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Neutron Scattering

Neutron Scattering - JuSER - Forschungszentrum Jülich

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Apart from the global description of the texture in the total orientation space, texture<br />

can also be described by a certain number of texture model components, although this<br />

description includes only restricted areas of the orientation space . Each component to be<br />

described, for instance, by a Gaussian distribution curve is given by (1) a prefened orientation<br />

g° locally restricted in orientation space, (2) a halfwidth b° characterizing the spread around g°<br />

(sec Fig . 18 .19) and (3) an intensity 1 ° indicating the volume share of all crystallites belonging<br />

to that component . The ODF approximation by means of texture components is expressed by<br />

f(g) = R + Y- 1 ° f(g) (7) .<br />

The quantity R gives the volume fraction of the randomly oriented crystallites, i .e. which are<br />

not restricted in the orientation space . The component method [10] can be applied to<br />

composite experimental pole figures, also of multi-phase geological material of any<br />

ciystallographic symmetry .<br />

5.2 Inverse Pole Figures<br />

The mathematical procedure ofpole figure inversion includes the calculation of coefficients H<br />

of so-called inverse pole figures . While the pole figures discussed so far are defmed for one<br />

particular crystallographic direction [hkl] and variable sample orientations (compare equation<br />

(5), the inverse pole figures represent shares of main crystallographic directions, e .g . basis<br />

axis, face and body diagonal of the cubic ciystal system, in a fixed sample orientation (Fig .<br />

18 .20) . Usually, the inverse pole figure is represented as stereographic projection with respect<br />

to the crystal coordinate system KK, while the standard` pole figure is defmed as<br />

stereographic projection with respect to the sample coordinate system KP (compare Fig . 18 .5) .<br />

Fig . 18.20 : Inverse polefigure of a<br />

cold drawn Al wire (sec (21) by<br />

representation of the preferred<br />

orientations of the most relevant<br />

crystallographic directions (cubic<br />

axis [100], face-diagonal [1101 and<br />

body-diagonal [1111) inside the<br />

sample . Pole densities are shown by<br />

equilevel contour Unes in m . r. d.<br />

6.0 Examples of Texture Analyses<br />

Texture appears in a great variety . A multitude of different types is kown according to<br />

different mechanisms of texture formation during ciystallization (grain growth) and reciystal-<br />

18- 1 3

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