By
using a mass balance equation, we deduce an effective equation
for the concentration of adsorbed particles that considers the surface
diffusion of the particles and an adsorption–desorption process
inside a pore of irregular shape. This equation, together with the
generalized Fick–Jacobs equation for the bulk diffusion, allows
us to quantify the augment in the effective flux through a porous
material due to the migration of the gas material along the surface.
The equation for the surface concentration has a similar structure
to the well-known Fick–Jacobs equation and it takes explicitly
into account the shape of the pore through the width and length of
the walls, making our model an important tool in the understanding
of the interaction of diffusion and adsorption in porous materials
where the length of the pores is greater than its width. In this work
we predict the profile for the fractional surface coverage as a function
of the geometry, the surface and bulk diffusion coefficients, and
the isotherm of the process in several illustrative situations that
permit us to prove that the effective diffusion coefficients augments
with the surface diffusion, that the surface diffusion can give place
to internal fluxes in opposite directions between bulk and surface
particles, and finally that the diffusivity of adsorbed particles
is greater in the narrow regions of the pore, in contrast with what
happens to bulk particles. Our description predicts very interesting
couplings between bulk and surface diffusion that occur locally and
are regulated by the adsorption–desorption kinetics.