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dc.contributor.authorAarnæs, Trygve Storm
dc.contributor.authorRingdalen, Eli
dc.contributor.authorTangstad, Merete
dc.date.accessioned2022-05-03T08:55:48Z
dc.date.available2022-05-03T08:55:48Z
dc.date.created2021-01-07T15:26:06Z
dc.date.issued2020
dc.identifier.citationScientific Reports 2020, 10 (1), 21831, 11.en_US
dc.identifier.issn2045-2322
dc.identifier.urihttps://hdl.handle.net/11250/2993802
dc.description.abstractSilicon carbide (SiC) formation plays an important role during the production of elemental silicon. SiC forms through a high temperature reaction between silicon monoxide gas (SiO) and carbon. Currently, the carbon sources are solids, however finding a way of substituting the solid carbon with methane could have several advantages. SiC formation was studied in argon, hydrogen and methane containing atmospheres at 1650 °C and 1750 °C. SiO gas was generated from pellets of a 1:2 molar ratio of SiC and silica (SiO2). The reactions were investigated through CO off-gas analysis in conjunction with measuring the weight change. After each experiment, the reaction products were examined in a scanning electron microscope with secondary electrons and through energy-dispersive X-ray spectroscopy. It was confirmed that SiC may form from SiO and methane. Increasing the methane content to 5% caused a significant increase in SiC formation. Furthermore, the SiC structure was also highly sensitive to the methane content that was used. In addition, the SiO producing reaction was affected by hydrogen. The hydrogen lead to an increased rate of SiO formation relative to what was seen in argon. The effect of hydrogen was most pronounced at 1750 °C which is right after the melting of silica.en_US
dc.language.isoengen_US
dc.publisherSpringer Natureen_US
dc.rightsNavngivelse 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no*
dc.titleSilicon carbide formation from methane and silicon monoxideen_US
dc.typePeer revieweden_US
dc.typeJournal articleen_US
dc.description.versionpublishedVersionen_US
dc.rights.holder© The Author(s) 2020.en_US
dc.source.pagenumber11en_US
dc.source.volume10en_US
dc.source.journalScientific Reportsen_US
dc.source.issue1en_US
dc.identifier.doi10.1038/s41598-020-79006-6
dc.identifier.cristin1867240
dc.relation.projectNorges forskningsråd: 280968en_US
dc.source.articlenumber21831en_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1


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