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Tracing electron density changes in langbeinite under pressure

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cris.lastimport.scopus2024-02-12T19:46:14Z
dc.abstract.enPressure is well known to dramatically alter physical properties and chemical behaviour of materials, much of which is due to the changes in chemical bonding that accompany compression. Though it is relatively easy to comprehend this correlation in the discontinuous compression regime, where phase transformations take place, understanding of the more subtle continuous compression effects is a far greater challenge, requiring insight into the finest details of electron density redistribution. In this study, a detailed examination of quantitative electron density redistribution in the mineral langbeinite was conducted at high pressure. Langbeinite is a potassium magnesium sulfate mineral with the chemical formula [K2Mg2(SO4)3], and crystallizes in the isometric tetartoidal (cubic) system. The mineral is an ore of potassium, occurs in marine evaporite deposits in association with carnallite, halite and sylvite, and gives its name to the langbeinites, a family of substances with the same cubic structure, a tetrahedral anion, and large and small cations. Single-crystal X-ray diffraction data for langbeinite have been collected at ambient pressure and at 1 GPa using a combination of in-house and synchrotron techniques. Experiments were complemented by theoretical calculations within the pressure range up to 40 GPa. On the basis of changes in structural and thermal parameters, all ions in the langbeinite structure can be grouped into `soft' (potassium cations and oxygens) and `hard' (sulfur and magnesium). This analysis emphasizes the importance of atomic basins as a convenient tool to analyse the redistribution of electron density under external stimuli such as pressure or temperature. Gradual reduction of completeness of experimental data accompanying compression did not significantly reduce the quality of structural, electronic and thermal parameters obtained in experimental quantitative charge density analysis.
dc.affiliationUniwersytet Warszawski
dc.contributor.authorWoźniak, Krzysztof
dc.contributor.authorGajda, Roman
dc.contributor.authorDera, Przemysław
dc.contributor.authorParafiniuk, Jan
dc.contributor.authorZhang, Dongzhou
dc.date.accessioned2024-01-26T11:04:33Z
dc.date.available2024-01-26T11:04:33Z
dc.date.issued2022
dc.description.accesstimeAT_PUBLICATION
dc.description.financeŚrodki finansowe, o których mowa w art. 365 pkt. 2 ustawy
dc.description.number1
dc.description.versionOTHER
dc.description.volume9
dc.identifier.doi10.1107/S2052252521012628
dc.identifier.urihttps://repozytorium.uw.edu.pl//handle/item/123628
dc.identifier.weblinkhttp://journals.iucr.org/m/issues/2022/01/00/ti5023/ti5023.pdf
dc.languageeng
dc.pbn.affiliationearth and related environmental sciences
dc.relation.ispartofIUCrJ
dc.relation.pages146-162
dc.rightsCC-BY
dc.sciencecloudnosend
dc.subject.enhigh pressure
dc.subject.enelectron density
dc.subject.entheoretical structure factors
dc.titleTracing electron density changes in langbeinite under pressure
dc.typeJournalArticle
dspace.entity.typePublication