Abstract
The isomorphous substitution of \(\hbox {Al}^{3+}\) and/or \(\hbox {Fe}^{3+}\) cations into the erionite zeolite framework were studied through periodic density functional theory computations. Taking as reference the Mulliken charges for siliceous framework computed in previous work (Antúnez-García et al. in J Mol Struct 1059:232–238, 2014), the present results show that the basicity of ERI zeolite increases when those cations are introduced into the framework. It was also observed that when at least two \(\hbox {Si}^{4+}\) cations are isomorphically substituted by \(\hbox {Fe}^{3+}\) in the unit cell of the erionite zeolite, it acquires magnetic properties. The results show that a specific net-spin polarization (up or down) could be correlated with particular configurations of erionite zeolite, containing ferric iron.
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Acknowledgements
This research was supported by the Project SENER-CONACyT 117373, UNAM PAPIIT IN107817 Grant and RFBR-CITMA Project No. 18-53-34004 and through the basic-science proposal A1-S-33492. We also want to thank for the supercomputing time provided by the UNAM through the project LANCAD-UNAM-DGTIC-041.
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Antúnez-García, J., Galván, D.H., Petranovskii, V. et al. Theoretical study of the effect of isomorphous substitution by \(\hbox {Al}^{3+}\) and/or \(\hbox {Fe}^{3+}\) cations to tetrahedral positions in the framework of a zeolite with erionite topology. J Mater Sci 54, 13190–13199 (2019). https://doi.org/10.1007/s10853-019-03845-6
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DOI: https://doi.org/10.1007/s10853-019-03845-6