Kinetics of reduction of iron oxides by H2: Part I: Low temperature reduction of hematite

This study deals with the reduction of Fe₂O₃ by H₂ in the temperature range of 220-680 °C. It aims to examine the rate controlling processes of Fe₂O₃ reduction by H₂ in the widest and lowest possible temperature range. This is to be related with efforts to decrease the emission of CO₂ in the atmosphere thus decreasing its green house effect.Reduction of hematite to magnetite with H₂ is characterized by an apparent activation energy ‘E_a’ of 76 kJ/mol. E_a of the reduction of magnetite to iron is 88 and 39 kJ/mol for temperatures lower and higher than 420 °C, respectively. Mathematical modeling of experimental data suggests that the reaction rate is controlled by two- and three-dimensional growth of nuclei and by phase boundary reaction at temperatures lower and higher than 420 °C, respectively.Morphological study confirms the formation of compact iron layer generated during the reduction of Fe₂O₃ by H₂ at temperatures higher than 420 °C. It also shows the absence of such layer in case of using CO. It seems that the annealing of magnetite's defects around 420 °C is responsible for the decrease of E_a.The rate of reduction of iron oxide with hydrogen is systematically higher than that obtained by CO.