Thermal expansion of molten Fe2SiO4 at high pressure

Details Thermal expansion of molten Fe2SiO4 at high pressure Thermal expansion of molten Fe2SiO4 at high pressure

Jun 1992

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1992georl..19.1173a&link_type=abstract

Geophysical Research Letters (ISSN 0094-8276), vol. 19, no. 11, June 2, 1992, p. 1173-1176.

Physics

4

High Pressure, Iron Oxides, Melts (Crystal Growth), Silicates, Thermal Expansion, Buoyancy, Density Measurement, Pressure Effects, Ruby

Scientific paper

The density of molten Fe2SiO4 has been bracketed at temperatures up to 1873 K in the pressure range 1.1 to 1.6 GPa by observing sinking and floating ruby buoyancy markers in piston-cylinder experiments. The sink/float method can be employed not only for compressibility studies of silicate melts, but as well for determining melt thermal expansion at high pressure.

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