THE CRYSTAL CHEMISTRY OF SYNTHETIC POTASSIUM-BEARING NEIGHBORITE, (NA1-x Kx)MGF3
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dc.contributor.author | Chakhmouradian A.R. | |
dc.contributor.author | Ross K. | |
dc.contributor.author | Mitchell R.H. | |
dc.contributor.author | Swainson I. | |
dc.date.accessioned | 2021-03-30T10:40:26Z | |
dc.date.available | 2021-03-30T10:40:26Z | |
dc.date.issued | 2001 | |
dc.identifier | https://www.elibrary.ru/item.asp?id=872482 | |
dc.identifier.citation | Physics and Chemistry of Minerals, 2001, 28, 4, 277-284 | |
dc.identifier.issn | 0342-1791 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/27156 | |
dc.description.abstract | A series of fluoride perovskites related to neighborite was investigated using X-ray and neutron diffraction techniques, and Rietveld profile refinement of powder diffraction data. The series (Na1− x K x )MgF3 comprises orthorhombic (Pbnm, a ≈ , b ≈ , c ≈ 2a p , Z=4) perovskites in the compositional range 0 ≤ x ≤ 0.30, tetragonal perovkites (P4/mbm, a ≈ , c ≈ a p , Z=2) in the range 0.40 ≤ x ≤ 0.46, and cubic phases (Pm3¯m, Z=1) for x > 0.50. The structure of the orthorhombic neighborite is derived from the perovskite aristotype by rotation of MgF6 octahedra about the [110] and [001] axes of the cubic subcell. The degree of rotation, measured as a composite tilt Φ about the triad axis, varies from 18.2° at x=0 to 11.2° at x=0.30 (as determined from the fractional atomic coordinates). Orthorhombic neighborite also shows a significant displacement of Na and K from the “ideal” position (≤0.25 Å). The tetragonal members of the neighborite series exhibit only in-phase tilting about the [001] axis of the cubic subcell (φ) ranging from 4.5° to 4.8° (determined from the atomic coordinates). The solid solution (Na1− x K x )MgF3, shows a regular variation of unit-cell dimensions with composition from 3.8347 Å for the end-member NaMgF3 (reduced to pseudocubic subcell, a p ) to 3.9897 Å for KMgF3. This variation is accompanied by increasing volumes of the A-site polyhedra, whereas the volume of MgF6 octahedra initially decreases (up to x=0.40), and then increases concomitantly with K content. The polyhedral volume ratio, V A /V B , gradually increases towards the tetragonal structural range, in agreement with diminishing octahedral rotation in the structure. The P4/mbm-type neighborite has an “anomalous” polyhedral volume ratio (ca. 5.04) owing to the critical compression of MgF6 polyhedra. | |
dc.subject | PEROVSKITE | |
dc.subject | NEIGHBORITE | |
dc.subject | CRYSTAL STRUCTURE | |
dc.subject | PHASE TRANSITION | |
dc.title | THE CRYSTAL CHEMISTRY OF SYNTHETIC POTASSIUM-BEARING NEIGHBORITE, (NA1-x Kx)MGF3 | |
dc.type | Статья |
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