A Hierarchical Model for Longitudinal and IntraparticleDiffusion Coefficients in Liquid Chromatography

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The model for theeffective longitudinal diffusion coefficient Deff, recently derived from the two-zone momentanalysis approach, is adapted to predict the intraparticle diffusioncoefficient Dpart of the general ratemodel for chromatography. The model for Dpart, coupled with the model for Deff, allowsus to predict with great accuracy numerical data for Deff obtained by solving the detailed diffusion-adsorptiontransport model, via the Brenner–Adler method of moments, indifferent 2D and 3D hierarchical retentive porous structures. Theproposed models make explicit the dependence of Deff and Dpart on the obstructionfactors of the macroporous and mesoporous zone, internal and externalporosity, equilibrium constant, specific surface area, and surfacediffusion coefficient. Detailed numerical simulations also allowedus to verify the inaccuracy of the parallel-connection model for Dpart when surface diffusion in the stationaryphase layer contributes significantly to the transport of the analytein the mesoporous zone.

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SummaryThe complex pore structure and storage mechanism of organic-rich ultratight reservoirs make the hydrocarbon transport within these reservoirs complicated and significantly different from conventional oil and gas reservoirs. A substantial fraction of pore volume in the ultratight matrix consists of nanopores in which the notion of viscous flow may become irrelevant. Instead, multiple transport and storage mechanisms should be considered to model fluid transport within the shale matrix, including molecular diffusion, Knudsen diffusion, surface diffusion, and sorption. This paper presents a diffusion-based semianalytical model for a single-component gas transport within an infinite-acting organic-rich ultratight matrix. The model treats free and sorbed gas as two phases coexisting in nanopores. The overall mass conservation equation for both phases is transformed into one governing equation solely on the basis of the concentration (density) of the free phase. As a result, the partial differential equation (PDE) governing the overall mass transport carries two newly defined nonlinear terms; namely, effective diffusion coefficient, De, and capacity factor, Φ. The De term accounts for the molecular, Knudsen, and surface diffusion coefficients, and the Φ term considers the mass exchange between free and sorbed phases under sorption equilibrium condition. Furthermore, the ratio of De/Φ is recognized as an apparent diffusion coefficient Da, which is a function of free phase concentration. The nonlinear PDE is solved by applying a piecewise-constant-coefficient technique that divides the domain under consideration into an arbitrary number of subdomains. Each subdomain is assigned with a constant Da. The diffusion-based model is validated against numerical simulation. The model is then used to investigate the impact of surface and Knudsen diffusion coefficients, porosity, and adsorption capacity on gas transport within the ultratight formation. Further, the model is used to study gas transport and production from the Barnett, Marcellus, and New Albany shales. The results show that surface diffusion significantly contributes to gas production in shales with large values of surface diffusion coefficient and adsorption capacity and small values of Knudsen diffusion coefficient and total porosity. Thus, neglecting surface diffusion in organic-rich shales may result in the underestimation of gas production.

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