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Intracrystalline transport limitation

Understanding the adsorption, diffusivities and transport limitations of hydrocarbons inside zeolites is important for tailoring zeolites for desired applications. Knowledge about diffusion coefficients of hydrocarbons inside the micropores of zeolites is important in discriminating whether the transport process is micropore or macropore controlled. For example, if the diffusion rate is slow inside zeolite micropores, one can modify the post-synthesis treatment of zeolites such as calcination, steaming or acid leaching to create mesopores to enhance intracrystalline diffusion rates [223]. The connectivity of micro- and mesopores then becomes an... [Pg.151]

The concept of transport resistances localized in the outermost regions of NS crystals was introduced in order to explain the differences between intracrystalline self-diffusion coefficients obtained by n.m.r methods and diffusion coefficients derived from non-equilibrium experiments based on the assumption that Intracrystalline transport is rate-limiting. This concept has been discussed during the past decade, cf. the pioneering work [79-81] and the reviews [2,7,8,23,32,82]. Nowadays, one can state that surface barriers do not occur necessarily in sorption uptake by NS crystals, but they may occur if the cross-sections of the sorbing molecular species and the micropore openings become comparable. For indication of their significance, careful analysis of... [Pg.205]

It should be mentioned that—if zeolites are technically applied as formed pellets—transport limitation may be due to both intracrystalline zeolitic diffusion and long-range diffusion as just considered. Denoting the mean radii of the crystallites and of the pellets by rc and rp, respectively, the respec-... [Pg.100]

The ZLC method offers advantages of speed and simplicity and requires only a very small adsorbent sample thus making it useful for characterization of new materials. The basic experiment using an inert carrier (usually He) measures the limiting transport difiiisivity (Do) at low concentration. A variant of the technique using isotopically labeled tracers (TZLC) yields the tracer diffiisivity and counter diffusion in a binary system may also be studied by this method. To obtain reliable results a number of preliminary experiments are needed, e.g. varying sample quality, nature of the purge gas, the flow rate and, if possible, particle size to confirm intracrystalline diffusion control. [Pg.20]

If the calculated value of is equal to the measured intracrystalline lifetime, Tinira, the rate of molecular exchange between different crystals is controlled by the intracrystalline self-diffusion as the rate-limiting process. Any increase of Timn, in comparison with Tf,j L indicates the existence of transport resistances different from intracrystalline mass transport. Under the conditions of TD NMR one has A r. > Antra, thus these resistances can only be brought about by sur ce barriers. The ratio Timra/Tfn L represents, therefore, a direct measure of the influence of surface barriers on molecular transport. [Pg.356]

Studies of intracrystalline diffusion can delineate factors limiting transport within crystals and hence will aid understanding of molecule sieving and site accessibility in catalysis. One may hope to learn from basic diffusion studies how diffusion coefficients within zeolites are related to ... [Pg.2]

Fig. 56 Correlation between the actual boundary concentration (Csurf) and the relative uptake (m) at the corresponding instant of time. Three different cases are shown the mass transport is essentially limited by intracrystalline diffusion (la/D = 100), by surface barriers la/D = 0.01), and both by intracrystalline diffusion and surface resistance la/D = 1)... Fig. 56 Correlation between the actual boundary concentration (Csurf) and the relative uptake (m) at the corresponding instant of time. Three different cases are shown the mass transport is essentially limited by intracrystalline diffusion (la/D = 100), by surface barriers la/D = 0.01), and both by intracrystalline diffusion and surface resistance la/D = 1)...

See other pages where Intracrystalline transport limitation is mentioned: [Pg.751]    [Pg.386]    [Pg.238]    [Pg.152]    [Pg.264]    [Pg.357]    [Pg.402]    [Pg.75]    [Pg.79]    [Pg.122]    [Pg.22]   
See also in sourсe #XX -- [ Pg.100 ]




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