
Glass diffraction 199
no well-defined geometrical order within it. The best model to date
of such glass consists of random chains, nets, and three-dimensional
arrays of SiO
4
tetrahedra, linked together through oxygen atoms, with
appropriately situated cations. Many attempts have been made to fit
models with different kinds of short-range order to the observed dif-
fraction patterns and to other quantitative physical and chemical data
available on various glasses. This is done in an effort to define more pre-
cisely what might be meant by “the structure of glass” (Warren, 1940;
Tanaka et al., 1985).
In contrast to the traditional glasses that are the products of fusion
and can be “thawed” and reworked without crystallizing, there are
now known to be many other glass-forming composition systems and,
as a result, there are several ways of generating glasses and other
amorphous materials. Each of these gives rise to properties that are
useful. For example, amorphous metal films can be made by “splat
cooling”—that is, a jet of liquid metal is directed onto a cold surface and
therefore is cooled to a solid so rapidly from the melt that it has been
deprived of the time required for crystal organization. Another indus-
trial example is provided by the use of a chemical reaction in the gas
phase to generate an extremely fluffy amorphous “soot” that may be
sintered and compressed to three-dimensional solidity without crystal-
lizing. Optical-waveguide–laser communication technology depends in
large measure on the purity, composition control, and perfection of
such processes, achievable by starting with pure gases, such as silicon
tetrafluoride and oxygen, and reacting them to form a condensed phase
of pure silica “soot” where, presumably, the surface is both highly
energetic and unique such that particles “join” under pressure without
melting (sintering) to form a continuum; such sintering without melt-
ing precludes the possibility of any crystallization. A third example is
provided by glass-ceramics, which, although noncrystalline as formed,
cannot be heated to the softening point because they undergo crys-
tallization from the solid state; this crystallization must be controlled
carefully in order to obtain a glass-ceramic with the desired physical
properties.
The peak near 1 Å represents the intramolecular O–H interaction and that at 2.9 Å
represents hydrogen-bonding interactions between oxygen atoms of neighboring water
molecules. A sequence of broad peaks follows, notably those near 4.5 Å and 7 Å, and they
may be attributed to preferred distances of separation for second and higher coordination
shells. At distances large compared with atomic dimensions, and also with increasing
temperature, the values of G(r) merge to unity—that is, to the value for a structureless
liquid.
In liquid water the average coordination in the first shell represents about 4.4 mole-
cules (independent of temperature), compared with exactly 4 molecules in ice, in support
of the idea that the increase in density when ice melts is due to a small increase in
the average coordination number in the first coordination shell. Other details in the
distribution curves are compatible with an approximately tetrahedral coordination of
molecules, as found in ice.
The curves were kindly provided by Dr. A. H. Narten from Oak Ridge National
Laboratory Report 4378, June 1970.