Joint 52nd Northeastern Annual Section / 51st North-Central Annual Section Meeting - 2017

Paper No. 7-6
Presentation Time: 8:00 AM-12:00 PM

THE EFFECT OF FLUORINE ON MELT VISCOSITY IN JADEITE-LEUCITE MELTS


CARTY, Olin1, ROBERT, Geneviève1 and SMITH, Rebecca2, (1)Department of Geology, Bates College, Carnegie Science Hall, Lewiston, ME 04240, (2)Department of Geosciences, University of Massachusetts Amherst, Morrill Science Center, Amherst, MA 01003; Department of Geology, Bates College, Carnegie Science Hall, Lewiston, ME 04240, ocarty@bates.edu

We synthesized glasses along the jadeite-leucite (NaAlSi2O6-KAlSi2O6) join with various amounts of dissolved fluorine (up to 4 wt.%). All fluorine contents quoted are nominal amounts. Na:K ratios synthesized include Jd100, Jd75Lct25, Jd62.5Lct37.5, Jd50Lct50, Jd37.5Lct62.5, and Jd25Lct75, all of which have nominal ratios of non-bridging oxygen to tetrahedrally-coordinated cations (NBO/T) of 0. For Jd50Lct50, we synthesized glasses with 0, 1, 2, 3, and 4 wt.% F. For all other Na:K ratios, we only synthesized glasses with 0 and 2 wt.% F. We measured the viscosity of each melt by parallel-plate viscometry at temperatures between 655°C and 980°C. We use the temperature at which the viscosity is 1012 Pa.s (T12) to compare the effect of F on the different composition melts.

For F contents of 0 and 2 wt.%, at constant temperature, decreasing Na:K ratio increases viscosity. At 825°C, F-free Jd100 has a viscosity ~1.75 log units lower than F-free Jd25Lct75. At the same temperature, but with 2 wt.% dissolved F, Jd100 has a viscosity over ~3 log units lower than Jd25Lct75.

The addition of fluorine decreases the viscosity of each melt relative to its F-free equivalent. With the addition of 2 wt.% F, T12 decreases between 45°C and 130°C for the samples studied. The smallest reduction in T12 is for the Jd25Lct75 composition (45°C) while the largest reduction in T12 is calculated for Jd100 (130°C). The effect of F on viscosity therefore seems to be greater for Na-rich compositions. This is further confirmed in Jd50Lct50 melts for which we synthesized melts with additional nominal F contents. At 825°C, the addition of 1 wt.% F decreases viscosity by nearly 1 log unit. The addition of 2 and 3 wt.% F reduces viscosity by over 1.6 log units and 2 log units, respectively. The addition of 4 wt.% F reduces viscosity by almost 2.7 log units.

We conclude that increasing Na:K ratio and wt.% F both decrease the viscosity of the melts in this study and that dissolved F has a greater effect on the viscosity of Na-rich melts. Our results are consistent with the observed effect of Na:K ratio in more silica rich melts, with albite melt having a viscosity nearly 3 orders of magnitude lower than orthoclase melt at ~925°C. Our results also show a similar effect of F on the viscosity of jadeite and albite melts, with a reduction in T12 for 2 wt.% F of ~130°C in both melts.