The intrinsic uniform and non-uniform contributions to the anisotropic
part of the surface energy are considered. Our analysis shows that th
e uniform part can be separated into an intrinsic and an extrinsic ter
m. The first one is due to the nematic-nematic interaction only, where
as the second one is due to the nematic-substrate interaction. They ar
e found to be of the same order of magnitude (approximate to 1 erg cm(
2)). The non-uniform part takes its origin from the spatial variation
of the elastic constants. By means of a semi-microscopic model it is s
hown that, in the framework of perfect nematic order, the extrapolatio
n length of the elastic origin is microscopic. On the contrary, if the
spatial variation of the scalar order parameter is taken into account
, simple calculations indicate that the extrapolation length is of the
order of the coherence length in the nematic phase.