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dc.contributor.authorMangena, S.J.
dc.contributor.authorBunt, J.R.
dc.contributor.authorWaanders, F.B.
dc.date.accessioned2015-05-29T09:28:09Z
dc.date.available2015-05-29T09:28:09Z
dc.date.issued2013
dc.identifier.citationMangena, S.J. et al. 2013. Mineralogical behaviour of North Dakota lignite in an oxygen/steam blown moving bed reactor. Fuel processing technology, 106:474-482. [https://doi.org/10.1016/j.fuproc.2012.09.015]en_US
dc.identifier.issn0378-3820
dc.identifier.urihttp://hdl.handle.net/10394/13873
dc.identifier.urihttps://doi.org/10.1016/j.fuproc.2012.09.015
dc.identifier.urihttps://www.sciencedirect.com/science/article/pii/S0378382012003311
dc.description.abstractIn this study, lignite fromNorth Dakota (USA)was thermally treated in a commercial-scale oxygen/steamblown moving bed reactor at the Dakota Gasification Conpany (DGC) in order to identify mineralogical changes that occur during the conversion process. After reaction, the solid particulate remnants were extracted from the reactor reaction zones and characterised using XRD, CCSEM and SEMPC techniques. It was found that the feed coal mineralization was mainly dominated by organically bound calcium. On the other hand, the crystalline phases present in the hottest regions of the reactor were governed by gehlenite and bredigite which may have formed from the transformation, (at higher temperatures), of the organically bound Ca and Mg to form CaO and MgO and subsequent interaction with the reactive silica and transformation products of the clays. A significant amount of calcitewas found to develop at the start of the reduction zone; it is suggested that the calcitewas synthesised fromthe reaction of CaO (formed fromthe transformation of the organically bound Ca)with the CO2 from the product gas in the reactor, in agreementwith the literature. The glass phase was found to constitute the major part of the ash mineral assemblage in the reduction and combustion zones of the reactor. This phase was composed mainly of the Ca, Mg, Na aluminosilicates with some Fe. There was therefore a significant amount of melting that occurred in the hotter reaction zones (i.e. reduction and combustion zones) of the reactor. The organically bound Ca, Mg and Na seemed to have played a significant role in the formation of this glass phase.en_US
dc.language.isoenen_US
dc.publisherElsevieren_US
dc.subjectMoving-bed gasificationen_US
dc.subjectcoalen_US
dc.subjectmineralogyen_US
dc.subjectXRDen_US
dc.subjectCCSEMen_US
dc.subjectSEMPCen_US
dc.titleMineralogical behaviour of North Dakota lignite in an oxygen/steam blown moving bed reactoren_US
dc.typeArticleen_US
dc.contributor.researchID20164200 - Bunt, John Reginald
dc.contributor.researchID10059571 - Waanders, Frans Boudewijn


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