Many of the important properties of colloidal
systems are determined directly or indirectly by the electrical charge (or
potential) on the particles. Adsorption of ions and dipolar molecules is
determined by, and also determines, this charge and potential distribution.
The potential distribution itself determines the interaction energy between
the particles, and this is in many cases responsible for the stability of
particles towards coagulation and for many aspects of the flow behaviour of
the colloidal suspension. It is also possible to correlate the zeta
potential with the sedimentation behaviour of colloidal systems and
with the flotation behaviour of mineral ores.
Since much of the theoretical basis of colloid
chemistry demands a knowledge of the potential distribution around the
particles, it is essential that we have access to accurate knowledge of that
potential.
The most important techniques used to acquire
information about these potentials are
(i) the measurement of
volta
potential differences in surface chemistry and (ii) the measurement of zeta
potential. Despite the very real limitations of both of these procedures
they remain the most valuable ones we haw at present.
There are many situations in which the zeta
potential is used as a parameter in its own right characterizing the
outer, diffuse part of the double layer and hence valuable for discussing
the interaction between particles or the flow of liquid through membrane
pores or porous plugs. There are other situations in which one wishes to
construct a picture of the charge and potential distribution across the
entire interfacial region, and in this case potential values may be taken as
part of the input information.
There are also many situations, especially in
the field of biochemistry, in which one is more interested in separating a
complex mixture of components with differing mobilities rather than in
attempting to understand those mobilities in a fundamental way.