2012
DOI: 10.1007/s11814-012-0176-z
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Mineral behavior of low-temperature lignite ashes under gasification atmosphere

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Cited by 13 publications
(1 citation statement)
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“…Moreover, Jing et al [ 11 ] studied the impact of pressure on the fusibility of ash and concluded that the interactions among different mineral matters were also dependent on the reaction atmosphere at elevated pressure. Li et al [ 12 ] examined the ash obtained from the reducing atmosphere at different pressures and stated that with increasing pressure, the decompositions of muscovite and calcite were restrained, whereas the formations of orthoclase and iron minerals were enhanced. In our previous work, [ 13 ] the experimental results revealed that as the pressure increased, the high‐temperature minerals (eg, mullite) in the ash disappeared and some low‐temperature minerals (eg, calcite) were found in the ash.…”
Section: Introductionmentioning
confidence: 99%
“…Moreover, Jing et al [ 11 ] studied the impact of pressure on the fusibility of ash and concluded that the interactions among different mineral matters were also dependent on the reaction atmosphere at elevated pressure. Li et al [ 12 ] examined the ash obtained from the reducing atmosphere at different pressures and stated that with increasing pressure, the decompositions of muscovite and calcite were restrained, whereas the formations of orthoclase and iron minerals were enhanced. In our previous work, [ 13 ] the experimental results revealed that as the pressure increased, the high‐temperature minerals (eg, mullite) in the ash disappeared and some low‐temperature minerals (eg, calcite) were found in the ash.…”
Section: Introductionmentioning
confidence: 99%