The relative current density of conduction neutrons in a neutron star crust beyond the neutron drip threshold can be expected to be related to the corresponding particle momentum covector by a linear relation of the form in terms of a physically well defined mobility tensor . This result is describable as an ``entrainment’’ whose effect - wherever the crust lattice is isotropic - will simply be to change the ordinary neutron mass m to an effective mass such that in terms of the relevant number density n of unconfined neutrons we shall have . In a preceding analysis based on an independent particle treatment using Bloch boundary conditions to obtain the distribution of energy and associated group velocity as a function of wavenumber , it was shown that the mobility tensor would be given by , where is the Fermi energy. Using the approach due to Bogoliubov, it is shown here that the effect of BCS pairing with an energy gap \Delta_F and corresponding quasiparticle energy function \EE_k=\sqrt{(E_k-\mu)^2+\Delta_F^2}$ will just be to replace the Dirac distributional integrand by a smoother distribution : . It is also shown how the pairing condensation gives rise to superfluidity in the technical sense of providing (meta) stability against resistive perturbations for a current that is not too strong (its momentum must be small enough to give $2|p_i v_k^i|<\EE_k^2/|E_k-\mu|$ for all modes). It is concluded that the prediction of a very large effective mass enhancement in the middle layers of the crust will not be significantly affected by the pairing mechanism.

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