1999
DOI: 10.1016/s0009-2509(98)00538-7
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Influence of isotherm inflection on diffusion in silicalite

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Cited by 100 publications
(87 citation statements)
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“…Then, species concentrations per unit length become functions of a continuous variable K (x = na) ≈ a −1 K n , where we leave implicit the tdependence. To develop h-RDE, one needs an appropriate description of collective or chemical diffusion in this multispecies lattice-gas system 4,5,16,17,26 incorporating the singlefile nature of diffusion.…”
Section: Hydrodynamic Regime and Reaction-diffusion Equationsmentioning
confidence: 99%
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“…Then, species concentrations per unit length become functions of a continuous variable K (x = na) ≈ a −1 K n , where we leave implicit the tdependence. To develop h-RDE, one needs an appropriate description of collective or chemical diffusion in this multispecies lattice-gas system 4,5,16,17,26 incorporating the singlefile nature of diffusion.…”
Section: Hydrodynamic Regime and Reaction-diffusion Equationsmentioning
confidence: 99%
“…A similar expression applies for the flux, J B , of B. The four diffusion coefficients, D K,K , with K, K = A or B, can be conveniently collected into a 2 × 2 diffusion tensor D. Onsager's theory 16,17,26 further shows that this tensor involves both a thermodynamic "inverse compressibility" factor and a kinetic "conductivity" factor.…”
Section: Hydrodynamic Regime and Reaction-diffusion Equationsmentioning
confidence: 99%
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