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  • American Geophysical Union  (3,270)
  • American Physical Society (APS)
  • International Union of Crystallography (IUCr)
  • 1990-1994  (4,593)
  • 1955-1959
  • 1992  (4,593)
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  • 1990-1994  (4,593)
  • 1955-1959
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  • 1
    Electronic Resource
    Electronic Resource
    Copenhagen : International Union of Crystallography (IUCr)
    Applied crystallography online 25 (1992), S. 1-5 
    ISSN: 1600-5767
    Source: Crystallography Journals Online : IUCR Backfile Archive 1948-2001
    Topics: Geosciences , Physics
    Notes: Based on investigations at 9 and 295 K, Na2UI6 has been shown to crystallize in a new structure type corresponding to space group R{\bar 3}, in contrast to ionic conductors of the type Na2UX6 for X = Cl, Br which crystallize in the space group P{\bar 3}ml. Atomic positions of sodium and iodine have been refined using the Rietveld profile fitting procedure. It was found that in space group R{\bar 3} the U, Na and I atoms occupy positions 3(a), 6(c) and 18(f), respectively. The relation between the Na2UCl6-type structure and the structure of Na2UI6 is discussed.
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  • 2
    Electronic Resource
    Electronic Resource
    Copenhagen : International Union of Crystallography (IUCr)
    Applied crystallography online 25 (1992), S. 11-15 
    ISSN: 1600-5767
    Source: Crystallography Journals Online : IUCR Backfile Archive 1948-2001
    Topics: Geosciences , Physics
    Notes: An in situ observation of the structure transition of GeO2 has been made under 3.0 GPa at various temperatures with a diamond-anvil pressure cell. The time-resolved energy-dispersive (ED) diffraction experiment was undertaken using synchrotron X-radiation. A profile analysis of ED spectra observed every 15 min elucidates the transition process from the α-quartz form (P3221, Z = 3) to the rutile form (P42/mmm, Z = 2). The time-resolved measurement of their diffraction intensity ratio reveals the change of the mass fraction of the transformed product with time, which provides the transition rate. A transition curve showed three stages at low temperature; firstly a long inductance period after initiation of heat supply, secondly a rapid initiation of transition and finally a marked deceleration of growth. At high temperatures the inductance period of the transition was not observable. The transition is extremely sluggish. An apparent activation energy was calculated by the Avrami–Erofeev equation for the solid-solid transition and found to be 57.4 kJ mol−1.
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  • 3
    Electronic Resource
    Electronic Resource
    Copenhagen : International Union of Crystallography (IUCr)
    Applied crystallography online 25 (1992), S. 6-10 
    ISSN: 1600-5767
    Source: Crystallography Journals Online : IUCR Backfile Archive 1948-2001
    Topics: Geosciences , Physics
    Notes: Nonlinear equations are given for determining the crystallographic orientation of surfaces of single crystals. The equations are solved by an iterative method in several variables. The angle φ between the surface plane and the lattice plane in question is decomposed into two components α and β. These two components are obtained from the solution of a nonlinear system of equations using two measurements and the Bragg angle. The diffractometric system considered is the well known θ/2θ with a sufficiently large area of X-ray detection and the capability of holding single-crystal samples. The results obtained are discussed from experimental and theoretical points of view.
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  • 4
    Electronic Resource
    Electronic Resource
    Copenhagen : International Union of Crystallography (IUCr)
    Applied crystallography online 25 (1992), S. 26-30 
    ISSN: 1600-5767
    Source: Crystallography Journals Online : IUCR Backfile Archive 1948-2001
    Topics: Geosciences , Physics
    Notes: A method to improve the scaling of multiple intensity data sets is presented. A general scaling function K(x, s), which uses the direction cosine of the diffraction vector (x) and (sin θ)/λ (s) as scaling parameters, is developed by combining an isotropic scaling function, K(s) = A exp (Bs2), and a multiple s-shell anisotropic scaling function, K(x)s = (Σ Σ cijxij)s. This combined scaling function can greatly reduce the systematic differences in intensities among multiple data sets measured independently. This scaling method for the multiple data sets consists of three steps. In the first step, the individual isotropic scaling functions, K(s), are determined by an indirect least-squares method. Then the weighted mean intensity, 〈I〉, is calculated by applying the K(s) to the individual data sets. In the second step, the data in each data set are divided equally into 20 thin shells of (sin θ)/λ (s). The anisotropic scaling functions, K(x)s, of each s shell are determined by using the weighted mean intensity, 〈I〉, obtained in the first step as the target quantity in a least-squares minimization, i.e. Σ wi{〈I〉i − K(x)s[K(s)Ii]}2. In the final step, the new weighted mean intensity, 〈I〉, is calculated by applying the combined scaling function, K(x, s) = K(s)K(x)s, to the individual data sets. The new multiple s-shell anisotropic scaling functions are determined using the new weighted mean intensity, 〈I〉, as the target quantity in another least-squares minimization. By repeating this procedure three to five times, the least-squares minimization will converge. The method was successfully used to scale and merge 27 sets of S-adenosylmethionine synthetase data into a single data set. It was also used to scale the isomorphous replacement data sets of the enzyme.
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  • 5
    Electronic Resource
    Electronic Resource
    Copenhagen : International Union of Crystallography (IUCr)
    Applied crystallography online 25 (1992), S. 16-25 
    ISSN: 1600-5767
    Source: Crystallography Journals Online : IUCR Backfile Archive 1948-2001
    Topics: Geosciences , Physics
    Notes: This work presents a new method of synthesizing the reflection profile, based on the calculation of Fourier coefficients of instrumental functions. The classification and construction of Fourier coefficients are effected, in a general way, from the analysis of the possible paths of beams in the diffractometer. Relationships were obtained which made it possible to synthesize the line profiles in different experimental conditions. The possibility of calculating the reflection profiles of a standard (annealed BaF2) without introducing varying profile parameters is shown. Better results in describing the reflection profiles have been obtained than by applying the Pearson VII function with varying profile parameters.
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  • 6
    Electronic Resource
    Electronic Resource
    Copenhagen : International Union of Crystallography (IUCr)
    Applied crystallography online 25 (1992), S. 31-38 
    ISSN: 1600-5767
    Source: Crystallography Journals Online : IUCR Backfile Archive 1948-2001
    Topics: Geosciences , Physics
    Notes: A model of size distribution and structural disorder for palladium grown on pumice is developed. The model parameters are determined by fitting the simulated powder pattern to the experimental data. Three samples, characterized by 2.4, 1.14 and 0.86 wt.% Pd respectively were examined. The results point to nearly spheroidal crystallites, with sizes ranging from 40 to 20 Å, affected by stacking faults in the sequence of the close-packed (111) layers to an extent independent of size and by intralayer second-kind distortions. A comparison with the results obtained following classical procedures is supplied. In the Appendix a new approach for the determination of growth stacking faults from peak shifts is presented.
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  • 7
    Electronic Resource
    Electronic Resource
    Copenhagen : International Union of Crystallography (IUCr)
    Applied crystallography online 25 (1992), S. 39-45 
    ISSN: 1600-5767
    Source: Crystallography Journals Online : IUCR Backfile Archive 1948-2001
    Topics: Geosciences , Physics
    Notes: Approximate analytic expressions for determining the transmission of neutron benders which take into account reflectivity losses using the mean number of reflections agree well with computer simulation results which track the neutron trajectories directly, provided that the reflectivity is high. The exact calculation which can be performed using exponential integral functions for any value of the reflectivity is presented. Ray-tracing techniques for determining the transmission and number of reflections for non-perfect reflectivity can therefore be replaced by direct calculation.
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  • 8
    Electronic Resource
    Electronic Resource
    Copenhagen : International Union of Crystallography (IUCr)
    Applied crystallography online 25 (1992), S. 46-51 
    ISSN: 1600-5767
    Source: Crystallography Journals Online : IUCR Backfile Archive 1948-2001
    Topics: Geosciences , Physics
    Notes: The simulation of the experimental symmetric X-ray rocking curve of a coherent heteroepitactic structure, using first-order expressions in the incidence parameter, is shown to give a strain-depth profile not consistent with asymmetric rocking curves taken on the same sample. Two different expressions are suggested for the incidence parameter to attain internal consistency among all the rocking curves. The former involves second-order approximations and considers both normal and parallel lattice mismatches. The latter is the result of an exact derivation and takes into account only the normal mismatch. These models make the data from rocking-curve simulation reliable, provided that the angle between the surface and the planes corresponding to the nominal crystallographic orientation is not ignored.
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  • 9
    Electronic Resource
    Electronic Resource
    Copenhagen : International Union of Crystallography (IUCr)
    Applied crystallography online 25 (1992), S. 65-68 
    ISSN: 1600-5767
    Source: Crystallography Journals Online : IUCR Backfile Archive 1948-2001
    Topics: Geosciences , Physics
    Notes: A procedure for evaluating peaks in the difference Patterson maps calculated from a complete native data set and partial (incomplete) potential isomorphous heavy-atom-derivative data sets is described. A sampling function is defined such that it is unity where data are available and zero elsewhere. It is the Patterson of this sampling function whose characteristics are useful. This function will not reconstruct unavailable information, but can reveal the presence of distorted and/or `false' peaks introduced by the sampling technique used in collecting partial data. This procedure is useful in screening potential heavy-atom derivatives using a minimum number of crystals.
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  • 10
    Electronic Resource
    Electronic Resource
    Copenhagen : International Union of Crystallography (IUCr)
    Applied crystallography online 25 (1992), S. 52-64 
    ISSN: 1600-5767
    Source: Crystallography Journals Online : IUCR Backfile Archive 1948-2001
    Topics: Geosciences , Physics
    Notes: The theory of surface differential diffraction (SDD) is extended to the case of polarized neutron diffraction. Nuclear and magnetic surface contributions are thus separated. A method for coherent description of the geometry of the grains is proposed. A saturated D layer chemisorbed on Ni carried by silica is studied with the following results: (111) faces represent the majority of the surface; D atoms sit above the centers of surface Ni triangles with no Ni atom in the underlying layer, the Ni–D distance is equal to 0.215 (7) nm; the magnetic moment modification induced by chemisorption is mainly localized in the surface layer of nickel. Two possible interpretations of the magnetic structure factor are discussed: one assumes no magnetic moment on D atoms but Ni displacements; the other is based on opposite assumptions.
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