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dc.contributor.authorSyvertsen, Martin
dc.contributor.authorKvithyld, Anne
dc.contributor.authorGundersen, Eilif
dc.contributor.authorJohansen, Inge
dc.contributor.authorEngh, Thorvald Abel
dc.date.accessioned2020-03-20T10:04:53Z
dc.date.available2020-03-20T10:04:53Z
dc.date.created2019-07-02T13:52:18Z
dc.date.issued2019
dc.identifier.citationThe Minerals, Metals & Materials Series. 2019, 1051-1056.en_US
dc.identifier.issn2367-1181
dc.identifier.urihttps://hdl.handle.net/11250/2647754
dc.description.abstractHydrogen solubility is much higher in liquid than in solid aluminium. Therefore, if the hydrogen concentration in liquid aluminium is too high prior to solidification, there is high risk of gas porosity formation during the solidification. In a gas or oil fired reverberatory furnace for aluminium, combustion produces large amounts of water vapour. The water vapour may react with aluminium forming aluminium oxide and hydrogen gas. This hydrogen gas is then the main source for hydrogen in molten aluminium. Measurements of both water vapour in the furnace atmosphere (combustion off-gas) and dissolved hydrogen in the melt are presented. The measurements are compared to a model for hydrogen concentration in aluminium as function of the measured water vapour concentration. It is concluded that H2O reacts with aluminium to H2 and Al2O3. 49% of this H2 escapes from the interface to the bulk gas phase, and 51% acts as a source for dissolved hydrogen in the melt.en_US
dc.language.isoengen_US
dc.publisherSpringeren_US
dc.titleFurnace Atmosphere and Dissolved Hydrogen in Aluminiumen_US
dc.typePeer revieweden_US
dc.typeJournal articleen_US
dc.description.versionacceptedVersionen_US
dc.source.pagenumber1051-1056en_US
dc.source.journalThe Minerals, Metals & Materials Seriesen_US
dc.identifier.doi10.1007/978-3-030-05864-7_128
dc.identifier.cristin1709423
dc.relation.projectNorges forskningsråd: 269634en_US
dc.description.localcodeCopyright © 2019, The Minerals, Metals & Materials Society. This is a post-peer-review, pre-copyedit version of an article. The final authenticated version is available online at: 10.1007/978-3-030-05864-7_128en_US
cristin.ispublishedtrue
cristin.fulltextpostprint
cristin.qualitycode1


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