 92; no. 1; p. 114-123; DOI: 10.2138/am.2007.2246
© 2007 Mineralogical Society of America
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Similar articles in Web of Science
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Web of Science (5)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Lange, R. A.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

The density and compressibility of KAlSi3O8 liquid to 6.5 GPa

Rebecca A. Lange*

Department of Geological Sciences, 1100 N. University Avenue, University of Michigan, Ann Arbor, Michigan 48109-1005, U.S.A.

Correspondence: * E-mail: becky{at}umich.edu

The thermodynamic properties of crystalline and liquid KAlSi3O8 are used to calculate the fusion curve of sanidine to 6.5 GPa. New values for the enthalpy and entropy of fusion of sanidine at one bar and 1200 °C ({Delta}HTf = 63.0 kJ/mol, {Delta}STf = 42.8 J/mol-K) are recommended on the basis of improved heat-capacity equations for KAlSi3O8 crystal, glass, and liquid. On the basis of phase-equilibrium experiments on the congruent melting reaction between 2 and 6.5 GPa, the pressure dependence of the liquid compressibility (K0 ’ = dK0/dP, where K0 = 1/ß0) is constrained to be 12.2 ± 1.0 in a third-order Birch-Murnaghan equation of state (EOS). The metastable, one-bar melting temperature (Tf ) is additionally constrained to be 1203 ± 26 °C. Determination of the liquid K0 ’ allows the density and compressibility of KAlSi3O8 liquid to be calculated to 6.5 GPa (2.709 ± 0.014 g/cm3 at 1600 °C). The uncertainty in K0 ’ of ±1.0 leads to an error in melt density at 6.5 GPa of ±0.52%. With a K0 ’ = 12.2, the relatively high compressibility of KAlSi3O8 liquid at 1600 °C (K0 = 15.8 GPa) drops rapidly with increasing pressure. The dominant mechanism of compression for KAlSi3O8 liquid between 0 and 6.5 GPa most likely involves topological changes and increases in network connectivity with pressure. It is probable that highly compressible liquids, such as hydrous, silica-rich liquids formed by partial melting of a subducted slab, may have K0 values that exceed 12 (at pressures ≤ 6.5 GPa).

Key Words: Sanidine • fusion curve • enthalpy of fusion • topology • equation of state




This article has been cited by other articles:


Home page
American MineralogistHome page
T. J. Tenner, R. A. Lange, and R. T. Downs
The albite fusion curve re-examined: New experiments and the high-pressure density and compressibility of high albite and NaAlSi3O8 liquid
American Mineralogist, October 1, 2007; 92(10): 1573 - 1585.
[Abstract] [Full Text] [PDF]




JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2009 by Mineralogical Society of America