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Effect of Ti4+ on the structure of nepheline (NaAlSiO4) glass

Authors :
Emily T. Nienhuis
Charles Le Losq
José Marcial
Daniel R. Neuville
Thibaut Robine
John S. McCloy
Martin C. Stennett
Neil C. Hyatt
Washington State University (WSU)
Pacific Northwest National Laboratory (PNNL)
Institut de Physique du Globe de Paris (IPGP)
Institut national des sciences de l'Univers (INSU - CNRS)-IPG PARIS-Université de La Réunion (UR)-Centre National de la Recherche Scientifique (CNRS)-Université de Paris (UP)
University of Sheffield [Sheffield]
Source :
Geochimica et Cosmochimica Acta, Geochimica et Cosmochimica Acta, Elsevier, 2020, 290, pp.333-351. ⟨10.1016/j.gca.2020.09.015⟩
Publication Year :
2020
Publisher :
Elsevier BV, 2020.

Abstract

International audience; In this study, the effect of Ti 4+ on the structure of nepheline glass (NaAlSiO 4) is investigated as SiO 2 is systematically replaced with TiO 2. Traditionally, TiO 2 is considered to be a nucleating agent for silicate crystallization but can also be incorporated into the glass network in relatively large amounts as either a network former or modifier depending on its coordination with oxygen. To determine the effect of Ti 4+ on the structure of nepheline glass, X-ray and neutron pair distribution function (PDF) analysis paired with Empirical Potential Structure Refinement (EPSR) were conducted and are supplemented with Raman spectroscopy, electron probe microanalysis, and X-ray absorption spectroscopy (including Extended X-ray Absorption Fine Structure, EXAFS). Through these methods, it has been found that up to 15 mol% (16 wt%) TiO 2 can incorporate into the glass network as a four-fold coordinated species, with a minor contribution of higher coordinated Ti. Between NaAlTi 0.1 Si 0.9 O 4 and NaAlTi 0.2 Si 0.8 O 4 , EXAFS suggests a local structure change in the second coordination sphere of Ti, which changes from Ti-Ti to Ti-Al. Raman spectroscopy also suggests that as Ti content increases, the Na environment becomes more ordered. These results suggest that the Ti activity coefficient and its isotopic fractionation for magnetite and other Ti-bearing minerals should be fairly constant in polymerized melts, such as metaluminous and peraluminous rhyolites.

Details

ISSN :
00167037
Volume :
290
Database :
OpenAIRE
Journal :
Geochimica et Cosmochimica Acta
Accession number :
edsair.doi.dedup.....31fbcef5ca487d284877933313fbc13f
Full Text :
https://doi.org/10.1016/j.gca.2020.09.015