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<div class="csl-entry">Missen, O. P., Mills, S. J., Canossa, S., Hadermann, J., Nénert, G., Weil, M., Libowitzky, E., Housley, R., Artner, W., Kampf, A. R., Rumsey, M., Spratt, J., Momma, K., & Dunstan, M. A. (2022). Polytypism in mcalpineite: a study of natural and synthetic Cu₃TeO₆. <i>Acta Crystallographica Section B: Structural Science, Crystal Engineering and Materials</i>, <i>78</i>(Part 1), 20–32. https://doi.org/10.1107/S2052520621013032</div>
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dc.identifier.issn
2052-5206
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dc.identifier.uri
http://hdl.handle.net/20.500.12708/142271
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dc.description.abstract
Synthetic and naturally occurring forms of tricopper orthotellurate, CuII₃TeVIO₆ (the mineral mcalpineite) have been investigated by 3D electron diffraction (3D ED), X-ray powder diffraction (XRPD), Raman and infrared (IR) spectroscopic measurements. As a result of the diffraction analyses, CuII₃TeVIO₆ is shown to occur in two polytypes. The higher-symmetric CuII₃TeVIO₆ -1C polytype is cubic, space group Ia3, with a = 9.537 (1) Å and V = 867.4 (3) Å3 as reported in previous studies. The 1C polytype is a well characterized structure consisting of alternating layers of CuIIO6 octahedra and both CuIIO6 and TeVIO6 octahedra in a patchwork arrangement. The structure of the lower-symmetric orthorhombic CuII₃TeVIO₆ -2O polytype was determined for the first time in this study by 3D ED and verified by Rietveld refinement. The 2O polytype crystallizes in space group Pcca, with a = 9.745 (3) Å, b = 9.749 (2) Å, c = 9.771 (2) Å and V = 928.3 (4) Å3. High-precision XRPD data were also collected on CuII₃TeVIO₆ -2O to verify the lower-symmetric structure by performing a Rietveld refinement. The resultant structure is identical to that determined by 3D ED, with unit-cell parameters a = 9.56157 (19) Å, b = 9.55853 (11) Å, c = 9.62891 (15) Å and V = 880.03 (2) Å3. The lower symmetry of the 2O polytype is a consequence of a different cation ordering arrangement, which involves the movement of every second CuIIO6 and TeVIO6 octahedral layer by (1/4, 1/4, 0), leading to an offset of TeVIO6 and CuIIO6 octahedra in every second layer giving an ABAB* stacking arrangement. Syntheses of CuII₃TeVIO₆ showed that low-temperature (473 K) hydrothermal conditions generally produce the 2O polytype. XRPD measurements in combination with Raman spectroscopic analysis showed that most natural mcalpineite is the orthorhombic 2O polytype. Both XRPD and Raman spectroscopy measurements may be used to differentiate between the two polytypes of CuII₃TeVIO₆ . In Raman spectroscopy, CuII₃TeVIO₆ -1C has a single strong band around 730 cm-1, whereas CuII₃TeVIO₆ -2O shows a broad double maximum with bands centred around 692 and 742 cm-1.
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dc.language.iso
en
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dc.publisher
INT UNION CRYSTALLOGRAPHY
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dc.relation.ispartof
Acta Crystallographica Section B: Structural Science, Crystal Engineering and Materials
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dc.subject
Powder Diffraction
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dc.subject
Spectrophotometry, Infrared
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dc.subject
X-Ray Diffraction
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dc.subject
3D ED
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dc.subject
copper
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dc.subject
crystal structure
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dc.subject
mcalpineite
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dc.subject
polytypes
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dc.subject
tellurate
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dc.subject
Electrons
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dc.subject
Spectrum Analysis, Raman
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dc.title
Polytypism in mcalpineite: a study of natural and synthetic Cu₃TeO₆