“…By probing the properties of the hydrothermally deteriorated zeolite crystallites by N M R self-diffusion measurements with methane as a probe molecule, it has been found that lattice distortions are predominantly in the vicinity of the crystallite surface, since the desorption rates (i.e., 1 / T , , ,~, ) , not the intracrystalline diffusivities, were dramatically reduced (Karger et al, 1988). In this paper, we concentrated on the application of the N M R tracer desorption measurements for determining the intracrystalline mean life, since the general measurement of the intracrystalline diffusivities was prohibited due to the small sizes of crystallites .…”