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Thermal diffusivity of fluid oxygen to 12 GPa and 300[degree]C

Journal Article · · Journal of Chemical Physics
DOI:https://doi.org/10.1063/1.479849· OSTI ID:6060686
;  [1];  [2]
  1. Department of Chemistry, University of Washington, Seattle, Washington 98195 (United States)
  2. Geophysics Program, University of Washington, Seattle, Washington 98195 (United States)
The thermal diffusivity of fluid oxygen in the diamond-anvil cell has been measured from 1 to 12.6 GPa and 25 to 300 hthinsp;[degree]C. These constitute the first experimental measurements of thermal transport properties of simple fluids above 1 GPa. Diffusivities are found to rise sharply from a minimum at intermediate pressures and then to level off at [approximately]6 GPa. Thermal conductivities derived from these measurements do not vary as [radical]T, rather the excess conductivities are approximately independent of temperature. The diffusivities of nitrogen, previously measured to 1 GPa, closely match those of oxygen when scaled as suggested by a simple, corresponding states theory. [copyright] [ital 1999 American Institute of Physics.]
OSTI ID:
6060686
Journal Information:
Journal of Chemical Physics, Journal Name: Journal of Chemical Physics Vol. 111:20; ISSN JCPSA6; ISSN 0021-9606
Country of Publication:
United States
Language:
English

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