Thermal diffusivity of fluid oxygen to 12 GPa and 300[degree]C
Journal Article
·
· Journal of Chemical Physics
- Department of Chemistry, University of Washington, Seattle, Washington 98195 (United States)
- 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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Related Subjects
37 INORGANIC, ORGANIC, PHYSICAL, AND ANALYTICAL CHEMISTRY
400201* -- Chemical & Physicochemical Properties
ELEMENTS
FLUIDS
LIQUEFIED GASES
LIQUIDS
NONMETALS
OXYGEN
PHYSICAL PROPERTIES
TEMPERATURE DEPENDENCE
TEMPERATURE RANGE
TEMPERATURE RANGE 0273-0400 K
THERMAL CONDUCTIVITY
THERMAL DIFFUSIVITY
THERMODYNAMIC PROPERTIES
VERY HIGH PRESSURE
400201* -- Chemical & Physicochemical Properties
ELEMENTS
FLUIDS
LIQUEFIED GASES
LIQUIDS
NONMETALS
OXYGEN
PHYSICAL PROPERTIES
TEMPERATURE DEPENDENCE
TEMPERATURE RANGE
TEMPERATURE RANGE 0273-0400 K
THERMAL CONDUCTIVITY
THERMAL DIFFUSIVITY
THERMODYNAMIC PROPERTIES
VERY HIGH PRESSURE