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  • 1
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Journal of the American Ceramic Society 87 (2004), S. 0 
    ISSN: 1551-2916
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Mechanical Engineering, Materials Science, Production Engineering, Mining and Metallurgy, Traffic Engineering, Precision Mechanics , Physics
    Notes: The crystallization of ordered (Zr,Ti)2O4 from the oxides succeeded for the first time, at 800°–1200°C and 13–20 kbar, using either ammonium carbonate or copper oxide as flux. The composition of the ordered phase, coexisting with either zirconia or rutile, is pressure–temperature dependent, ranging from XTi= 0.60 to 0.68. Its reproducibility and reversibility suggest the ordered compound crystallized at/near thermodynamic equilibrium. The presence of flux permits the equilibration of phase assemblages well below 1200°C, a region previously inaccessible for equilibrium experiments in the ZrO2–TiO2 system due to sluggish kinetics. Thus we were able to determine the ZrO2–TiO2 phase diagram at 20 kbar at temperatures as low as 800°C. In contrast, room-pressure experiments did not result in the spontaneous nucleation of ordered (Zr,Ti)2O4 from the oxides, and seeds were required to initiate growth. The flux-aided synthesis of ordered (Zr,Ti)2O4 from the oxides, at constant temperature and in its stability field, has the following advantages over previous crystallization attempts, which consisted of slow cooling of the disordered polymorph through the ordering transition. The ordered compound forms at equilibrium, therefore permitting phase equilibrium studies and thermodynamic interpretation. Large grain sizes facilitate quantitative analysis of the composition with electron microscopy. Microcracks and ZrO2 exsolution, reported from samples cooled through the transition, can be avoided. The composition and the ordering state of the ordered compound can be controlled with pressure and temperature. Using the flux-based synthesis method, well-crystallized samples can now be obtained for future crystal structure refinements, calorimetric and dielectric measurements, or investigations into the phase transition.
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  • 2
    Electronic Resource
    Electronic Resource
    s.l. : American Chemical Society
    The @journal of physical chemistry 〈Washington, DC〉 96 (1992), S. 8173-8176 
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology , Physics
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    Springer
    Physics and chemistry of minerals 16 (1989), S. 343-351 
    ISSN: 1432-2021
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Geosciences , Physics
    Notes: Abstract The concept of short-range interlayer interactions, fundamental to spin-analogue models for polytypism, is examined in the case of sapphirine. Consideration of interactions out to fourth-nearest neighbours provides a rationale for the difference between the polytype suites observed for sapphirine and wollastonite. In each case, the observed long-period structures are consistent with those predicted to be stable by the appropriate mappings onto the axial next-nearest neighbour model. Short-range interaction parameters may also be used to express stacking fault energies. This approach, combined with a simple nucleation-andgrowth model, is used to examine the possibility of metastable generation of complex polytypes in sapphirine. Statistical analysis of defect distributions and frequencies in sapphirine suggests that interactions over several hundred Ångstroms must be considered if the stacking energetics are to be accurately modelled.
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  • 4
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 123 (1929), S. 873-874 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] THE dominant feature of the M-type stars is the very extensive group of titanium oxide bands, beginning in the blue region of the spectrum and continuing far to the red. The group of bands occurring in the blue-green region has been analysed (see Christy and Birge, NATURE, 122, 205; ...
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  • 5
    Electronic Resource
    Electronic Resource
    Springer
    Contributions to mineralogy and petrology 102 (1989), S. 422-428 
    ISSN: 1432-0967
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Reaction textures and chemographic relations in sapphirine-bearing basic granulites at Finero, Italy, suggest that sapphirine and aluminous diopside were formed in mutual equilibrium from an inferred early spinel-bearing assemblage. Finero appears to be the only known locality where this association has been found in situ, although it is also known from kimberlite and breccia pipe nodules elsewhere. The reactions deduced to have occurred in these rocks suggest the existence of stable invariant points involving the phases sapphirine-spinel-orthopyroxene-clinopyroxene-garnet-anorthite and sapphirine-two pyroxenes-garnetanorthite-kyanite (or sillimanite) in the CMAS end-member system. P-T estimates for the relevant rocks, and the available experimental data, suggest that these points lie at around 800°–900° C, 9–11 kbar. A semi-quantitative petrogenetic grid, incorporating these invariant points with previously determined univariant reactions, is proposed. It is inferred that sapphirine+diopside are stable relative to spinel-bearing assemblages below 900° C. The relatively low temperature explains why sapphirine has not to date been reported from experimental work on the CMAS system. It also suggests that sapphirine may be an important aluminous phase in Mg-rich metagabbros under conditions corresponding to the base of the continental crust, despite the observed rarity of such rocks at the surface.
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  • 6
    Electronic Resource
    Electronic Resource
    Springer
    Contributions to mineralogy and petrology 103 (1989), S. 203-215 
    ISSN: 1432-0967
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Microprobe analyses and structural characterisation by means of transmission electron microscopy and powder X-ray diffraction are presented for a suite of natural and synthetic sapphirines. Most sapphirines appear to consist of intergrowths of the common 2M polytype with minor amounts of the 1Tc phase, although the converse situation is found in some cases. Attempts to correlate the structural state of the mineral with other factors reveal that: (i) There is no strong relationship between mean tetrahedral cation radius or mean octahedral cation radius and the preferred polytype. The Tschermak substitution M2+M4+-M3+M3+ does not appreciably influence the 1Tc-2M equilibrium, (ii) However, the total content and mean oxidation state of iron in sapphirine are important in this respect. Fe2+ stabilises the 2M phase, whereas Fe3+ stabilises the 1Tc phase. (iii) P-T estimates for the host rocks, and estimates for the conditions of sapphirine crystallisation, where obtainable, suggest that the 1Tc phase is stable at lower T and higher P than the 2M phase. Some quantitative constraints are inferred.
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  • 7
    Electronic Resource
    Electronic Resource
    Springer
    Physics and chemistry of minerals 15 (1988), S. 548-558 
    ISSN: 1432-2021
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Geosciences , Physics
    Notes: Abstract Transmission electron microscopy of various natural and synthetic sapphirines shows the existence of extensive polytypic variation in some samples. In addition to the previously described 1Tc and 2M polytypes, 3Tc, 4M and 5Tc structures are observed. The structural principles underlying the polytypism and the associated diffraction behaviour are reviewed, and the correlation between the nature of the observed stacking faults and their origin during crystal growth, in deformation or as a result of solid-state transformation is discussed. Pairs of c/2 partial dislocations observed in synthetic material provide a likely solid-state transformation mechanism, although the evidence suggests that most observed stacking variation arises during growth. A new type of non-conservative planar defect has been found in sapphirine from Finero, Italy, suggestive of unit-cell scale intergrowth with a surinamite- or pyroxene-like structure. A polysomatic model of the sapphirine and surinamite structures as stackings of pyroxene 〈P〉 and spinel 〈S〉 modules is proposed.
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    Springer
    Physics and chemistry of minerals 22 (1995), S. 129-135 
    ISSN: 1432-2021
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Geosciences , Physics
    Notes: Abstract Comparisons of the structures of the high-pressure and high-temperature phases of both anorthite and clinopyroxene show that they are quite distinct although they share a common space group and site symmetries for all atoms. The low-pressure, low-temperature phases in both systems are formed by zone-boundary transitions from the high-pressure or high-temperature structures, and have structures that are made up of the alternation of portions of the high-pressure and high-temperature structures. This behaviour is analyzed in terms of the order parameter behaviour of the high-symmetry structures, and it is shown that the stability of the low-symmetry phases arises naturally from inhomogeneity in this order parameter.
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  • 9
  • 10
    Publication Date: 2012-05-01
    Description: We modified the self-consistent coherent potential approximation (CPA) for modeling properties of granular composite materials so that it takes into consideration the grain coordination number and distinctive elastic moduli for grain-contact zones. The original CPA was reasonably accurate for low-porosity consolidated sandstones but used only inclusion (pore or grain) shape and did not take into account morphological parameters such as coordination number and contact area or contact moduli. In our modified model, the grain inclusion was represented as a “grain with contact area”; therefore, scattering of elastic waves by contacts was incorporated. The modified CPA has been used to calculate data for 3D digital models of sintered quartz bead samples and Fontainebleau sandstones. Reduction of local elastic moduli for contact zones of specified area and thickness reduced effective overall moduli of the bulk sample. The modified theory predicted this weakening accurately, as compared to finite-element simulations.
    Print ISSN: 0016-8033
    Electronic ISSN: 1942-2156
    Topics: Geosciences , Physics
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