International
Tables for Crystallography Volume C Mathematical, physical and chemical tables Edited by E. Prince © International Union of Crystallography 2006 |
International Tables for Crystallography (2006). Vol. C. ch. 4.2, pp. 221-229
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If each of the atoms gives rise to scattering in which momentum but not energy changes occur, and if each of the atoms can be considered to scatter as if it were an isolated atom, the cross section may be written as where
Reliable tables of f(q, Z) exist and have been reviewed recently by Kane, Kissel, Pratt & Roy (1986). The most recent schematic tabulations of f(q, Z) are those of Hubbell & Øverbø (1979
) and Schaupp et al. (1983
). The data used in these tables have been derived from the tabulation for q = 0.02 to 109 Å−1, for all Z's from 1 to 100 by Hubbell & Øverbø (1979
) based on the exact formula of Pirenne (1946
) for H, and relativistic calculations by Doyle & Turner (1968
), Cromer & Waber (1974
), Øverbø (1977
, 1978
), and high-q extensions using the Bethe–Levinger expression in Levinger (1952
).
As mentioned in Creagh & Hubbell (1987), the atoms in highly ordered single crystals do not scatter as though they are isolated atoms. Rather, cooperative effects become important. In this case, the Rayleigh scattering cross section must be replaced by two cross sections:
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That is, is replaced by
.
These effects are discussed elsewhere (Subsection 4.2.3.2). Briefly,
In equation (4.2.4.7)
, which is due to De Marco & Suortti (1971
),
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It is assumed that the total thermal diffuse scattering is equal to the scattering lost from Laue–Bragg scattering because of thermal vibrations. This equation is not in a convenient form for computation and the alternative formalism presented by Sano, Ohtaka & Ohtsuki (1969
) is often used in calculations. In this formalism,
The values of f(q, Z) are those of Cromer & Waber (1974).
Cross sections calculated using equation (4.2.4.8) tend to oscillate at low energy and this corresponds to the inclusion of Bragg peaks in the summation or integration. Eventually, these oscillations abate and
becomes a smoothly varying function of energy.
Creagh & Hubbell (1987) and Creagh (1987a
) have stressed that, before cross sections are calculated for a given ensemble of atoms, care should be taken to ascertain whether single-atom or single-crystal scattering is appropriate for that ensemble.
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