19–22 May 2025
US/Mountain timezone

Ion Pairing of Ca2+, Zn2+, and La3+ with Acetate is Enhanced in Nanopores

21 May 2025, 09:50
15m
Oral Presentation (MS17) Complex fluid and Fluid-Solid-Thermal coupled process in porous media: Modeling and Experiment MS17

Speaker

Bidemi Fashina (Geochemistry Department, Sandia National Laboratories, Albuquerque, New Mexico)

Description

Nanoscale confined systems are common in the environment and in many technological innovations. Recent studies have shown that the fundamental properties and reactivity of bulk water or unconfined surfaces change under nanoscale confinement. These confinement-imposed changes, in turn, influence several nanoscale processes. Understanding nanoscale processes within confined systems is important for predicting the fate and transport of chemical species, water treatment by nano-filtration, and the fixation of contaminants in porous materials. In this study, we investigated the impact of nanoscale confinement on the ion pairing involving Ca²⁺, Zn²⁺, and La³⁺ with CH₃COO⁻ anions. By modeling the Raman spectra of bulk and confined solutions, we quantified the complexed and uncomplexed acetate species in aqueous solutions and then in the same solutions confined within mesoporous silica with 4 nm cylindrical pores. From these values, we estimated the binding constants and standard Gibbs free energy of ion formation in solution versus in nanopores. The equilibrium constants increased by 0.09, 1.70, and 2.5 units for Ca²⁺–, Zn²⁺–, and La³⁺–CH₃COO⁻, respectively, when compared to analogous constants measured for bulk solutions. Hence, ion pair formation is more favorable in nanopores than in bulk aqueous solutions. Through density functional theory (DFT) calculations, we predicted the stabilization of ion pairs in confined and aqueous environments. In agreement with the experimental findings, the DFT-calculated thermodynamic values for the free energy of formation predict the stabilization of contact ion pairs in confined systems compared to the bulk aqueous environment. These findings have broad implications on the fate and transport of chemical species in soils and other terrestrial environments and can improve the predictive geochemical modeling of cation-anion complexes in confined systems.

Acknowledgement: SNL is managed and operated by NTESS under DOE NNSA contract DE-NA0003525.

Country United States
Water & Porous Media Focused Abstracts This abstract is related to Water
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Authors

Bidemi Fashina (Geochemistry Department, Sandia National Laboratories, Albuquerque, New Mexico) Anthony Baldo (Geochemistry Department, Sandia National Laboratories, Albuquerque, New Mexico) Heath Watts (Department of Earth, Environmental & Resource Sciences, University of Texas at El Paso, El Paso, Texas) Kevin Leung (Geochemistry Department, Sandia National Laboratories, Albuquerque, New Mexico) James Kubicki (Department of Earth, Environmental & Resource Sciences, University of Texas at El Paso, El Paso, Texas) Anastasia Ilgen (Geochemistry Department, Sandia National Laboratories, Albuquerque, New Mexico)

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