Diffusion of normal alkanes in one-dimensional zeolites is theoretically studied on the basis of the stochastic equation formalism. The calculated diffusion coefficient accounts for the vibrations of the diffusing molecule and zeolite framework, molecule-zeolite interaction, and specific structure of the zeolite. It is shown that when the interaction potential is predominantly determined by the zeolite pore structure, the diffusion coefficient varies periodically with the number of carbon atoms of the alkane molecule, a phenomenon called resonant diffusion. A criterion for observable resonance is obtained from the balance between the interaction potentials of the molecule due to the atomic and pore structures of the zeolite. It shows that the diffusion is not resonant in zeolites without pore structure, such as ZSM-12. Moreover, even in zeolites with developed pore structure no resonant dependence of the diffusion constant can be detected if the pore structure energy barriers are not at least three times higher than the atomic structure energy barriers. The role of the alkane molecule vibrations is examined as well and a surprising effect of suppression of the diffusion in comparison with the case of a rigid molecule is observed. This effect is explained with the balance between the static and dynamic interaction of the molecule and zeolite.Zeolites attract scientific attention because of their remarkable catalytic and sorption properties. They are regular porous materials with pore size in the order of several Angstroms. Because of their structure, zeolites can exhibit molecular shape selectivity to certain molecules, which is very important for many applications of practical interest 1 . An important factor for the efficiency of each process utilizing zeolites is the rate of intracrystalline mass transfer of species. For instance, chemical reactions are catalyzed in zeolites at some active centers and, therefore, are frequently diffusion controlled since the reactants have to reach these active centers first.The methods to measure the mobility of molecules in zeolites are naturally divided in two groups 2 . The first group consists of measurements of some macroscopic integral response of the system. One can mention here, for instance, the classical absorption/desorption experiments. On this method the diffusion constant is calculated by comparing the experimental absorption/ desorption curves with exact solutions of the unsteady state diffusion equation for the particular shape of zeolite grains employed 3 . The experimental curves, however, are influenced not by the diffusion process only. In fact, there are at least three consequent processes, namely, transfer of