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  • 1
    Electronic Resource
    Electronic Resource
    s.l. : American Chemical Society
    The @journal of physical chemistry 〈Washington, DC〉 98 (1994), S. 12687-12694 
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology , Physics
    Type of Medium: Electronic Resource
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  • 2
    Electronic Resource
    Electronic Resource
    s.l. : American Chemical Society
    The @journal of physical chemistry 〈Washington, DC〉 93 (1989), S. 2019-2027 
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology , Physics
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    Copenhagen : International Union of Crystallography (IUCr)
    Applied crystallography online 18 (1985), S. 258-262 
    ISSN: 1600-5767
    Source: Crystallography Journals Online : IUCR Backfile Archive 1948-2001
    Topics: Geosciences , Physics
    Notes: STRUPL084 is a Fortran plot program for drawing crystal structures in polyhedral or skeletal representation. All data are read in free format by standard Fortran routines. Atomic positions are also accepted in formats compatible with the input for the programs SHELX and ORFLS. The structure can be rotated by three rotation angles applied to the orthogonal axes. Instead of giving the rotation angles a view direction can be specified. The output includes a list of direct and orthogonal coordinates and tables with interatomic distances and angles. Atoms that were found to form coordination polyhedra are listed separately. The program is `user friendly' inasmuch as an acceptable plot can be achieved with minimum input by making use of the default options. Atoms not belonging to any polyhedra can be drawn as circles with specified radii.
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  • 4
    Electronic Resource
    Electronic Resource
    Copenhagen : International Union of Crystallography (IUCr)
    Acta crystallographica 53 (1997), S. 440-443 
    ISSN: 1600-5740
    Source: Crystallography Journals Online : IUCR Backfile Archive 1948-2001
    Topics: Chemistry and Pharmacology , Geosciences , Physics
    Notes: Samples of two differently prepared zeolite rho loaded with different amounts of dimethylamine (DMA) were studied in their hydrated forms by X-ray diffraction. Both zeolites are partially dealuminated, as indicated by nonframework A1 which is assumed to be Al2O3 or AlOOH. Series I was prepared from dry-calcined NHn-rho at 873 K, series II from steam-calcined NHn-rho at 773 K. The samples were loaded with different amounts of DMA. Rietveld refinements yielded the following results for series I: (1) H3.8(H-DMA)5Cs0.2Al9Si39O96.Al2O3.21H2O, X-ray data collection at room temperature, Im\overline 3m, a = 15.0590 (2) Å, Rwp = 0.089; (2) (H-DMA)8.8Cs0.2Al9Si39O96.Al2O3.18H2O, X-ray data collection at room temperature, Im\overline 3m, a = 15.0680 (2) Å, Rwp = 0.091. Series II: (3) H0.3(H-DMA)5Cs0.7Al6Si42O96.2.5Al2O3.24H2O, X-ray data collection at room temperature, Im\overline 3m, a = 15.0596 (2) Å, Rwp = 0.120. DMA resides on the center axis through the \alpha-cage with the N atoms pointing to the single eight-ring and the two methyl groups oriented towards the center of the \alpha-cage.
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  • 5
    Electronic Resource
    Electronic Resource
    Copenhagen : International Union of Crystallography (IUCr)
    Applied crystallography online 23 (1990), S. 462-468 
    ISSN: 1600-5767
    Source: Crystallography Journals Online : IUCR Backfile Archive 1948-2001
    Topics: Geosciences , Physics
    Notes: Two definitions of profile agreement indices are now in common use for estimating the degree of fit in Rietveld refinement and in structure-independent pattern-fitting methods of powder diffraction analysis. In the original program written by Rietveld, the background was subtracted and the `non-peak' regions of the pattern were removed from further consideration in a preliminary data-reduction stage prior to Structure refinement. However, the agreement indices used in many of the more recent programs retain the background counts in the observed step intensities and include all portions of the pattern in the sums. These latter definitions are strongly dependent on the signal-to-noise ratio and on the relative amount of `background-only' regions and do not, therefore, provide a sound basis for comparing the degree of fit of peak profile and crystal structure model refinements in the general case. The extent of this dependence is illustrated quantitatively using conventional and synchrotron X-ray and constant-wavelength and time-of-flight neutron data sets with different inherent background levels and peak densities. The unweighted background-corrected peak-only profile agreement index R′p = Σi|Yio − Yic|/Σi|Yio −Yib| (and, to a lesser extent, its weighted equivalent) is recommended as the most appropriate criterion of fit for comparative work between diffraction patterns of all kinds.
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  • 6
    Electronic Resource
    Electronic Resource
    Oxford [u.a.] : International Union of Crystallography (IUCr)
    Acta crystallographica 43 (1987), S. 1852-1854 
    ISSN: 1600-5759
    Source: Crystallography Journals Online : IUCR Backfile Archive 1948-2001
    Topics: Chemistry and Pharmacology , Geosciences , Physics
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    Oxford [u.a.] : International Union of Crystallography (IUCr)
    Acta crystallographica 44 (1988), S. 775-776 
    ISSN: 1600-5759
    Source: Crystallography Journals Online : IUCR Backfile Archive 1948-2001
    Topics: Chemistry and Pharmacology , Geosciences , Physics
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  • 8
    Electronic Resource
    Electronic Resource
    Oxford [u.a.] : International Union of Crystallography (IUCr)
    Acta crystallographica 45 (1989), S. 983-989 
    ISSN: 1600-5759
    Source: Crystallography Journals Online : IUCR Backfile Archive 1948-2001
    Topics: Chemistry and Pharmacology , Geosciences , Physics
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  • 9
    Electronic Resource
    Electronic Resource
    Copenhagen : International Union of Crystallography (IUCr)
    Acta crystallographica 53 (1997), S. 444-450 
    ISSN: 1600-5740
    Source: Crystallography Journals Online : IUCR Backfile Archive 1948-2001
    Topics: Chemistry and Pharmacology , Geosciences , Physics
    Notes: Samples of two differently prepared zeolites rho loaded with different amounts of trimethylamine (TMA) were studied in their hydrated and dehydrated forms by X-ray and neutron diffraction experiments. Both zeolites are partially dealuminated, as indicated by nonframework Al, which is assumed to be Al2O3 or AlOOH. Series I was prepared from dry-calcined NHn-rho at 873 K, series II from steam-calcined NHn-rho at 773 K. The samples were loaded with different amounts of deuterated TMA. Rietveld refinements yielded the following results for series I: (1) H3.8(H-TMA)5Cs0.2Al9 Si39O96.Al2O3.22H2O, X-ray data collection at room temperature, Im\overline 3m, a = 15.0542 (2) Å, Rwp = 0.094; (2) composition as in (1) (anhydrous), neutron data collection at 5 K of dehydrated and deuterated sample, Im3m, a = 15.0467 (4) Å, Rwp = 0.034. Series II: (3) H0.3(H-TMA)5Cs0.7Al6Si42O96.2.5Al2O3.22H2O, X-ray data collection at room temperature, Im\overline 3m, a = 15.0574 (2) Å, Rwp = 0.118; (4) composition as in (3) (anhydrous), neutron data collection at 5 K of dehydrated and deuterated sample, lm\overline 3m, a = 15.0761 (5) Å, Rwp = 0.037. In all determinations the TMA molecules reside with the N and H (D in neutron diffraction analysis) atoms on the central axes (x, 0, 0) pointing towards the center of the single eight-ring, whilst the three methyl groups point away to the center of the \alpha-cage.
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  • 10
    Electronic Resource
    Electronic Resource
    Copenhagen : International Union of Crystallography (IUCr)
    Acta crystallographica 53 (1997), S. 429-439 
    ISSN: 1600-5740
    Source: Crystallography Journals Online : IUCR Backfile Archive 1948-2001
    Topics: Chemistry and Pharmacology , Geosciences , Physics
    Notes: Samples of two differently prepared zeolite rho loaded with different amounts of monomethylamine (MMA) were studied in their hydrated and dehydrated forms by X-ray and neutron diffraction. Both zeolites are partially dealuminated, as indicated by nonframework alumina, which is assumed to be Al2O3 or AlOOH. Series I was prepared from dry-calcined NH4-rho at 873 K, series II from steam-calcined NH4-rho at 773 K. The samples were loaded with different amounts of deuterated MMA, Rietveld refinements yielded the following results for series I (dry): (1) H3.8(H-MMA)5Cs0.2Al9Si39O2.Al2O3.28H2O, X-ray data collection at room temperature, Im\overline 3m, a = 14.9991 (2) Å, Rwp = 0.095; (2) composition as in (1), anhydrous and deuterated, neutron data collected at 5 K, disproportionation into two phases in I\overline 43m, with a = 14.8410 (7) and 14.5273 (11) Å, Rwp = 0.038; (3) (H-MMA)8.8Cs0.2Al9Si39O96.Al2O3.25H2O, X-ray data collection at room temperature, I\overline 43m, a = 14.9771 (2) Å, Rwp = 0.090. Series II (steam): (4) H0.3(H-MMA)5Cs0.7Al6Si42O96.2.5Al2O3.23H2O, X-ray data collected at room temperature,Im\overline 3m, a = 15.0323 (2) Å, Rwp = 0.124; (5) composition as in (4), anhydrous and deuterated, neutron data collected at 5 K, disproportionation into two phases in I\overline 43m with a = 14.9151 (2) and 14.6475(8) Å, Rwp = 0.031. In the hydrated samples MMA resides on the center axis in the α-cage with the N atoms pointing to the single eight-ring; upon dehydration it migrates into the double eight-rings.
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