Remark on the Phase Problem in Crystallography (original) (raw)

1975, Proceedings of the National Academy of Sciences

The ambiguities found in determining a crystal structure from x-ray diffraction can be resolved if one takes into account the random thermal motion of the atoms.

Fundamentals of Crystallography

2011

The crystalline State and isometric Operations 1 Symmetry elements 3 Axes of rotational symmetry 3 Axes of rototranslation or screw axes 5 Axes of inversion 5 Axes of rotorefiection 5 Refiection planes with translational component (glide planes) 6 Lattices 6 The rational properties of lattices 7 Crystallographic directions 7 Crystallographic planes 8 Symmetry restrictions due to the lattice periodicity and vice versa 9 Point groups and symmetry classes 11 Point groups in one and two dimensions 16 The Laue classes 17 The seven crystal Systems 17 The Bravais lattices 18 Plane lattices 18 Space lattices 19 The space groups 22 The plane and line groups 30 On the matrix representation of symmetry Operators 32 Appendices: LA The isometric transformations 35 l.B Some combinations of movements 37 l.C Wigner-Seitz cells 41 l.D The space-group rotation matrices l.E Symmetry groups l.F Symmetry generalization References Crystallographic Computing Carmelo Giacovazzo

X-Ray Diffraction Crystallography

The use of general descriptive names, registered names, trademarks, etc. in this publication does not imply, even in the absence of a specific statement, that such names are exempt from the relevant protective laws and regulations and therefore free for general use.

Derivation of conventional crystallographic descriptions of new phases from results of ab initio inorganic structure modelling

Journal of Applied Crystallography, 1996

The results of ab initio inorganic structure modelling are often in the form of Cartesian coordinates of atoms in a large, periodical and in general oblique simulation box containing hundreds to thousands of atoms. The contents of that box may correspond to a single crystal, a twin, a mixture of phases or a disordered block of matter. The problem of extracting corresponding crystallographic descriptions for single-crystal regions in the box, a necessary step in view of full quantum calculations and publication, is different from the familiar problem of extracting crystal symmetry and structure from experimental diffracted intensity data. The deductive computeraided method developed at the National Research Council of Canada over the years is based on eye identification of three pairs of atoms related by conjugate translations in the same single-crystal region on a stereo plot, followed by derivation of fractional coordinates for the atomic content of the corresponding primitive cell. Running this data through the MISSYM program discloses potential symmetry elements of the structure, with their corresponding crystallographic directions. These elements are then critically examined and accepted either as symmetry or pseudosyrnmetry on the basis of comparison of coordinate deviations between related atoms with the expected magnitude of thermal motion. All calculations described here can be performed with the NRCVAX system of programs.

Crystal Structure

In chapter three we have discussed that there are three states of matter; solids, liquids and gases. In the same chapter under section 3.3, we tried to mention water as an example exists in three state forms; ice (solid), water (liquid) and vapor (gas). If you see in this case the same matter is in three forms and the difference is only temperature. Based on the pressure and temperature, a matter exists in various phases. Liquids and gases are called fluids because of their ability to flow. The fluidity in both of these states is due to the fact that the molecules are free to move around.

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