Title: Notes on Orientations, Pole Figures, Orientation Distribution
1Notes on Orientations, Pole Figures, Orientation
Distribution
- A. D. Rollett
- Spring 2001
2Relation of PFs to OD
- A pole figure is a projection of the information
in the orientation distribution. - Equivalently, can integrate along a line in the
OD to obtain the intensity in a PF.
3Fundamental Equation of Texture
- We can calculate the intensity in the pole
figure, P(w), by summing over all the symmetry
operators and integrating over the range of Euler
angles (or as a sum if the OD is in discrete
form). - wposition in PF h (hkl) S symmetry
4- First rotate the crystal with thth(,q) so as to
place the pole of interest, h, in the center of
the hemisphere, i.e. at the North pole. This
matrix can be obtained by first finding a
rotation axis, , as the vector product of 001
and h.
5(hkl)
001
t
6The rotation angle, q, is given by the inverse
cosine of the scalar product Cos(q)h3 From
this axis-angle pair, the rotation matrix, th,
can be constructed as follows.
7- Once the pole has been rotated onto the North
pole, the crystal can then be rotated freely
about the pole without affecting the position of
the pole. This rotation matrix is similar to the
intermediate rotation step described above for
constructing the orientation matrix from the
Euler angles.
8z
(hkl)
9- This is the key step in this development because
this provides the free parameter over which we
can integrate in order to find the intensity in
the pole figure, based on a line of intensity in
orientation space. A rotation, tf, about the
North pole is simply tf tf(001,z), where z is
the (free) rotation angle. Finally, we need to
rotate the pole onto the position in the pole
figure that is of interest. This is accomplished
by successive rotations about 100/RD by c and
then 001/ND by f.
10Pole Figure angles
TD
f
azimuth
c
declination
(hkl)
RD
ND
11The product of this set of 4 rotations must then
be equal to the orientation matrix, i.e.
g(f1,F,f2) (tftctzth)T tT(h,z,w) where the
matrix on the RHS contains only one free
parameter, i.e. the rotation by z about the pole
h.
12Sample Symmetry
- Add up intensities for locations in a pole figure
related by the sample symmetry. - For example, if orthorhombic sample symmetry
(mmm) then, f,-f,p-f, and pf must give same
intensity.
13Active versus Passive Rotations
- Passive rotation typical (unstated assumption in
materials literature) axis transformation. - Active rotation typical in solid mechanics (also
unstated assumption) fixed coordinate frame,
move vectors (tensors) through the space.
14Rotation of axes in the planex, y old axes
x,y new axes
y
y
v
x
q
x
N.B. Passive Rotation/ Transformation of Axes
15Rotation of vectors in the planev old vector
v new vector
y
v
v
q
x
N.B. Active rotation (in the plane)
16- Can write the following for the intensity, P, at
w(c,f) in the pole figure. - This is sometimes termed the fundamental equation
of texture analysis because, for the standard
situation in which only pole figure data are
available, this is the equation that one seeks to
invert in order to obtain the orientation
distribution.
17Summary
- Aim of derivation show how a free rotation (as
an integration parameter) is incorporated into
the orientation description. - Sum over variants related by crystal symmetry and
by sample symmetry required. - Similar analysis for inverse pole figures.