Abstract
THE direct F2 Fourier series of Patterson1 is one of the most powerful methods in modern crystal analysis, and many of its applications have been described from time to time in NATURE2. Patterson's original result was derived as an extension of the application to crystals of the theory of scattering of X-rays in liquids made by Gingrich and Warren3. Patterson computes the weighted average distribution of electron density ; about a point in the crystal, cell-size abc, volume v, by the relation which gives the distribution about the point as a function of the parameters uvw. Making use of the usual expression for the electron density in terms of the structure amplitudes F(hkl), namely, the function A (uvw) is obtained as The importance of A(uvw) arises because it will only be large when there are high values in ;(xyz) both at (xyz) and at (x+u, y+v, z+w). Thus a peak in the function A(uvw) at (u1v1w1) corresponds to an interatomic distance in the crystal defined by a vector the components of which are (u1v1w1).
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References
Patterson, A. L., Phys. Rev., 46, 372 (1934); Z. Krist., 90, 517 (1935).
See NATURE, 142, 581, 955, 994 (1938); 143, 75 (1939); 149, 491 (1942); 150, 324 (1942).
Warren, B. E., and Gingrich, N. S., Phys. Rev., 46, 368 (1934).
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ROBERTSON, J. Interpretation of Patterson Diagrams. Nature 152, 411–412 (1943). https://doi.org/10.1038/152411a0
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DOI: https://doi.org/10.1038/152411a0
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