2018
DOI: 10.1021/acs.iecr.7b04840
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Hindrance Factor Expression for Diffusion in Random Mesoporous Adsorbents Obtained from Pore-Scale Simulations in Physical Reconstructions

Abstract: Hindered diffusion of solutes is the rate-limiting step in many processes for which random porous media play a central role as providers of adsorbing or reactive interfaces. The key to an optimized layout of these processes is the knowledge of the overall diffusive hindrance factor H(λ) = D eff,H(λ)/D m, which quantifies the degree to which diffusion through a material (represented by the effective diffusion coefficient D eff,H) is hindered compared with diffusion in the bulk liquid (represented by D m) in dep… Show more

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Cited by 61 publications
(78 citation statements)
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“…enhanced interactions with surface sulfonic acid groups or hydroxyls, but rather reects topological constraints of the pore system. This nding agrees with pore-scale diffusion simulations, 67,68 which reveal that the effective tortuosity of mesoporous SBA-15 and KIT-6 silicas depends on the size of the probe molecule. Note that this contrasts with simulations 67,68 and PFG-NMR studies of amorphous mesoporous silicas, for which effective tortuosity is independent of molecular size.…”
Section: Structure-reactivity Correlationssupporting
confidence: 87%
“…enhanced interactions with surface sulfonic acid groups or hydroxyls, but rather reects topological constraints of the pore system. This nding agrees with pore-scale diffusion simulations, 67,68 which reveal that the effective tortuosity of mesoporous SBA-15 and KIT-6 silicas depends on the size of the probe molecule. Note that this contrasts with simulations 67,68 and PFG-NMR studies of amorphous mesoporous silicas, for which effective tortuosity is independent of molecular size.…”
Section: Structure-reactivity Correlationssupporting
confidence: 87%
“…The fluid flow through shale reservoirs is a complex, multi-scale phenomenon because of a combination of phenomena including adsorption, desorption, surface diffusion along pore walls, convection (Darcy flow) and Knudsen diffusion through open pore spaces [3]. Many experimental and theoretical efforts have been carried out to understand the relationship between the morphology of porous materials and the relevant transport properties [4][5][6]. For example, Reich et al [4,5] employed a reconstruction-simulation approach to quantify the impact of degree of heterogeneity and packingscale order on hindered diffusion in mesoporous silica.…”
Section: Introductionmentioning
confidence: 99%
“…Although mesopore space and macropore space are microscopically disordered, their threedimensional physical reconstruction combined with morphological analysis as well as fluid flow and mass transport simulations yielded quantitative morphology-transport relationships for these materials. [11][12][13][14] A summary of relevant morphological features of silica monoliths, which are also employed in the present work, and useful further background information can be found in Section S1 and Figure S1 of the Supporting Information (SI).…”
Section: Introductionmentioning
confidence: 99%