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  • Inorganic Chemistry  (2)
  • 157-1; 204-1247B; 204-1248C; 204-1249C; 204-1250C; Bush Hill; Center for Marine Environmental Sciences; Comment; Crystal size; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Elevation of event; Event label; Joides Resolution; Latitude of event; Leg204; Location scan method; Longitude of event; MARUM; North Pacific Ocean; OTEGA II; Sample code/label; SO174/2; SO174/2_157-1; Sonne; Standard deviation; Television-Grab; TVG  (1)
  • Fluorosilicates, zwitterionic
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  • 1
    ISSN: 0009-2940
    Keywords: Spirosilicates, zwitterionic ; Silicon, pentacoordinate ; Bond cleavage, Si - C ; Solid-state NMR, 29Si and 15N ; Chemistry ; Inorganic Chemistry
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology
    Notes: New Zwitterionic λ51-Spirosilicates: Syntheses, Single-Crystal X-Ray Structure Analyses, and Solid-State NMR StudiesThe zwitterionic spirocyclic λ51-silicates bis[3,4,5,6-tetrabromo-1,2-benzenediolato(2-)][2-(pyrrolidinio)ethyl]silicate (5; and its monohydrate 5 · H2O) and bis[1,2-benzenediolato(2-)]1-[(dimethylammonio)methyl]silicate (6) were synthesized by various methods including Si - C bond cleavage reactions. The crystal structures of 5, 5·H2O, and 6 were investigated by X-ray diffarction. Furthermore, 5, 5·H2O, 6, and the related zwitterionic λ51-spirosilicates 1·1/4 CH3CN, 2·CH3CN, 3·CH3CN, and 4 were characterized by solid-state NMR spectroscopy (29Si and 15N CP/MAS). The pentacoordinate silicon atoms of 5, 5·H2O (two cystallographically independent zwitterions and two crystallographically independent water molecules), and 6 (two crystallographically independent zwitterions) are surrounded by four oxygen atoms and one carbon atom. The coordination polyhedrons around the silicon atoms of 5 and 6 can be described as distorted (5) or nearly ideal (6) trigonal bipyramids, the carbon atoms being in equatorial positions. 5 forms intramolecular and 6 intermolecular (→ for-mation of dimeric units) N - H…O hydrogen bonds. The co-ordination polyhedrons around the two crystallographically independent silicon atoms of 5·H2O can be described as a nearly ideal and slightly distorted square pyramid, respectively, the carbon atoms being in the apical positions. In the crystal lattice of 5·H2O, intermolecular N - H…O O - H…O hydrogen bonds between the zwitterions and water molecules are observed. The results obtained by X-ray diffraction and solid-state NMR spectroscopy are consistent for each compound studied.
    Additional Material: 7 Ill.
    Type of Medium: Electronic Resource
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  • 2
    ISSN: 0009-2940
    Keywords: Fluorosilicates, zwitterionic ; Pentacoordinate silicon ; Chemistry ; Inorganic Chemistry
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology
    Notes: On the Existence of Zwitterionic λ5-(Ammonioorganyl)tetrafluorosilicates: Synthesis and Crystal and Molecular Structure of Tetrafluoro(pyrrolidiniomethyl)silicateThe zwitterionic tetrafluoro(pyrrolidiniomethyl)silicate (6) was synthesized by the reaction of trimethoxy(pyrrolidinomethyl)silane (7) with hydrogen fluoride in ethanol/hydro-fluoric acid (yield 83%). 6 crystallizes in the space group P1/c with two crystallographically distinct molecules in the asymmetric unit. In both molecules the pentacoordinate silicon atom is surrounded by four fluorine atoms and one carbon atom, the latter being in an equatorial position. The coordination polyhedron of the silicon atoms can be described as a slightly distorted trigonal bipyramid. The zwitterionic structure was also proved for dissolved 6 (solution in CD3CN, NMR-spectroscopic studies).
    Additional Material: 1 Ill.
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  • 3
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    In:  Supplement to: Klapp, Stephan A; Klein, Helmut; Kuhs, Werner F (2009): Gas hydrate crystallite size investigations with high-energy synchrotron radiation. In: Long, D; Lovell, MA; Rees, JG; Rochelle, CA (eds.) Sediment-Hosted Gas Hydrates: New Insights on Natural and Synthetic Systems. The London Geological Society, London, Special Publications, London, 319, 161-170, https://doi.org/10.1144/SP319.13
    Publication Date: 2023-06-27
    Description: The grain sizes of gas hydrate crystallites are largely unknown in natural samples. Single grains are hardly detectable with electron or optical microscopy. For the first time, we have used high-energy synchrotron diffraction to determine grain sizes of six natural gas hydrates retrieved from the Bush Hill region in the Gulf of Mexico and from ODP Leg 204 at the Hydrate Ridge offshore Oregon from varying depth between 1 and 101 metres below seafloor. High-energy synchrotron radiation provides high photon fluxes as well as high penetration depth and thus allows for investigation of bulk sediment samples. Gas hydrate grain sizes were measured at the Beam Line BW 5 at the HASYLAB/Hamburg. A 'moving area detector method', originally developed for material science applications, was used to obtain both spatial and orientation information about gas hydrate grains within the sample. The gas hydrate crystal sizes appeared to be (log-)normally distributed in the natural samples. All mean grain sizes lay in the range from 300 to 600 µm with a tendency for bigger grains to occur in greater depth. Laboratory-produced methane hydrate, aged for 3 weeks, showed half a log-normal curve with a mean grain size value of c. 40 µm. The grains appeared to be globular shaped.
    Keywords: 157-1; 204-1247B; 204-1248C; 204-1249C; 204-1250C; Bush Hill; Center for Marine Environmental Sciences; Comment; Crystal size; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Elevation of event; Event label; Joides Resolution; Latitude of event; Leg204; Location scan method; Longitude of event; MARUM; North Pacific Ocean; OTEGA II; Sample code/label; SO174/2; SO174/2_157-1; Sonne; Standard deviation; Television-Grab; TVG
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    Format: text/tab-separated-values, 25 data points
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