Recent theories of gas chromatography and similar separation methods only satisfactorily solve the linear type of equilibrium chromatography’-5 and some simple types of non-equilibrium chromatography o--O.The present communication describes a theory which simultaneously takes .into account the longitudinal diffusion in the mobile phase, the radial diffusion inside the porous grains of the packing material, the finite rate of mass transfer through the boundary (which may comprise diffusion in the thin layer of the immobile phase on the surface of the grains) and the sorption on the internal surface of grains. In spite of the fact that no analytical solution can be given even for the simplest model of the column with a granular filling, which will be described below, it is possible to obtain valuable informatlon based on the known Laplace transform of the solution. Let an infinitely long column with section $Jbe uniformly filled with the packing consisting of small porous grains of uniform size having the shape of spheres (index v = 3) or “infinite” cylinders (V = 2) of radius 22 or “infinite” plates (v = I) with thickness d = 2R. Among the internal co-ordinates only the co-ordinate Y, which is measured in the direction from centers (or axes or planes) of symmetry perpendicularly to the surface of the grains, is significant. The area of the geometric surface of grains per unit volume of the column is given by the formula SV = v(x - a)/ri where txis the external porosity, A homogeneous distribution of pores in the grains is supposed. The average area of boundary surface between pores and the external free volume per unit volume of the column is PV = /3S, where f3 is the internal porosity. “Incompressible” carrier flows through the free external volume along axis z of the column, with velocity ZG.The rate of flow through the whole cross section J!Jof the column is then given by $ = +zc. It is assumed that the concentration C of the compound being separated in the free volume is the same in the whole cross section of the column at any moment, thus depending only on the longitudinal co-ordinate z and time f. The flow of the given compound is defined hy the velocity of the carrier and by the diffusion and therefore it may be written as follows:
ac
ac
z+~~az-“~g=Q~
82C
The grain is presumed to be small enough so that the concentration C of the given compound may be assumed to be the same along the whole grain at any moment, only being dependent on the location of the grain center. Inside the gmins, J. Clwomalog.,
19 (1965)
237-243
E. ltTJ6ERA
238
concentrations c (Y, a, i) and 9t(L/,z, t) do not depend on angular co-ordinates. Further, sorption on the internal surface of the grains (boundary between pores and the solid part of grains) may occur. Then it is valid for concentration in the pores:
ac -A
at
D?
@G
U-I
&e-~&z
ac >
=
Qn=--8
where c is the concentration in the pores and 31is the concentration of the sorbed compound on the internal surface; both concentrations are given per unit volume of the pores. For the flow of the compound in the direction of the normal to the external surface of the pores ,
and since Pv is the external pore area in unit volume of the column, the rate of decay of the substance from the pores in unit volume is equal to jR& and also to cxQC,as the rate of influx of the compound into the carrier is the same as the rate of decay from the pores. Hence
Further, due to the symmetry aG
of the grains the following condition is valid
I
ar
It is assumed that the transfer and sorption equations’ : and
Qc = ---Wc(Ic&
-
c/r=R)
Qn =
-
n)
-H,(K,G
rates are defined by the linear
where K, and K, are equilibrium constants and Hc and Hn are mass transfer coefficients. The system of equations is solved for these initial and boundary conditions: