Glossary 241
Crystal system. There are seven crystal systems, best
classified in terms of their symmetry. They are: triclinic,
monoclinic, orthorhombic, tetragonal, cubic, trigonal, and
hexagonal. As a result of their symmetries they lead to the
seven fundamental shapes for unit cells consistent with
the 14 Bravais lattices (q.v.).
Crystallographic point group, crystal class. A point
group is a group of symmetry operations that leave at
least one point unmoved within an object when the sym-
metry operation is carried out. There are 32 crystallo-
graphic point groups (crystal classes) that contain rotation
and rotatory-inversion axes (n =1, 2, 3, 4, 6). The crystal-
lographic point groups characterize the external symme-
try of well-formed crystals.
Cubic unit cell. A unit cell in which there are three-
fold rotation axes along all four body diagonals. All axial
lengths are therefore identical by symmetry, and all inter-
axial angles must be 90
◦
(a = b = c, · = ‚ = „ =90
◦
).
Data reduction. Conversion of measured intensities,
I(hkl), to structure amplitudes |F (hkl)| or to |F
2
(hkl)|,by
application of various factors including Lorentz, polariza-
tion, and absorption corrections (q.v.).
Database. A collection of data on a particular subject, such
as atomic coordinates from crystal structure determina-
tions. These data are readily retrievable by computer.
Defect. A crystal lattice imperfection. This may be due to
impurities. A point defect is a vacancy or an interstitial
atom. A line defect is a dislocation in the crystal lattice.
Deformation density. The difference between the exper-
imental electron density in a molecule (with all its dis-
tortions as a result of chemical bonding) and the pro-
molecule density (q.v.) (a model of the molecule with a
spherical electron density around each isolated free atom).
The deformation-density map contains information on
chemical bonding, although this information is modified
by errors in the phases and the measured intensities of
the Bragg reflections and inadequacies in the calculated
scattering factors of free atoms.
Deliquescence. The property that some crystals have of
attracting and absorbing moisture from the surrounding
atmosphere and dissolving gradually, eventually becom-
ing a solution.
Density modification, solvent flattening. A computa-
tional method for improving phases, particularly when
a unit cell contains a high proportion of solvent as do
macromolecular crystals. When an electron-density map
is calculated with |F (hkl)| and an initial set of possible
relative phases, the map will probably be noisy if the
relative phases are not very good. However, the outline
of an “envelope,” the protein–solvent boundary, may be
evident. The overall density of atoms in aqueous areas
of the crystal (involving oxygen–oxygen distances near
2.7 Å) is lower than in the interior of the molecule (involv-
ing C–C, C–O, and C–N distances near 1.4 Å). An “enve-
lope” defining the approximate boundary of the molecule
is determined from the electron-density map. All of the
electron density outside this envelope, that is, the electron
density in the solvent area, is then set to a single low value
(the average for disordered water) and a new set of phases
is then determined by Fourier inversion of this “solvent-
flattened” map. The process is used to improve the phases
and may be repeated, if necessary.
Difference synthesis or difference map. A Fourier map
for which the input Fourier coefficients are the differences
between measured structure factors and those calculated
from a proposed structural model. Such a map will have
peaks at positions in which there is not enough electron
density in the trial structure, and troughs where too much
is included. It is an exceedingly valuable tool both for
locating missing atoms and for correcting the positions of
those already present in the trial structure.
Differential synthesis. A method of refining parameters
of an atom from a mathematical consideration of the slope
and curvature of the difference synthesis (q.v.) in the
region of each atom.
Diffraction. When radiation passes by the edges of an
opaque object or through a narrow slit, the waves appear
to be deflected and they produce fringes of parallel light
and dark bands. This effect may best be explained as the
interference of secondary waves generated in the area
of the slit or the opaque object. These secondary waves,
so generated, interfere with one another, and the inten-
sity of the beam in a given direction is determined by a
superposition of all the wavelets in that direction. When
light passes through a narrow slit all the waves will be
in phase in the forward direction. In any other direc-
tion, each secondary wave traveling in a given direction
will be slightly out of phase with its neighbors by an
amount that depends on the wavelength of the light and
the angle of deviation from the direct beam. The shorter
the wavelength, the more a wave is out of phase with its
neighbor. In X-ray crystallography, the radiation is X rays
and the slit is replaced by the electron clouds of atoms
in a crystal which scatter the X rays. Because the crystal
contains a regularly repeating atomic arrangement, the
beams diffracted from one unit cell may be in phase with
those from other unit cells and can reinforce each other to