Appendix 4 223
spacings a and b. Thus atoms may be imagined to be present at the crystal
lattice points in Figure A4.1 (they will normally also be present at other points,
lying between these crystal lattice points, but spaced identically in each unit
cell). If scattering is to occur in the direction specified by ¯
, then the radiation
scattered in that direction from every crystal lattice point must be exactly in
phase with that from every other crystal lattice point. (If scattering from any
two crystal lattice points is somewhat out of phase, that from some other pair
of crystal lattice points will be out of phase by a different amount, and the
net sum over all crystal lattice points, considering the crystal to be essentially
infinite, will consist of equal positive and negative contributions and thus will
be zero.)
Consider waves 1 and 2, scattered by atoms separated by a (Figure A4.1). For
these waves to be just in phase after scattering, the path difference (PD
1
)must
be an integral number (h) of wavelengths (ray 1 travels a distance q, while ray
2 travels a distance p):
PD
1
= p − q = a cos ¯ − a cos ¯
= hÎ (A4.1)
Similarly, the path difference for waves 1 and 3, scattered by atoms separated
by b, must also be an integral number of wavelengths (ray 3 travels a distance
r + s more than ray 1):
PD
2
= r + s = b sin ¯ + b sin ¯
= kÎ (A4.2)
where k is some integer.
Both of these conditions must hold simultaneously. They are sufficient con-
ditions to ensure that the scattering from all atoms in this two-dimensional
net will be in phase in the direction ¯
. In three dimensions, another similar
equation, corresponding to the spacing in the third (noncoplanar) direction,
must be added. Each of these equations describes a cone. In three dimensions,
the three cones intersect in a line corresponding to the direction of the diffracted
beam, such that the conditions hÎ =PD
1
, kÎ =PD
2
, and lÎ =PD
3
all are satisfied
simultaneously. This is why, when a three-dimensional crystal diffracts, there
are very few diffracted beams for any given orientation of the incident beam
with respect to the (stationary) crystal. The chance that all three conditions will
be satisfied at once is small.
Now let us see how this set of conditions can be related to the Bragg equation.
Consider several parallel planes, I, II, and III, each passing through a set of
crystal lattice points and making equal angles, Ë, with the incident and scattered
beams (Figure A4.2). The planes make an angle · with the a axis. The angles ¯
and ¯
are defined as in Figure A4.1, and so
Ë = ¯ + · = ¯
− · (A4.3)
Substituting for ¯ and ¯
from Eqn. (A4.3) into Eqns. (A4.1) and (A4.2), we find
hÎ =2a sin · sin Ë (A4.4)
kÎ =2b cos · sin Ë (A4.5)