Quantification of the confinement effect in microporous materials

• Published in: Physical chemistry chemical physics : PCCP Vol. 15; no. 15; pp. 5648 - 5657
• Main Authors: GARCIA, Edder J, PEREZ-PELLITERO, Javier, JALLUT, Christian, PIRNGRUBER, Gerhard D
• Format: Journal Article
• Language: English
• Published: Cambridge Royal Society of Chemistry 21.04.2013
• Subjects: Chemical and Process Engineering; Chemical engineering; Chemical Sciences; Chemistry; Colloidal state and disperse state; Confinement; Correlation; Curvature; Engineering Sciences; Exact sciences and technology; Gaussian; General and physical chemistry; Mathematical analysis; Mathematical models; Methodology; Porosity; Porous materials; Porous material; Confinement; Microporosity; ACL
• DOI: 10.1039/c3cp44375b
• ISSN: 1463-9076

The confinement effect plays a key role in physisorption in microporous materials and many other systems. Confinement is related to the relationship between the pore geometry (pore size and topology) and the geometry of the adsorbed molecule. Geometric properties of the porous solid can be described using the concepts of Gaussian and mean curvatures. In this work we show that the Gaussian and mean curvatures are suited descriptors for mathematically quantifying the confinement of small molecules in porous solids. A method to determine these geometric parameters on microporous materials is presented. The new methodology is based on the reconstruction of the solid's accessible surface. Then, a numerical calculation of the Gaussian and mean curvatures is carried out over the reconstructed mesh. On the one hand, we show that the local curvature can be used to identify the most favourable adsorption sites. On the other hand, the global mean curvature of the solid is correlated to the heat of adsorption of CO2 and CH4 on several zeolites and MOFs. A theoretical justification for this empirical correlation is provided. In conclusion, our methodology allows for a semi-quantitative estimation of confinement, applicable to any pore geometry, independent of the chemical composition, and without the need for applying a force field.