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dc.contributor.authorMare, Eleanor Rose
dc.contributor.authorO'Neill, Hugh
dc.contributor.authorBerry, Andrew
dc.contributor.authorFrigo, Corinne
dc.contributor.authorGlover, Chris
dc.date.accessioned2022-03-16T00:41:12Z
dc.date.available2022-03-16T00:41:12Z
dc.date.issued2021-03-16
dc.identifier.citationMare , E R , O'Neill , H , Berry , A , Frigo , C & Glover , C 2021 , ' Coordination change of Ge 4+ and Ga 3+ in silicate melt with pressure ' , Geochimica et Cosmochimica Acta , vol. In press . https://doi.org/10.1016/j.gca.2021.03.008en
dc.identifier.issn0016-7037
dc.identifier.otherPURE: 273217964
dc.identifier.otherPURE UUID: ec3fc74b-bc47-41e1-b5aa-20eeda59e029
dc.identifier.otherORCID: /0000-0003-0531-7755/work/90952296
dc.identifier.otherWOS: 000651801700010
dc.identifier.otherScopus: 85104356281
dc.identifier.urihttp://hdl.handle.net/10023/25054
dc.descriptionHON thanks the Australian Research Council for funding through grant FL130100066. ERM acknowledges an Australian Government Research Training Program Scholarship (formerly Australian Postgraduate Award).en
dc.description.abstractThe coordination environments of ∼ 2000 ppm Ge4+ and Ga3+ in silicate glasses of three compositions based on the CaO-MgO-Al2O3-SiO2 (CMAS) system were determined as a function of pressure by X-ray absorption near edge structure (XANES) spectroscopy. Glasses of 11 additional compositions were examined to check for any effect of composition on coordination at low pressure (1 atm to 1 GPa). Glasses were synthesised at pressures from 1 atm to 10 GPa using either a melt-quench method or glass-annealing method (annealing near the glass transition temperature, ∼780 °C). The glasses also contained H2O and CO2, which were quantified by attenuated total reflectance infrared spectroscopy, using an estimated density-normalised calibration factor for CO2. While changes in average coordination number are sensitively monitored by the changes in the XANES spectra, quantification of these changes requires assuming that the XANES spectra of crystalline substances of known structure provide analogues for the glasses. Linear combination fits of the spectra using the crystalline analogues indicate that the average coordination numbers of Ge4+ and Ga3+ increase from 4 at ambient pressure to approximately 5 at 10 GPa. Ge4+ and Ga3+ have higher average coordination numbers in annealed glasses compared to those from quenched melts prepared at the same pressure up to 4 GPa, but at 5–6 GPa quenched melts and annealed glasses record similar coordination numbers. Coordination changes occur at lower pressures in more depolymerised melt compositions, and are therefore relevant to natural melts of the mantle. The partition coefficients of Ge and Ga between melts and coexisting minerals are likely to be affected by such coordination changes.
dc.language.isoeng
dc.relation.ispartofGeochimica et Cosmochimica Actaen
dc.rightsCopyright © 2021 Elsevier Ltd. This work has been made available online in accordance with publisher policies or with permission. Permission for further reuse of this content should be sought from the publisher or the rights holder. This is the author created accepted manuscript following peer review and may differ slightly from the final published version. The final published version of this work is available at https://doi.org/10.1016/j.gca.2021.03.008en
dc.subjectGermaniumen
dc.subjectGalliumen
dc.subjectXANESen
dc.subjectFictive temperatureen
dc.subjectFictive pressureen
dc.subjectGE Environmental Sciencesen
dc.subjectDASen
dc.subject.lccGEen
dc.titleCoordination change of Ge4+ and Ga3+ in silicate melt with pressureen
dc.typeJournal articleen
dc.description.versionPostprinten
dc.contributor.institutionUniversity of St Andrews. School of Earth & Environmental Sciencesen
dc.identifier.doihttps://doi.org/10.1016/j.gca.2021.03.008
dc.description.statusPeer revieweden
dc.date.embargoedUntil2022-03-16


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