We explore the feasibility of vacancy condensation as the void-nucleat
ing mechanism underlying ductile fracture by void growth and coalescen
ce in single crystals at room temperature. Vacancies are presumed to b
e primarily generated by the dragging of intersection jogs. The equati
ons governing the rate of growth of voids by vacancy condensation are
derived. These equations are used to follow the evolution of vacancy c
oncentrations and void sizes in the Wang and Anderson [Acta metall. 39
, 779 (1991)] [1] Sigma 9 test. We find that, when pipe diffusions are
taken into account, the time required for the nucleation of a macrosc
opic void in the near-tip region is of the order of one minute, which
is well within the lime-scale of quasistatic fracture tests.