Effect of interlayer hydration on CO2 adsorption in iron-montmorillonite: A DFT study

Authors

Triati Dewi Kencana Wungu1,2*  ID,  Husni Ihsudha3 ID,  Muhammad Nauval Farras Russamsi3 ID,  Sparisoma Viridi1,2 ID,  Suprijadi1,4 ID,  Yoshitada Morikawa5 ID
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1 Nuclear Physics and Biophysics Research Group, Faculty of Mathematics and Natural Sciences, Institut Teknologi Bandung, Bandung 40132, Indonesia
2 Research Center for Nanoscience and Nanotechnology, Institut Teknologi Bandung, Bandung 40132, Indonesia
3 Department of Nanotechnology, Graduate School of Multidisciplinary Science and Technology, Institut Teknologi Bandung, Bandung 40132, Indonesia
4 Instrumentation and Computational Physics Research Group, Faculty of Mathematics and Natural Sciences, Institut Teknologi Bandung, Bandung 40132, Indonesia
5 Department of Precision Engineering, The University of Osaka, Suita 565-0871, Japan
Article ID: 859
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DOI:

https://doi.org/10.18686/cest859

Keywords:

CO2 adsorption; iron-montmorillonite; interlayer hydration; DFT+U; physisorption; carbon capture and storage

Abstract

Growing atmospheric CO2 concentrations have intensified the demand for efficient carbon capture and storage (CCS) systems. Montmorillonite (MMT), a smectite clay mineral, is widely studied for its structural flexibility and CO2 intercalation capacity. This study evaluates iron-modified montmorillonite (Fe-MMT) as a CO2 adsorbent using density functional theory (DFT), systematically investigating a hydration gradient of zero to four interlayer water molecules in a fully periodic Fe-MMT model to examine the interplay between interlayer swelling, water content, and CO2 adsorption. The Fe-MMT model was constructed via Fe2+ ion-exchange substitution (verified by charge balance and a high-spin magnetic moment of 3.92 μB), and analyzed using spin-polarized DFT+U (U = 4.0 eV) with the Grimme DFT-D2 dispersion correction. Under dry conditions, CO2 adsorption requires +1.26 eV of interlayer widening energy while releasing only −0.89 eV of binding energy, giving a net endothermic balance of +0.37 eV that is energetically unfavorable. Within the hydration range investigated (n = 0–4), three interlayer water molecules yield the most favorable adsorption condition, with an adsorption energy of −0.37 eV at the ground-state DFT level, eliminating the dry-state widening penalty and enabling favorable CO2 adsorption. PDOS and charge density analyses show that Fe modifies the local interlayer electronic environment, while CO2 stabilization at n = 3 H2O is governed primarily by long-range dispersion and electrostatic interactions through the hydrogen-bonded water network rather than direct Fe–CO2 orbital overlap. These results identify Fe-MMT as a promising CCS candidate, with interlayer hydration as a key parameter for optimizing CO2 capture performance.

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Published

2026-10-08

How to Cite

Wungu, T. D. K., Ihsudha, H., Russamsi, M. N. F., Viridi, S., Suprijadi, & Morikawa, Y. (2026). Effect of interlayer hydration on CO2 adsorption in iron-montmorillonite: A DFT study. Clean Energy Science and Technology, 4(5). https://doi.org/10.18686/cest859