We show, using an atomistic model with a Stillinger-Weber potential (S
WP), that in the absence of reconstruction, the basic assumption of th
e Peierls-Nabarro (PN) model that the dislocation core is spread withi
n the glide plane is verified for silicon. The Peierls stress (PS) obt
ained from the two models are in quantitative agreement (approximate t
o 0.3 mu), when restoring forces obtained from first principles genera
lized stacking-fault energy surfaces are used in the PN model [B. Joos
, Q. Ren, and M. S. Duesbery, Phys. Rev. B 50, 5890 (1994)]. The PS wa
s found to be isotropic in the glide plane. Within the SWP model no ev
idence of dissociation in the shuffle dislocations is found bur, glide
sets do separate into two partials.