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Volume Changes of Iron Oxide Compacts under Isothermal Reduction Conditions
Author(s) -
Mousa ElSayed A.,
Omar Adel A.,
Nasr Mahmoud I.,
ElGeassy AbdelHady A.
Publication year - 2007
Publication title -
steel research international
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.603
H-Index - 49
eISSN - 1869-344X
pISSN - 1611-3683
DOI - 10.1002/srin.200706252
Subject(s) - isothermal process , materials science , swelling , volume (thermodynamics) , hydrogen , diffusion , metal , wüstite , carbon monoxide , activation energy , chemical reaction , whiskers , iron oxide , oxide , metallurgy , chemical engineering , chemistry , composite material , thermodynamics , catalysis , physics , organic chemistry , engineering , biochemistry
Compacts made from chemically grade Fe 2 O 3 were fired at 1473K for 6 hrs. The fired compacts were isothermally reduced either by hydrogen or carbon monoxide at 1073–1373K. The O 2 weight‐loss resulting from the reduction process was continuously recorded as a function of time using TGA technique, whereas the volume change at different reduction conditions was measured by displacement method. Porosity measurements, microscopic examination and X‐ray diffraction analysis were used to characterize the fired and reduced products. The rate of reduction at both the initial and final stages was increased with temperature. The reduction mechanism deduced from the correlations between apparent activation energy values, structure of partially reduced compacts and application of gas‐solid reaction models revealed the reduction rate (dr/dt) at both the initial and final stages. At early stages, the reduction was controlled by a combined effect of gaseous diffusion and interfacial chemical reaction mechanism, while at the final stages the interfacial chemical reaction was the rate determining step. In H 2 reduction, maximum swelling (80%) was obtained at 1373K, which was attributed to the formation of metallic iron plates. In CO reduction, catastrophic swelling (255%) was obtained at 1198K due to the formation of metallic iron plates and whiskers.