Theoretical insights into seawater metal ion binding on β-d-ribose: site selectivity, thermodynamics, and electronic
Ayoub Kanaani1,2, Mahmood Akbari1, Alireza Vakili3
1UNESCO-UNISA-iThemba LABS/NRF Africa Chair in Nanoscience and Nanotechnology, College of Graduate Studies, University of South Africa (UNISA) Muckleneuk Ridge, P.O. Box 392 Pretoria South Africa makbari@tlabs.ac.za.
Abstract:
Metal ion contamination of seawater poses growing environmental and public health challenges, driving demand for sustainable, selective adsorbents. Here, we employ density functional theory (DFT) at the (M06-2X/6-311++G(d,p) level with implicit aqueous solvation (PCM) to investigate the adsorption of seawater metal ions (Na+, K+, Ca2+, Mg2+, Fe2+, Zn2+) onto β-d-ribose. Among six evaluated coordination sites, Site 5 consistently exhibited the strongest binding for all cations, attributable to its highly nucleophilic oxygen atoms. The binding affinity follows the order Fe2+>> Zn2+ > Mg2+ >> Ca2+ > K+ ≥ Na+, consistent with the cation charge density and M-O bond lengths. NBO second-order perturbation energies E (2) (kcal mol-1) further reflect this trend: Fe2+ (120.30) > Zn2+ (87.27) > Mg2+ (64.94) > Ca2+ (24.84) > Na+ (19.38) > K+ (5.39). Divalent cations, particularly Fe2+, exhibit significantly stronger interactions and greater charge-transfer stabilization compared to monovalent ions, as corroborated by AIM analysis showing the highest electron density at the bond critical point (ρ) for the Fe2+⋯Ri complex. Global reactivity descriptors further confirm the electronic stability and relative softness of the resulting complexes. Overall, β-d-ribose shows promise as a bio-based scaffold for selective ion capture with potential applications in desalination and environmental remediation.
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