The graphite --> diamond transition in the diamond stability field can be e
ither direct or solvent-assisted. The direct transition may proceed by spre
ading a puckered basal plane of graphite in the direction perpendicular to
it. The kinetics of such a transition may be approximated by the growth of
a two-dimensional nucleus. The threshold temperature of the transition appe
ars to depend on the degree of perfection of the original graphite. Hence,
the more perfect the graphite is, the lower temperature it may transform in
to diamond. The solvent-assisted transition normally proceeds by rapid nucl
eation followed by growth of these nuclei. The kinetic model for continuous
nucleation may be applied to the early stage of such transition. The activ
ation energies for the transition can then be calculated, it is found that
these activation energies seem to vary inversely with the solubility of car
bon in these solvents at ambient pressure. Hence, the higher the amount of
carbon a solvent dissolves at ambient pressure, the more effective it can b
e as a catalyst for the graphite --> diamond transition under high pressure
. (C) 2000 Kluwer Academic Publishers.