The brittle-ductile transition (BDT) has been studied in silicon single cry
stals of different orientations and purities. It is shown that the BDT temp
erature at a given loading rate can be significantly varied depending on st
ructural parameters, especially the density of cleavage defects (steps,...)
. The critical BDT temperature is raised when the cleavage defect density i
s lowered. This is explained by observations at crack tips which prove that
dislocation nucleation is highly inhomogeneous. A first preliminary attemp
t to identify nucleation sites by AFM is reported. In crystals containing h
ighly perfect cleavage cracks, dislocation formation prior to fracture in m
ode I loading could be suppressed. In such cases, a very small number of di
slocations created on purpose from remote sources, sufficed to trigger the
formation of a plastic zone as soon as they touched the crack front. Experi
mental results are compared to theoretical models and recent numerical comp
utations.