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  • 1980-1984  (4)
Material
Years
Year
  • 1
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 288 (1980), S. 675-679 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] On the basis of their primary structure, the lysine-rich histones are a unified family of proteins. Each has an amino acid chain which falls into three distinct domains. Only the central domain (∼80 residues) is in a folded conformation. It is protected from trypsin digestion in chromatin and ...
    Type of Medium: Electronic Resource
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    Algebra universalis 17 (1983), S. 376-392 
    ISSN: 1420-8911
    Source: Springer Online Journal Archives 1860-2000
    Topics: Mathematics
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    Springer
    Physics and chemistry of minerals 11 (1984), S. 149-152 
    ISSN: 1432-2021
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Geosciences , Physics
    Notes: Abstract Using an interatomic potential function specific surface energies, attachment energies and slice energies have been calculated for 7 F faces and 18 S faces of orthorhombic sulphur. These energies are compared with statistical parameters (P values) for the frequency of occurrence of these faces on natural sulphur. It is found that P values are not correlated with the specific surface energies, except for the most important F faces. There is a positive correlation (r=0.881) with the surface energy per mol although this quantity has no physical meaning. It is supposed that an S face is due to alternating periods of dissolution (or evaporation) and growth, so that it occurs as a narrow face on the site of a previous edge. An excellent correlation (r=0.951) is found between the P value of an S face and a quantity P 1 P 2ξh, where P 1 and P 2 are the P values of neighbouring faces that constitute the S face, ξ is proportional to the slice energy and h a distance determined by the interfacial angles of the three faces. This process should hold for the morphological development of any mineral, provided that no face-specific adsorption of cosolutes occurs.
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    Springer
    Physics and chemistry of minerals 6 (1980), S. 313-325 
    ISSN: 1432-2021
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Geosciences , Physics
    Notes: Abstract The electrostatic lattice energies of expanded and unexpanded micas are calculated starting from a “generic” structure the ionic charges of which are varied. The mode of expansion is to move the layers apart perpendicular to (001), the K+ ions remaining midway between the layers. The energy required for expansion is a quadratic function of the layer charge. It is larger when the layer charge is in the octahedral sites (K x Al2−x Mg x Si4O10(OH)2) than when it is in the tetrahedral sites (K x Mg3Si4−x Al x O10(OH)2). Fluormicas have a slightly larger expansion energy than OH-micas. With the tetrahedral layer charge, dioctahedral micas have a slightly larger expansion energy than trioctahedral micas. This mode of expansion is less favourable than the mode usually adopted, viz. an expansion whereby the K ions divide themselves between the layers. The energy difference increases with the separation distance and is about 60 kJ mol−1 at 2.5 Å expansion. An intercalated water layer would be necessary to stabilize the K ions in positions midway between the layers.
    Type of Medium: Electronic Resource
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