Gasification Removal Behaviour of Phosphorus Compounds from High‐Phosphorous Iron Ore
The gasification removal behaviour of phosphorus from high‐phosphorus iron ore is theoretically and experimentally studied in the temperature range of 400–900 °C under H2 reducing and N2 atmospheres. In the first step, thermodynamic analysis is conducted to reveal the gasification and reaction behav...
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Veröffentlicht in: | Steel research international 2024-10, Vol.95 (10), p.n/a |
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Format: | Artikel |
Sprache: | eng |
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Zusammenfassung: | The gasification removal behaviour of phosphorus from high‐phosphorus iron ore is theoretically and experimentally studied in the temperature range of 400–900 °C under H2 reducing and N2 atmospheres. In the first step, thermodynamic analysis is conducted to reveal the gasification and reaction behaviours of common phosphorus compounds, namely P4O10, FePO4, AlPO4, Ca2P2O7, and Ca3(PO4)2. The results indicate that P4O10, FePO4, and AlPO4 under H2 reducing atmosphere and P4O10 under a N2 atmosphere can be removed by gasification, and the influence of the interaction between the vaporized gases and iron ore should be investigated. Therefore, dephosphorization experiments are performed on simulated iron ores containing P4O10, FePO4, or AlPO4. For the sample containing P4O10, ferric phosphates and iron phosphides are formed under the N2 and H2 reducing atmospheres, respectively, and their formation rates decreases with decreasing temperature, becoming almost stagnant at 400 °C. Moreover, it is confirmed that FePO4 and AlPO4 cannot be removed even when pure H2 is introduced.
In this study, gasification removal of phosphorus from high‐phosphorus iron ore is investigated experimentally and theoretically at temperatures ranging from 400 to 900 °C under H2 reducing and N2 atmospheres. Thermodynamic analysis shows effective removal of certain phosphorus compounds, while dephosphorization experiments reveal resistance in removing FePO4 and AlPO4, attributed to the reduction in Fe2O3 and increased H2O content in the atmosphere. |
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ISSN: | 1611-3683 1869-344X |
DOI: | 10.1002/srin.202400131 |