2015
DOI: 10.1016/j.fuproc.2014.12.027
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Effect of H2O on pyrite transformation behavior during oxy-fuel combustion

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Cited by 31 publications
(11 citation statements)
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“…On the other hand, the combustion particles are more easily fragmented as more oxygen diffuses to the particle surface making it greatly difficult for iron-bearing minerals to be in contact with clay or other silicates included in the particles to form Fe-glass. 2,12,25 Our previously-reported study 34 supported the results presented herein, highlighting that the reaction rate of pyrite in the steam-containing atmosphere to be higher than that in the CO 2 -containing atmosphere. In the DTF experiment, the addition of water vapor increases the transformation of octahedral magnetite to tetrahedral magnetite, thus, facilitating the formation of hematite from magnetite.…”
Section: Fe-containing Phases Of Ashes Produced From Dtf Experimentssupporting
confidence: 89%
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“…On the other hand, the combustion particles are more easily fragmented as more oxygen diffuses to the particle surface making it greatly difficult for iron-bearing minerals to be in contact with clay or other silicates included in the particles to form Fe-glass. 2,12,25 Our previously-reported study 34 supported the results presented herein, highlighting that the reaction rate of pyrite in the steam-containing atmosphere to be higher than that in the CO 2 -containing atmosphere. In the DTF experiment, the addition of water vapor increases the transformation of octahedral magnetite to tetrahedral magnetite, thus, facilitating the formation of hematite from magnetite.…”
Section: Fe-containing Phases Of Ashes Produced From Dtf Experimentssupporting
confidence: 89%
“… 33 On the one hand, water vapor replaces part of the dilute CO 2 gas, and O 2 diffusion is faster in H 2 O. 34 Thus, molecular O 2 is more likely to reach the surface of combustion particles and be in close contact with iron minerals in coal to form more iron oxides during the short residence time in the DTF chamber. On the other hand, the combustion particles are more easily fragmented as more oxygen diffuses to the particle surface making it greatly difficult for iron-bearing minerals to be in contact with clay or other silicates included in the particles to form Fe-glass.…”
Section: Resultsmentioning
confidence: 99%
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“…In the past decade, the research group at the State Key Laboratory of Coal Combustion has conducted a series of studies on the effects of CO 2 and H 2 O on pyrite transformation, shedding more light on the effects of oxyfuel combustion. Thermogravimetric analyses showed that pure pyrite behaved kinetically different in CO 2 and N 2 in the range of 948–1073 K, although the decomposition solid products had similar mineralogy.…”
Section: Transformation Of Mineral Mattermentioning
confidence: 99%
“…10). It can be expected that reactions (9) and (10) [45]. As a result, the interaction between minerals (CaO, Al 2 O 3 and SiO 2 ) was promoted and more gehlenite was generated.…”
Section: Morphological Characterization and Mineral Compositionsmentioning
confidence: 99%