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Abstract

Inelastic Neutron Scattering Study of Brønsted Acidity and Water Confinement in Zeolites †

1
Institute Laue-Langevin, 71 Avenue des Martyrs, 38000 Grenoble, France
2
Instituto de Tecnologia Quimica, Avda. Los Naranjos s/n, 46022 Valencia, Spain
*
Author to whom correspondence should be addressed.
Presented at the 37th International Symposium on Dynamical Properties of Solids (DyProSo 2019), Ferrara, Italy, 8–12 September 2019.
Proceedings 2019, 26(1), 47; https://doi.org/10.3390/proceedings2019026047
Published: 5 September 2019
(This article belongs to the Proceedings of The 37th International Symposium on Dynamical Properties of Solids)
Zeolites, crystalline and microporous aluminosilicates, are one of the most important groups of functional materials. Zeolites are widely used as solid acid catalysts in petroleum refinery and petrochemical industries. Zeolites can be described as microcoporous polymorphs of quartz. Whilst quartz is SiO2, zeolites asmit the isomorphous substitution of Si by many tetrahedrally coordinated atom, typically Al (Si4+ à Al3+ + H+). In this way, the Si/Al ratio gives the number of acid sites, but not their location and strength.The catalytic properties of a zeolite depend strongly on its acidity, and this in turns depends on: the total number of acid sites, their individual strength, and their individual location. These three factors are strongly correlated. Geometric parameters that are defined by the location of the acid site (i.e., bond angles and lengths around the acid site) make a remarkable contribution to the acid strength. It was found that the strong acid sites have the trend to be found in relatively small micropores [1].
In the present work we study the zeolite LTA Si/Al = 40 (only one acid site per unit cell). The structure of LTA zeolite has the micropores consisting of large and small cavities. Inelastic neutron scattering (INS) has been used to study the acid sites of the LTA zeolite with different Si/Al ratios. There are two groups of bands: the first one found at 1050–1100 cm−1 that corresponds to the SiOH in-plane bending and another one found near 400–500 cm−1 which is attributed to the out-of-plane bending. These bending modes of the acid site are not no possible to measure with IR spectroscopy since these bands overlap with the strong bands from the zeolite framework. The combination of an extremely high quality of the samples and the sensitivity of the instrument allows to detect with high precision the acid sites of LTA Si/Al = 40 and obtain information about its position. In order to fully understand the INS spectra we performed ab-initio calculations [2,3].
In addition the polar properties of zeolites can be nicely tuned by selecting the appropriate chemical composition and concentration of structural defects in their frameworks. In the present study we were particularly interested about the mechanism of water adsorption on small pore zeolites and the influence of the polarity of the zeolite cavities in the clustering of water molecules when adsorbed in confined spaces, since there is controversy on the formation of hydroxonium cations when water is adsorbed on acid zeolites, and in case of hydroxonium formation, who many water molecules participate into the hydroxonium species. The simple framework of the chabazite makes this zeolite and ideal candidate for the INS study of adsorbed molecules with theoretical approaches in order to provide a deep understanding on the influence of the polarity of zeolite on the clustering of adsorbed water [4].

References

  1. Katada, N.; Suzuki, K.; Noda, T.; Sastre, G.; Niwa, M. Correlation between Brønsted Acid Strength and Local Structure in Zeolites. J. Phys. Chem. C 2009, 113, 19208–19217. [Google Scholar] [CrossRef]
  2. Lemishko, T.; Valencia, S.; Rey, F.; Jiménez-Ruiz, M.; Sastre, G. Inelastic Neutron Scattering Study on the Location of Brønsted Acid Sites in High Silica LTA Zeolite. J. Phys. Chem. C 2016, 120, 24904–24909. [Google Scholar] [CrossRef]
  3. Lemishko, T.; Jiménez-Ruiz, M.; Rey, F.; Valencia, S.; Blasco, T.; Vidal Moya, A.; Sastre, G. Inelastic Neutron Scattering Study of the Aluminum and Brønsted Site Location in Aluminosilicate LTA Zeolites. J. Phys. Chem. C 2018, 122, 11450–11454. [Google Scholar] [CrossRef]
  4. Jimémez-Ruiz, M.; Gahle, D.; Lemishko, T.; Valencia, S.; Sastre, G.; Rey, F. Evidence of Hydronium Formation in Water-chabazite Zeolite Using INS experiments and ab-initio Molecular Dynamics Simulations. Manuscript in preparation.

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MDPI and ACS Style

Jiménez-Ruiz, M.; Lemishko, T.; Valencia, S.; Sastre, G.; Rey, F. Inelastic Neutron Scattering Study of Brønsted Acidity and Water Confinement in Zeolites. Proceedings 2019, 26, 47. https://doi.org/10.3390/proceedings2019026047

AMA Style

Jiménez-Ruiz M, Lemishko T, Valencia S, Sastre G, Rey F. Inelastic Neutron Scattering Study of Brønsted Acidity and Water Confinement in Zeolites. Proceedings. 2019; 26(1):47. https://doi.org/10.3390/proceedings2019026047

Chicago/Turabian Style

Jiménez-Ruiz, Mónica, Tetiana Lemishko, Susana Valencia, German Sastre, and Fernando Rey. 2019. "Inelastic Neutron Scattering Study of Brønsted Acidity and Water Confinement in Zeolites" Proceedings 26, no. 1: 47. https://doi.org/10.3390/proceedings2019026047

APA Style

Jiménez-Ruiz, M., Lemishko, T., Valencia, S., Sastre, G., & Rey, F. (2019). Inelastic Neutron Scattering Study of Brønsted Acidity and Water Confinement in Zeolites. Proceedings, 26(1), 47. https://doi.org/10.3390/proceedings2019026047

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