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  • 1
    ISSN: 0899-0042
    Keywords: quartz crystal microbalance ; electronic nose ; fragrance ; odour ; detection ; chemical sensor ; cyclodextrin ; chiral discrimination ; Chemistry ; Organic Chemistry
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology
    Notes: Quartz crystal microbalances (QCMB) have been constructed using 10 MHz AT cut quartz crystals coated with heptakis(2,3,6-tri-O-methyl)-β-cyclodextrin, heptakis(6-O-methyl-2,3-di-O-pentyl)-β-cyclodextrin, and octakis(6-O-methyl-2,3-di-O-pentyl)-γ-cyclodextrin as 50% and 20% (w/w) solutions in OV1701. The reduction in frequency seen on exposure of each coated QCMB to pure enantiomeric forms of α- and β-pinene and cis- and trans-pinane show that statistically significant (P = 0.05, n = 7) differences are observed between the enantiomeric pairs. The apparent preferential binding shown by the QCMB for enanciomers of α- and β-pinene and cis- and trans-pinane have been compared with the elution order observed on the corresponding gas chromatographic stationary phase. The magnitude of the observed separation factor (calculated as the ratio of the OV1701 normalised frequency shift) is seen to be dependent upon the chiral stationary phase concentration. These results indicate that on-line determination of enantiomeric excess and concentration of certain monoterpenes is possible at room temperature using QCMB in conjunction with chiral gas chromatographic stationary phases. Chirality 9:225-232, 1997. © 1997 Wiley-Liss, Inc.
    Additional Material: 3 Ill.
    Type of Medium: Electronic Resource
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  • 2
    Publication Date: 2013-08-31
    Description: Northern Europe has an assemblage of Ordovician probable impacts that is exceptional because the structures involved are relatively old yet well preserved because they formed at sea and because they formed within a restricted geological time in a relatively small area. The Tvaren, Kardla, and Lockne structures might not be strictly contemporaneous but all formed near the beginning of the Caradoc Age (about 460 Ma), whereas the Granby structure is about 20 Ma older. The range of diameters is from about 2 km (Tvaren, Granby) to 8 km (Lockne). The stratigraphic succession formed on impact at sea, as uniformly documented by these structures, begins with a breccia lens consisting of basement rocks that are intensely crushed. Owing to expulsion of sea water by the impact, this breccia formed under essentially dry conditions. Later on this breccia was in part hydrothermally altered. It is overlain by backsurge turbidite that formed from fragments of local sedimentary bedrock and crystalline basement when the sea water returned to the crater site. Either the turbidite is simply a Bouma sequence (although quite thick - as much as over 50 m) from very coarse rubble to mud, or it is more complex. After deposition of the backsurge turbidite, or turbidite complex, the craters still remained as 150-200-m-deep holes in the sea bed. Together with the presence of relatively shallow water over the rim wall, this situation created predictable hydrologic conditions for extended histories of sedimentation and biological development at the crater as well as within it. The presence of a concentration of craters within a limited area of well-preserved and accessible Ordovician deposits raises a question about the Ordovician, especially its middle portion, as potentially an age of relatively intense impact activity even in wider areas. In this connection it may be apposite to mention that the only fossil stony meteorites so far recorded in rocks are from the late Early and the Middle Ordovician.
    Keywords: GEOPHYSICS
    Type: Lunar and Planetary Inst., International Conference on Large Meteorite Impacts and Planetary Evolution; p 47
    Format: application/pdf
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