The dynamic version of the Wicke-Kallenbach diffusion cell has been used extensively for the evaluation of effective diffusion coefficients (Suzuki and Smith, 1972; Dogu and Smith, 1975; Furusawaet al., 1976;Moffatt, 1978; Baiker et ai., 1982;Wang and Smith, 1983; DoZU et al., 1987). The single-pellet moment technique has also been used for the measurement of adsorption rate and equilibrium constants (Dozu and Smith, 1976; DoEu and Ercan, 1983), as well as reaction rate parameters (Do& 1984; Do& et al., 1986). Recently, the technique has been modified for the measurement of thermal conductivity of a porous solid (DoHu et al., 1989a(DoHu et al., , 1991 and permeability (Dogu et al., 1989b;Lu et al., 1992). Boundary conditions used in the single-pellet moment theory were discussed by Burghardt and Smith (1979) and more recently by Lu et al. (1992). In the analysis of Lu et al., the validity region of the simplified boundary conditions used in most of the published literature Correspondence concerning this work should be addressed to T. Dogu.