23 8
Chapter 2
where Eq. 2.129 is forward (-i) and Eq. 2.128 is reverse (+i) Fourier
transforms. Here, @(h) is the function defined in the reciprocal space, i.e. the
scattered amplitude; p(x) is the corresponding function defined in the direct
space, e.g. p(x) is the electron density when scattering of x-rays is of
concern or it is the nuclear density when scattering of neutrons on nuclei is
considered; h and x are the coordinate vectors in the reciprocal and direct
spaces, respectively;
V*
and
V
are, respectively, reciprocal and direct space
volumes, and
i
=
fi
.
Both integrals do not require assumption of periodicity and they can be
used to calculate the scattered amplitude or the corresponding density
function of any direct or reciprocal object, respectively. For example, Eq.
2.128 results in the atomic scattering factor,
flsinelh)
cc
I@(h)l, when the
integration is performed for an isolated atom.
In
this case, p(x) is the
electron density distribution in the atom, which is usually obtained from
quantum mechanics.
Considering a crystal, in which the electron density function is periodic,
the integral in Eq. 2.128 can be substituted by a sum:
F(h)
=
v
p(x)
exp[2ni(h
.
x)]
X
where P(h) is the structure amplitude at a reciprocal lattice point h,
V
is the
volume of the unit cell of the direct lattice and the summation is carried over
all possible coordinate vectors, x, in the unit cell for a specific h.
When Eq. 2.130 is compared with Eq. 2.87, it is easy to see that the
distribution of the electron density in the unit cell is modeled by
n products,
g'P(sinelhlfJ(sinelh), where
g',
P
and
f
j
are the population, temperature and
scattering factors of the
jth
atom, respectively, and the summation ranges
over all atoms (from 1 to n) that are present in the unit cell.
Similar substitution of the forward Fourier integral (Eq. 2.129) results in
the following sum, which enables one to calculate the distribution of the
electron (or nuclear) density in the unit cell from the known structure
amplitudes:
1
p(x)
=
-
~(h) exp[- 2ni(h
.
x)]
v
h
Here the summation is carried over all reciprocal lattice points, h, for a
given coordinate vector,
x.
The last equation has exceptional practical
importance as it allows one to convert the array of numbers
-
the observed
structure amplitudes obtained from the experimentally measured intensities
-