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| Naji, M. |
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| Motta, Antonella |
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| Aletan, Dirar |
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| Mohamed, Tarek |
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| Ertürk, Emre |
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| Taccardi, Nicola |
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| Kononenko, Denys |
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| Petrov, R. H. | Madrid |
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| Alshaaer, Mazen | Brussels |
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| Bih, L. |
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| Casati, R. |
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| Muller, Hermance |
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| Kočí, Jan | Prague |
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| Šuljagić, Marija |
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| Kalteremidou, Kalliopi-Artemi | Brussels |
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| Azam, Siraj |
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| Ospanova, Alyiya |
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| Blanpain, Bart |
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| Ali, M. A. |
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| Popa, V. |
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| Rančić, M. |
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| Ollier, Nadège |
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| Azevedo, Nuno Monteiro |
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| Landes, Michael |
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| Rignanese, Gian-Marco |
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Frost, Ray
in Cooperation with on an Cooperation-Score of 37%
Topics
Publications (18/18 displayed)
- 2020Volatilisation of trace elements during reduction of iron ore by hydrogencitations
- 2019Elemental deportment and chemical structure evolution of iron ore during direct reduction in hydrogen atmosphere
- 2016Environmental applications of inorganic-organic clays for recalcitrant organic pollutants removal: Bisphenol Acitations
- 2014Vibrational spectroscopy of the sulphate mineral sturmanite from Kuruman manganese deposits, South Africacitations
- 2014Infrared and raman spectroscopic characterization of the borate mineral vonsenite Fe2/2+ Fe3+BO5citations
- 2014A vibrational spectroscopic study of the phosphate mineral churchite (REE)(PO4).2H2Ocitations
- 2013Vibrational spectroscopic characterization of the phosphate mineral kulanite Ba(Fe2+,Mn2+,Mg)2(Al,Fe3+)2(PO4)3(OH)3citations
- 2013Vibrational spectroscopic characterization of the phosphate mineral series eosphorite-childrenite-(Mn,Fe)Al(PO4)(OH)2.(H2O)citations
- 2013The phosphate mineral arrojadite-(KFe) and its spectroscopic characterizationcitations
- 2013Vibrational spectroscopic characterization of the phosphate mineral phosphophyllite - Zn2Fe(PO4)2.4H2O, from Hagendorf Sud, Germany and in comparison with other zinc phosphatescitations
- 2012Thermal analysis and application of organoclays for water purification
- 2012Raman and infrared spectroscopic characterization of beryllonite, a sodium and beryllium phosphate mineral - implications for mineral collectorscitations
- 2011Characterisation of organoclays and adsorption of p-nitrophenol: Environmental applicationcitations
- 2011Synthesis and vibrational spectroscopy of halotrichite and bilinitecitations
- 2009Thermal decomposition of hydrotalcites with variable cationic ratioscitations
- 2008Thermal decomposition of synthesized layered double hydroxides based upon Mg/(Fe,Cr) and carbonatecitations
- 2008Thermal decomposition of hydrotalcite with molybdate and vanadate anions in the interlayercitations
- 2008Characterisation of red mud and seawater neutralised red mud using vibrational spectroscopic techniques
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article
Volatilisation of trace elements during reduction of iron ore by hydrogen
Abstract
<p>Reduction of iron ore directly by H<sub>2</sub> has been developed as an alternative technology for iron production, which can alleviate pollutant emissions by eliminating the needs of cokemaking and sintering processes. However, the behaviour of trace elements (especially the volatilisation of heavy metal(loid)s) in iron ore during reduction by H<sub>2</sub> is still unclear and the relevant research is scarce in literature. This study aimed to provide an insight into the volitilisation behaviour of trace elements and the environmental assessment during reduction of Australian iron ore with H<sub>2</sub> from room temperature to 1000 °C. The trace element concentrations in the iron ore at different reduction tempatures were analysed along with changes in chemical structure and surface morphology using X-ray diffraction, Fourier transform infrared spectroscopy, Raman spectroscopy and scanning electron microscopy. Results showed that the extent of As, S, Li, Sn and Pb volatilisation varied with temperature with nil, 22%, 82%, 82% and 72% respectively remaining in the sample at 1000 °C. Simutaneously, stepwise reduction of iron ore (goethite → wustite) with temperature was confirmed. Pearson's method of correlation was employed to determine the correlations between pairs of key indexes (LOI 1000, mass loss%, O loss% and loss ratios of elements) of goethite reduction. Results indicated that S loss exhibited a high correlation (r = 0.977) with Pb loss, implying the simultaneous volatilisation of Pb and S as well as possible presence of Pb and S-containing compounds, such as PbS in the sample. Li and Sn showed the coincidental simultaneous volatilisation as indicated by the highest correlation (r = 1.000 with p ≤ 0.01). The kinetic analysis indicated that the volatilisation of above elements best fitted diffusion models (D1 or D3) with activation energy (E) ranging within 11.65–26.75 kJ/mol. Risk assessment analysis demonstrated a much higher risk score of iron ore reduciton at 1000 °C (value of 94.758) than 200 and 500 °C (value of 1–3) due to obvious volatilisation of As and Pb at high temperature. Life cycle impact assessment (LCIA) data confirmed four valid impact categories with human toxicity being the most significnat with the major contribution ascribed to As element. Generally, the hazardous elements released from the ore reduction process can be eliminated before their discharge to the environment.</p>