Heat capacity and thermodynamic properties of nearly stoichiometric wustite from 13 to 450 K

Heat capacity and thermodynamic properties of nearly stoichiometric wustite from 13 to 450 K

The heat capacity of a three-phase sample of Fe0.990 ± 0.005O, Fe3O4 and Fe (mole fractions 0.915, 0.078 and 0.007, respectively) has been measured by adiabatic shield calorimetry at T from 13 to 450 K.

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Veröffentlicht in:The American mineralogist 1996-08, Vol.81 (7-8), p.973-981
Hauptverfasser: Stolen, Svein, Glockner, Ronny, Gronvold, Fredrik, Atake, Tooru, Izumisawa, Satoru
Format: Artikel
Sprache:eng
Schlagworte:
Calorimetry
Chemistry
Geology
Heat
heat capacity
Iron
Iron oxides
lattice parameters
magnetite
Mineralogy
Minerals
nonsilicates
order-disorder
oxides
phase equilibria
stoichiometry
thermodynamic properties
Thermodynamics
wustite
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container_end_page 981
container_issue 7-8
container_start_page 973
container_title The American mineralogist
container_volume 81
creator Stolen, Svein
Glockner, Ronny
Gronvold, Fredrik
Atake, Tooru
Izumisawa, Satoru
description The heat capacity of a three-phase sample of Fe0.990 ± 0.005O, Fe3O4 and Fe (mole fractions 0.915, 0.078 and 0.007, respectively) has been measured by adiabatic shield calorimetry at T from 13 to 450 K.
doi_str_mv 10.2138/am-1996-7-819
format Article
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source Free Full-Text Journals in Chemistry; EZB Electronic Journals Library
subjects Calorimetry
Chemistry
Geology
Heat
heat capacity
Iron
Iron oxides
lattice parameters
magnetite
Mineralogy
Minerals
nonsilicates
order-disorder
oxides
phase equilibria
stoichiometry
thermodynamic properties
Thermodynamics
wustite
title Heat capacity and thermodynamic properties of nearly stoichiometric wustite from 13 to 450 K
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