The surface nucleation of high-quartz solid solution crystals at fract
ured surfaces of glasses of the stoichiometric cordierite composition
(2MgO . 2Al(2)O(3) . 5SiO(2)) was studied by optical microscopy. Parti
cular attention was focused on the nucleation kinetics. A constant nuc
leation density, N approximate to 10(-4) mu m(-2), was found not to be
significantly influenced by the time and the temperature of nucleatio
n treatment. Even a very fast heating of samples employing heating rat
es up to 1200 K/min does not lower N substantially. However, for small
average crystal diameters (<20 mu m) a distribution of crystal size i
n the same order of magnitude is detectable indicating a simultaneous
appearance of both measurable nucleation rates and growth velocities.
It can be concluded that the surface nucleation of mu-cordierite occur
s during the thermal treatment from a limited number of preferred nucl
eation sites; these sites are ''used up'' rapidly enough to cause a st
rong saturation effect of nucleation, but slow enough to cause a cryst
al size distribution at the same time. The surface nucleation rate, I-
s, was calculated from the observed distribution of crystal sizes. I-s
progressively increases with rising temperature similar to the crysta
l growth velocity indicating a broad temperature range of essential nu
cleation activity. The latter must be regarded as the main obstacle to
measure or to control surface nucleation density by means of two-step
nucleation and growth treatments and must therefore be claimed to be
mainly responsible for the observed constancy of N.