Experimental data for oxygen precipitation densities in Czochralski-grown s
ilicon following multistep annealing treatments are compared with predictio
ns from a coupled-flux model for time-dependent nucleation. This is a more
correct model for diffusion-controlled nucleation processes than is the cla
ssical theory of nucleation since it directly couples the two stochastic fl
uxes of interfacial attachment and long-range diffusion. Quantitative agree
ment is obtained between the measured and calculated densities for nucleati
on temperatures greater than 650 degrees C. Good agreement is obtained for
lower temperatures if the oxygen diffusion rate is taken to be larger than
is predicted from high-temperature diffusion data. The fit values for the d
iffusion coefficient from the nucleation data are in good agreement with re
cent results from dislocation-unlocking experiments. The oxygen loss calcul
ated by coupled-flux nucleation and diffusion-limited growth agrees with th
e experimental observations. Classical theory nucleation calculations predi
ct a much greater oxygen loss, signaling the failure of the theory to corre
ctly treat nucleation when long-range diffusion is important, true in most
solid-state precipitation processes. (C) 2000 American Institute of Physics
. [S0021-8979(00)00921-X].