carbon monoxide reduces Fe2O3 to
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Natural hematite, the most widely studied Fe oxide, can be reduced by hydrogen (H2) [108], carbon monoxide (CO) [109, 110] , and gas mixtures [111]. The phase transformations of hematite in reducing gases between 650 and 900 °C occur via the following pathway: α-Fe2O3 → Fe3O4 → FeO → Fe 0 [108][109][110].
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