1965
DOI: 10.1063/1.1714396
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Description of Crystallite Orientation in Polycrystalline Materials. III. General Solution to Pole Figure Inversion

Abstract: A method is presented here by which orientation distribution of crystallites in anisotropic polycrystalline samples can be derived from a set of plane-normal distributions obtained by x-ray diffraction measurements. It is the generalization of the similar procedure proposed previously for analysis of samples having fiber texture. It thus represents a completely general solution to the problem of pole figure inversion, applicable to samples having any arbitrary symmetry elements. The plane-normal distribution f… Show more

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Cited by 859 publications
(330 citation statements)
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“…Texture measurements were conducted by X-ray diffraction using a Philips X'PERT system with an open cradle and copper K a radiation. Orientation distribution functions (ODF) of the global structure were calculated using the popLA algorithm based on the series expansion method proposed by Bunge 27) and Roe 28) from three incomplete pole figures of {200}, {110}, and {211}, which were measured up to an azimuth of 85 degrees. Experimental background and defocusing corrections were applied to the pole figures by measuring the texture of a pure random iron sample.…”
Section: Metallographic Analysismentioning
confidence: 99%
“…Texture measurements were conducted by X-ray diffraction using a Philips X'PERT system with an open cradle and copper K a radiation. Orientation distribution functions (ODF) of the global structure were calculated using the popLA algorithm based on the series expansion method proposed by Bunge 27) and Roe 28) from three incomplete pole figures of {200}, {110}, and {211}, which were measured up to an azimuth of 85 degrees. Experimental background and defocusing corrections were applied to the pole figures by measuring the texture of a pure random iron sample.…”
Section: Metallographic Analysismentioning
confidence: 99%
“…This fundamental consequence of the fact that the basis function having the coefficient w 400 varies only with the polar angle e, as can be seen from Eq. (1). When the polar axis is chosennormal to the plate, this contribution is independent of rotations of crystallites in the plane of the plate.…”
Section: I: Imentioning
confidence: 99%
“…(0 e e (1) R.=O m=-R. n=-R. R.mn R.mn where 6, cp and ljl are Euler angles descri bi ng the ori entat ion of a part i cular crystallite with respect to the sample axes, ~=cos6, the ZR.~n are the Generalized Legendre functions, and WR. are the orientation d1stribution coefficients (ODC's).…”
Section: I: Imentioning
confidence: 99%
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“…Following usual practice, we describe the crystallographic texture at X by an orientation distribution function (ODF) w. Using the convention initiated by Roe (3], we expand w as an infinite series of the generalized spherical functions:…”
Section: Model-independent Formulaementioning
confidence: 99%