摘要
Precipitated iron oxide samples were characterized using temperature-programmed reduction. H2 was used as the reduction agents. The two-stage reduction was observed: Fe2O3 was reduced to Fe3O4 and then reduced to metallic Fe. The activation energy for the two reduction steps of iron oxide are 89.13 and 70.412 (kJ mol-1), respectively. The simulation by reduction models of the TPR patterns presents well fitting of unimolecular model for Fe2O3 → Fe3O4 reduction and two-dimensional nucleation according to Avarmi-Erofeev model for Fe3O4 → Fe.
原文 | ???core.languages.en_GB??? |
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頁(從 - 到) | 61-67 |
頁數 | 7 |
期刊 | Thermochimica Acta |
卷 | 400 |
發行號 | 1-2 |
DOIs | |
出版狀態 | 已出版 - 17 4月 2003 |