1. The hydrocarbon-bearing clathrasil chibaite and its host-guest structure at low temperature.
- Author
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Scheidl KS, Effenberger HS, Yagi T, Momma K, and Miletich R
- Abstract
The natural sII-type clathrasil chibaite [chemical formula SiO
2 ·( M12 , M16 ), where Mx denotes a guest mol-ecule] was investigated using single-crystal X-ray diffraction and Raman spectroscopy in the temperature range from 273 to 83 K. The O atoms of the structure at room temperature, which globally conforms to space group [ V = 7348.9 (17) Å3 , a = 19.4420 (15) Å], have anomalous anisotropic displacement parameters indicating a static or dynamic disorder. With decreasing temperature, the crystal structure shows a continuous symmetry-lowering transformation accompanied by twinning. The intensities of weak superstructure reflections increase as temperature decreases. A monoclinic twinned superstructure was derived at 100 K [ A 2/ n , V = 7251.0 (17) Å3 , a ' = 23.7054 (2), b ' = 13.6861 (11), c ' = 23.7051 (2) Å, β' = 109.47°]. The transformation matrix from the cubic to the monoclinic system is ai ' = (½ 1 ½ / ½ 0 -½ / ½ -1 ½). The A 2/ n host framework has Si-O bond lengths and Si-O-Si angles that are much closer to known values for stable silicate-framework structures compared with the averaged model. As suggested from band splitting observed in the Raman spectra, the [512 ]-type cages (one crystallographically unique in , four different in A 2/ n ) entrap the hydro-carbon species (CH4 , C2 H6 , C3 H8 , i -C4 H10 ). The [512 64 ]-type cage was found to be unique in both structure types. It contains the larger hydro-carbon mol-ecules C2 H6 , C3 H8 and i -C4 H10 .- Published
- 2018
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