Investigation on the transformation behaviours of Fe-bearing minerals of coal in O2/CO2 combustion atmosphere containing H2O
The ratio of Fe2+-glass to Fe3+-glass in ashes from O2/CO2 atmosphere is significantly increased. The iron oxides (hematite or magnetite) formation of included iron minerals may be delayed in O2/CO2. H2O promotes iron oxides formation.
2016 ◽
Vol 82
(19)
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pp. 5869-5877
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1989 ◽
Vol 4
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pp. 244-248
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Keyword(s):
2009 ◽
Vol 8
(4)
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pp. 895-900
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