The model for the effective longitudinal diffusion coefficient Deff, recently derived from the two-zone moment analysisapproach, is adaptedto predictthe intraparticle diffusion coefficientDpart ofthegeneralratemodelforchromatography.The model for Dpart, coupled with the model for Deff, allows us to predict with great accuracy numerical data for Deff obtained by solving the detailed diffusion-adsorption transport model, via the Brenner−Adler method of moments, in different 2D and 3D hierarchical retentive porous structures. The proposed models makeexplicitthedependenceofDeff andDpart ontheobstruction factors of the macroporous and mesoporous zone, internal and external porosity, equilibrium constant, specific surface area, and surfacediffusioncoefficient.Detailednumericalsimulationsalsoallowedustoverifytheinaccuracyoftheparallel-connectionmodel for Dpart when surface diffusion in the stationary phase layer contributes significantly to the transport of the analyte in the mesoporous zone.
A Hierarchical Model for Longitudinal and Intraparticle Diffusion Coefficients in Liquid Chromatography / Adrover, Alessandra; Desmet, Gert. - In: ANALYTICAL CHEMISTRY. - ISSN 0003-2700. - 97:39(2025), pp. 21351-21357. [10.1021/acs.analchem.5c02838]
A Hierarchical Model for Longitudinal and Intraparticle Diffusion Coefficients in Liquid Chromatography
Adrover, Alessandra
;
2025
Abstract
The model for the effective longitudinal diffusion coefficient Deff, recently derived from the two-zone moment analysisapproach, is adaptedto predictthe intraparticle diffusion coefficientDpart ofthegeneralratemodelforchromatography.The model for Dpart, coupled with the model for Deff, allows us to predict with great accuracy numerical data for Deff obtained by solving the detailed diffusion-adsorption transport model, via the Brenner−Adler method of moments, in different 2D and 3D hierarchical retentive porous structures. The proposed models makeexplicitthedependenceofDeff andDpart ontheobstruction factors of the macroporous and mesoporous zone, internal and external porosity, equilibrium constant, specific surface area, and surfacediffusioncoefficient.Detailednumericalsimulationsalsoallowedustoverifytheinaccuracyoftheparallel-connectionmodel for Dpart when surface diffusion in the stationary phase layer contributes significantly to the transport of the analyte in the mesoporous zone.I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.


