Influence of oxygen partial pressure on crystallization behaviour and high-temperature stability of stone wool fibres

dc.bibliographicCitation.firstPage63
dc.bibliographicCitation.journalTitleGlass Science and Technologyeng
dc.bibliographicCitation.lastPage68
dc.bibliographicCitation.volume78
dc.contributor.authorKaasgaard, Martin
dc.contributor.authorJacobsen, Peter A. L.
dc.contributor.authorYue, Yuanzheng
dc.date.accessioned2023-12-15T15:29:13Z
dc.date.available2023-12-15T15:29:13Z
dc.date.issued2005
dc.description.abstractThe influence of oxygen partial pressure on the redox State of the iron in stone wool is studied using thermogravimetry (TG). The thermal response of the stone wool is measured using differential scanning calorimetry (DSC). The high-temperature stability of stone wool depending on the oxygen partial pressure is observed using scanning electron microscopy (SEM). It is confirmed that the oxidation of Fe2+ to Fe3+ is responsible for the high-temperature stability of stone wool. Even a minor increase in oxygen partial pressure can considerably alter the crystallization behaviour and enhance the high-temperature stability of the stone wool. The origin for that is discussed.eng
dc.description.versionpublishedVersion
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/13895
dc.identifier.urihttps://doi.org/10.34657/12925
dc.language.isoeng
dc.publisherOffenbach : Verlag der Deutschen Glastechnischen Gesellschaft
dc.relation.issn0946-7475
dc.rights.licenseCC BY 3.0 DE
dc.rights.urihttps://creativecommons.org/licenses/by/3.0/de/
dc.subject.ddc660
dc.titleInfluence of oxygen partial pressure on crystallization behaviour and high-temperature stability of stone wool fibreseng
dc.typeArticleeng
dc.typeTexteng
tib.accessRightsopenAccess
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