1996
DOI: 10.2355/isijinternational.36.269
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Evolution of Porosity Profiles of Magnetite Phase during High Temperature Reduction of Hematite.

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Cited by 9 publications
(4 citation statements)
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“…Haematite grains cracks and along the walls of these cracks and fissures magnetite preferentially forms. 15 By 960°C haematite is completely converted to magnetite (Fig. 9).…”
Section: Resultsmentioning
confidence: 99%
“…Haematite grains cracks and along the walls of these cracks and fissures magnetite preferentially forms. 15 By 960°C haematite is completely converted to magnetite (Fig. 9).…”
Section: Resultsmentioning
confidence: 99%
“…The hematite-to-magnetite transformation is direct, without a metastable amorphous intermediate. It is described by the ''shrinking-core'' model with the formation of a outer magnetite layer at the surface of the hematite particles that proceeds toward the core of the reacting hematite by diffusion of oxygen throughout the newly formed magnetite layer [29,30]. This mechanism of magnetite formation is confirmed by scanning-electron micrographs of A 6 and A 1 .…”
Section: Xrd Measurementsmentioning
confidence: 74%
“…The change in texture affect the oxidation and growth since the particle density of the nuclei formed is a function of temperature, oxygen pressure and crystallographic orientation. Moreover, Janowski et al [29] reported that at the end of the hematite-to-magnetite transformation a dramatic change in the texture of the sample occurs. They ascribed this change to an increase of porosity and an increase in pore diameter.…”
Section: Xrd Measurementsmentioning
confidence: 98%
“…[5][6][7][8][9][10][11][12][13][14][15][16] However, direct reduction with a solid carbon was not carried out and no consideration of crystallographic orientation was conducted. Furthermore, there is little publication on the in situ observation of the reaction and its mechanism between solid carbon and iron oxide.…”
Section: Introductionmentioning
confidence: 99%