Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
American Mineralogist Don't get GSW? Talk to your librarian.
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

American Mineralogist; December 1997; v. 82; no. 11-12; p. 1063-1072
This Article
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 Order Hardcopy of Full Text via AGI/GeoRef
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Siewert, R.
Right arrow Articles by Rosenhauer, M.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Viscoelastic relaxation measurements in the system SiO 2 -NaAlSiO 4 by photon correlation spectroscopy

Ralf Siewert, and Matthias Rosenhauer

Universitaet Goettingen, Mineralogisch-Petrologisches Institut, Goettingen, Federal Republic of Germany

Relaxation times of longitudinal strain for five supercooled liquids along the join SiO 2 (qz)-NaAlSiO 4 (ne) including the compositions of albite (ab), ab 50 jd 50 , jadeite (jd), jd 66 ne 33 , and jd 33 ne 66 were measured by photon correlation spectroscopy within the temperature and relaxation time ranges 711-1116 degrees C and 35-2X10 (super -4) s, respectively. The measured time correlation functions are fitted to the Kohlrausch-Williams-Watts equation, Phi 1 (t) = exp(-t/tau 1 (sub P,T) ) (super beta ) , yielding isothermal relaxation functions for longitudinal strain at constant stress. The temperature dependence of the longitudinal strain relaxation times obeys an Arrhenian type equation. The relaxation of the longitudinal strain cannot be described by a single relaxation time but by a relaxation time distribution. The width of the relaxation time distribution, which is represented by the parameter beta , is independent over a large temperature range, indicating thermorheological simplicity. The decrease of the parameter beta corresponds to an increase of the excess (configurational) heat capacity with increasing (Na+Al) content, together indicating an increasing fragility of the supercooled liquids toward the composition of NaAlSiO 4 . Increasing fragility is also shown from the activation energy obtained from longitudinal strain relaxation and shear viscosity measurements, which passes a minimum near 40 mol% NaAlSiO 4 at low temperatures but decreases toward NaAlSiO 4 composition at higher temperatures. A comparison between strain, stress, and enthalpy relaxation times shows clearly that the relaxation process resulting from a thermal perturbation is slower than from a mechanical perturbation.

This record provided courtesy of AGI/GeoRef.




This article has been cited by other articles:


Home page
American MineralogistHome page
H. Walter, K. Roselieb, H. Buttner, and M. Rosenhauer
Pressure dependence of the solubility of Ar and Kr in melts of the system SiO2-NaAlSi2O6
American Mineralogist, September 1, 2000; 85(9): 1117 - 1127.
[Abstract] [Full Text] [PDF]


Home page
Geological Society, London, Special PublicationsHome page
D. B. Dingwell
Recent experimental progress in the physical description of silicic magma relevant to explosive volcanism
Geological Society, London, Special Publications, January 1, 1998; 145(1): 9 - 26.
[Abstract] [PDF]




JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2008 by Mineralogical Society of America