The equation for the Brueckner G matrix is investigated for planar-slab geo
metry. A method for calculating the G matrix for a planar slab of nuclear m
atter is developed for a separable form of NN interaction. Actually, the se
parable version of the Paris NN potential is used. The singlet S-1(0) and t
he triplet S-3(1)-D-3(1) channel are considered The present analysis relies
on the mixed momentum-coordinate representation, where use is made of the
momentum representation in the slab plane and of the coordinate representat
ion in the orthogonal direction. The full two-particle Hilbert space is bro
ken down into the model subspace, where the two-particle propagator is cons
idered exactly, and the complementary subspace, where the local-potential a
pproximation is used, which was proposed previously for calculating the eff
ective pairing potential. Specific calculations are performed for the case
where the model subspace is constructed on the basis of negative-energy sin
gle-particle states. The G matrix is parametrically dependent on the total
two-particle energy E and the total momentum P-perpendicular to in the slab
plane. Since the G matrix is assumed to be further used to calculate the L
andau-Migdal amplitude, the total two-particle energy is fixed at the value
E = 2 mu, where mu is the chemical potential of the system under investiga
tion. The calculations are performed predominantly for P-perpendicular to =
0. The role of nonzero values of P-perpendicular to is assessed. The resul
ting G matrix is found to depend greatly on mu in the surface region. (C) 2
001 MAIK "Nauka/Interperiodica".