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  • 1
    Electronic Resource
    Electronic Resource
    [S.l.] : American Institute of Physics (AIP)
    Review of Scientific Instruments 67 (1996), S. 840-842 
    ISSN: 1089-7623
    Source: AIP Digital Archive
    Topics: Physics , Electrical Engineering, Measurement and Control Technology
    Notes: A new diamond-anvil cell for single-crystal x-ray diffraction structural studies is presented. By including a simple mechanism for adjusting the parallelism of the opposing diamond culets, the stability of the gasket is maintained to higher pressures than was achieved in earlier cells of a similar two-platen design. Equipped with 600 μm culet diamond anvils, the cell has been tested to a pressure of 25 GPa and has been used successfully for equation-of-state measurements and crystal structure determinations to 10 GPa. © 1996 American Institute of Physics.
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  • 2
    Electronic Resource
    Electronic Resource
    Copenhagen : International Union of Crystallography (IUCr)
    Applied crystallography online 30 (1997), S. 461-466 
    ISSN: 1600-5767
    Source: Crystallography Journals Online : IUCR Backfile Archive 1948-2001
    Topics: Geosciences , Physics
    Notes: The unit-cell parameters of quartz, SiO2, have been determined by single-crystal diffraction at 22 pressures to a maximum pressure of 8.9 GPa (at room temperature) with an average precision of 1 part in 9000. Pressure was determined by the measurement of the unit-cell volume of CaF2 fluorite included in the diamond-anvil pressure cell. The variation of quartz unit-cell parameters with pressure is described by: a −4.91300 (11) = −0.0468 (2) P + 0.00256 (7) P2 − 0.000094 (6) P3, c − 5.40482 (17) = − 0.03851 (2) P + 0.00305 (7) P2 − 0.000121 (6) P3, where P is in GPa and the cell parameters are in ångstroms. The volume–pressure data of quartz are described by a Birch–Murnaghan third-order equation of state with parameters V0 = 112.981 (2) å3, KT0 = 37.12 (9) GPa and K′ = 5.99 (4). Refinement of K′′ in a fourth-order equation of state yielded a value not significantly different from the value implied by the third-order equation. The use of oriented quartz single crystals is proposed as an improved internal pressure standard for high-pressure single-crystal diffraction experiments in diamond-anvil cells. A measurement precision of 1 part in 10 000 in the volume of quartz leads to a precision in pressure measurement of 0.009 GPa at 9 GPa.
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  • 3
    Electronic Resource
    Electronic Resource
    Amsterdam : Elsevier
    Physica C: Superconductivity and its applications 209 (1993), S. 415-420 
    ISSN: 0921-4534
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Physics
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  • 4
    Electronic Resource
    Electronic Resource
    Amsterdam : Elsevier
    Physica C: Superconductivity and its applications 185-189 (1991), S. 2501-2502 
    ISSN: 0921-4534
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Physics
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  • 5
    Electronic Resource
    Electronic Resource
    Oxford [u.a.] : International Union of Crystallography (IUCr)
    Acta crystallographica 46 (1990), S. 541-543 
    ISSN: 1600-5759
    Source: Crystallography Journals Online : IUCR Backfile Archive 1948-2001
    Topics: Chemistry and Pharmacology , Geosciences , Physics
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  • 6
    Electronic Resource
    Electronic Resource
    Springer
    Monatshefte für Chemie 126 (1995), S. 417-430 
    ISSN: 1434-4475
    Keywords: Crystal chemistry ; Lone-pair electrons ; Microporous structure ; Na2[Me 2(TeO3)3]·3H2O ; Zemannite type ; Zeolitic properties
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology
    Description / Table of Contents: Zusammenfassung Die Kristallstrukturuntersuchungen mittels Röntgen-Einkristalldiffraktionsmethoden von hydrothermal dargestelltem Na2[Zn2(TeO3)3]·3H2O (NZT) und Na2[Co2(TeO3)3]·3H2O (NCT) ergaben eine zeolithartige Gerüststruktur hexagonaler Symmetrie mit parallel zur c-Achse angeordneten röhrenartigen Kanälen (Zemannittyp). Die statistisch besetzten Punktlagen der Na+-Atome und H2O Moleküle innerhalb der Kanäle wie auch die Kanaldimensionen selbst weisen auf mögliche zeolithische Eigenschaften der Verbindungen hin. Thermoanalytische Untersuchungen anNZT ergaben einen irreversiblen Zusammenbruch der Gerüststruktur bereits beiT=533 K durch vollständige Entwässerung. Eine reversible Rehydratisierung wurde nur für partiell entwässertesNZT (T⩽493 K) beobachtet; ein nennenswerter Ionenaustausch aus Alkalichlorid-Lösungen konnte nur für Li+ bestimmt werden. Sowohl die Rehydratisierung als auch das Ionenaustauschvermögen sind durch relativ lange Reaktionszeiten charakterisiert. Die im Vergleich zu typisch zeolithischen Verbindungen relativ schlechten zeolithischen Eigenschaften konnten auf die stereochemische Aktivität der einsamen Elektronenpaare der Te4+ Atome zurüchgefürt werden, die einen gewissen Platz innerhalb der Kanäle beanspruchen und den effektiven freien Durchmesser der Kanäle auf etwa 2.5 Å einengen.
    Notes: Summary The crystal structure investigations of hydrothermally synthesized Na2[Zn2(TeO3)3]·3H2O (NZT) and Na2[Co2(TeO3)3]·3H2O (NCT) using single-crystal X-ray diffraction methods revealed a microporous framework structure of hexagonal symmetry with tubular channels running parallel to the c-axis (zemannite type). The statistically occupied sites of the Na+ ions and H2O molecules within the channels as well as the channel dimensions indicate a possible zeolitic behaviour of the compounds. Thermoanalytical investigations ofNZT show an irreversible breakdown of the framework already atT=533 K caused by complete dehydration. A reversible rehydration was solely observed for partially dehydratedNZT (T⩽493 K); a remarkable ion exchange rate from alkali-chloride solutions was observed only for Li+. Both the rehydration and the ion exchange properties are characterized by relatively long reaction times. The relatively poor zeolitic properties compared to typical zeolitic compounds could be related to the stereochemical activity of the lone-pair electrons of the Te4+ atoms which claim a certain volume within the channels and constrict the effective channel dimension to a free diameter of approximately 2.5 Å.
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  • 7
    Electronic Resource
    Electronic Resource
    s.l. ; Stafa-Zurich, Switzerland
    Materials science forum Vol. 321-324 (Jan. 2000), p. 791-795 
    ISSN: 1662-9752
    Source: Scientific.Net: Materials Science & Technology / Trans Tech Publications Archiv 1984-2008
    Topics: Mechanical Engineering, Materials Science, Production Engineering, Mining and Metallurgy, Traffic Engineering, Precision Mechanics
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  • 8
    Electronic Resource
    Electronic Resource
    Springer
    Physics and chemistry of minerals 26 (1998), S. 100-106 
    ISSN: 1432-2021
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Geosciences , Physics
    Notes: Abstract  Single crystals of the garnet Mn2+ 3Mn3+ 2[SiO4]3 and coesite were synthesised from MnO2-SiO2 oxide mixtures at 1000°C and 9 GPa in a multianvil press. The crystal structure of the garnet [space group Ia3¯d, a=11.801(2) Å] was refined at room temperature and 100 K from single-crystal X-ray data to R1=2.36% and R1=2.71%, respectively. In contrast to tetragonal Ca3Mn3+ 2[GeO4]3 (space group I41/a), the high-pressure garnet is cubic and does not display an ordered Jahn-Teller distortion of octahedral Mn3+. A disordered Jahn-Teller distortion either dynamic or static is evidenced by unusual high anisotropic displacement parameters. The room temperature structure is characterised by following bond lengths: Si-O=1.636(4) Å (tetrahedron), Mn3+-O=1.995 (4) Å (octahedron), Mn2+-O=2.280(5) and 2.409(4) Å (dodecahedron). The cubic structure was preserved upon cooling to 100 K [a=11.788(2) Å] and upon compressing up to 11.8 GPa in a diamond-anvil cell. Pressure variation of the unit cell parameter expressed by a third-order Birch-Murnaghan equation of state led to a bulk modulus K 0=151.6(8) GPa and its pressure derivatives K′=6.38(19). The peak positions of the Raman spectrum recorded for Mn2+ 3Mn3+ 2[SiO4]3 were assigned based on a calderite Mn2+ 3Fe3+ 2[SiO4]3 model extrapolated from andradite and grossular literature data.
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  • 9
    ISSN: 1432-2021
    Keywords: Key words Chromous silicate ; High-pressure ; Crystal chemistry ; Chromium dimer ; Metal-metal bonding
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Geosciences , Physics
    Notes: Abstract The high-pressure behaviour of chromous orthosilicate, Cr2SiO4, has been studied by means of single-crystal X-ray diffraction and electronic absorption spectroscopy. X-ray diffraction data show that the structure remains orthorhombic to the highest pressure reached of 9.22 GPa. The compressibility of the unit-cell is strongly anisotropic with the c axis approximately six times more compressible than the a and b axes. A third-order Birch-Murnaghan equation of state fitted to the volume-pressure data yields V 0 = 610.10(3) Å3, K = 94.7(4) GPa, K′ = 8.32(14). Cr2SiO4 is therefore more compressible than the isostructural Cd analogue, even though its molar volume is smaller. This unusual behaviour can be attributed to the fact that the Cr atom is too small for the six-coordinated site that it occupies, and the site is therefore strongly distorted. Structure refinements indicate that under high pressures the Cr atom remains strongly displaced from the central position of the octahedron. Polarized and unpolarized electronic absorption spectra include a strong absorption band occuring at 18.300 cm−1 for E//c (which is parallel to the shortest Cr-Cr vector in the structure) which has an unusually large half width (5000 cm−1), indicative of electronic interaction between metal centres. Deconvolution of unpolarized high-pressure spectra show that the relative integrated intensity of this component increases linearly from 40% at 1 bar to 60% at 11.2 GPa. Both the structural changes and the absorption spectra at high pressures suggest that pairs of adjacent Cr atoms in chromous orthosilicate form chromium dimers with a weak metal-metal bond, which is consistent with the diamagnetic response found at ambient pressure.
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  • 10
    Electronic Resource
    Electronic Resource
    Springer
    Physics and chemistry of minerals 27 (1999), S. 47-51 
    ISSN: 1432-2021
    Keywords: Key words Crystal structure ; Calcium aluminium silicate ; Barium ferrite
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Geosciences , Physics
    Notes: Abstract Single crystals of CaAl4Si2O11 were synthesised at 1,500 °C and 14 GPa in a multi-anvil press, and the structure of the phase determined by single-crystal X-ray diffraction at room conditions. The structure-type is that of the “hexagonal barium ferrites”. The space group of the average structure is P6 3 /mmc and the cell parameters are a = 5.4223(4) Å, c = 12.7041(6) Å, V = 323.28(5) Å3, with Z = 2, and its density is 3.905 g cm−3, which is reasonable for a high-pressure alumino-silicate phase. The 22 oxygen and two calcium atoms within the unit-cell form an approximate hexagonal-close-packed array. Ten of the twelve octahedral interstices within this array that have only oxygen atoms for apices are filled with Si and/or Al. M1 octahedra share edges to form a spinel-like sheet of octahedra. The average bond length 〈M1-O〉 = 1.833 Å suggests mixed occupancy by Si and Al. The M1 octahedral sheets are linked by shared corners to pairs of face-sharing M2 octahedra containing Al, with 〈M2-O〉 = 1.918 Å. The remaining two cations of the unit-cell contents statistically occupy four tetrahedrally-coordinated interstices, which occur as face-sharing pairs. The average bond length for these sites (1.742 Å) suggests that they are occupied by Al, although Si occupancy cannot be excluded by the data. It is proposed that only one interstice of each pair is locally occupied, with the possibility of some short-range ordering of such occupancies. Complete long-range order leading to the acentric space group P6 3 mc is excluded by the data, as is the possibility of the average structure being comprised of merohedral (0 0 0 1) twins of P6 3 mc symmetry.
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