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dc.contributor.authorGawel, Bartlomiej
dc.contributor.authorUlvensøen, Anna
dc.contributor.authorLukaszuk, Katarzyna Anna
dc.contributor.authorArstad, Bjørnar
dc.contributor.authorMuggerud, Astrid Marie Flattum
dc.contributor.authorErbe, Andreas
dc.identifier.citationRSC Advances. 2020, 10 29018-29030.en_US
dc.description.abstractFused silica crucibles are commonly used in the fabrication process of solar grade silicon ingots. These crucibles are manufactured from high purity natural quartz sand and as a consequence, their properties are influenced by the presence of water and hydroxyls in the raw quartz. In this work, diffuse reflectance IR, 1H magic angle spinning NMR, and Raman spectroscopy were used to investigate the influence of thermal treatment on water and hydroxyl groups in high purity natural quartz sand. Most of the water in dry sand is present in the form of closed inclusions within the quartz grains which were detected in Raman imaging studies, even after thermally treating the samples at 600 °C. Only after heating to 900 °C did this water completely vanish, most likely as a result of rupturing of the inclusions. However, newly formed OH groups, identified as isolated and hydrogen bound OH were observed as products of the reaction between water and quartz. Similarly, liquid water was observed in NMR spectra even after treatment at 600 °C while at temperatures >900 °C, only non-interacting silanol groups were present. The comparison of the temperature dependence of the IR and NMR spectra also yields insight into the assignment of the OH stretching mode region of the IR spectrum in this system. The intensity of water related bands decreases while the intensity of OH bands first increases and then decreases with increasing temperature. The band intensity of Al-rich defects as well as the characteristic feature at 3200 cm−1 does not follow the temperature dependence of typical water peaks. It is also shown that leaching the quartz sand in HF solution helps to remove water from inclusions, likely by forming pathways for fluid flow inside the quartz grains. Milling of the samples caused formation of an additional type of hydroxyl group, possibly due to partial amorphisation of the surfaces of the quartz grains surface during the process. The results improve the basis for a knowledge-based processes development for the processing of high purity natural quartz.en_US
dc.publisherRoyal Society of Chemistryen_US
dc.rightsNavngivelse 4.0 Internasjonal*
dc.subjectFused silica cruciblesen_US
dc.subjectthermal treatmenten_US
dc.titleStructural evolution of water and hydroxyl groups during thermal, mechanical and chemical treatment of high purity natural quartzen_US
dc.typePeer revieweden_US
dc.typeJournal articleen_US
dc.rights.holderThis article is open access CC-BY.en_US
dc.source.journalRSC Advancesen_US
dc.relation.projectNorges forskningsråd: 282341en_US

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Navngivelse 4.0 Internasjonal
Except where otherwise noted, this item's license is described as Navngivelse 4.0 Internasjonal