{"title":"Gold(I)-bisulfite complexation in hydrothermal nanodroplets: A molecular dynamics study","authors":"Wallace C.H. Hui, Kono H. Lemke","doi":"10.1016/j.gca.2025.01.015","DOIUrl":null,"url":null,"abstract":"Water nanodroplets present a unique environment for gold hydrothermal transport, with fluid properties in aqueous nanodroplets distinct from bulk liquid and vapor phases. By performing classical and <ce:italic>ab initio</ce:italic> molecular dynamics simulations, we have probed the stability of water nanodroplets (H<ce:inf loc=\"post\">2</ce:inf>O)<ce:italic><ce:inf loc=\"post\">n</ce:inf></ce:italic> (<ce:italic>n</ce:italic> = 100, 1000) at 25 °C and 100 °C. The solvation and complexation of gold(I)-bisulfite AuHSO<ce:inf loc=\"post\">3</ce:inf> in nanodroplet environments were also examined, with a particular focus on surface and interior solvation. Classical TIP4P/2005 molecular dynamics simulations reveal extreme densities in the interior of (H<ce:inf loc=\"post\">2</ce:inf>O)<ce:inf loc=\"post\">100</ce:inf> and (H<ce:inf loc=\"post\">2</ce:inf>O)<ce:inf loc=\"post\">1000</ce:inf> nanodroplets compared to droplet surface regions. At 25 °C, the interior region of (H<ce:inf loc=\"post\">2</ce:inf>O)<ce:inf loc=\"post\">100</ce:inf> exhibits fluctuating densities at 1.016–1.079 g/cm<ce:sup loc=\"post\">3</ce:sup>, with two maxima at 1.079 g/cm<ce:sup loc=\"post\">3</ce:sup> and 1.074 g/cm<ce:sup loc=\"post\">3</ce:sup>, corresponding to pressures of ∼ 2.23 kbar and 2.07 kbar, respectively; Reduced densities are predicted for the larger (H<ce:inf loc=\"post\">2</ce:inf>O)<ce:inf loc=\"post\">1000</ce:inf> systems, these being 1.013 g/cm<ce:sup loc=\"post\">3</ce:sup> (25 °C, 370 bar) and 0.968 g/cm<ce:sup loc=\"post\">3</ce:sup> (100 °C, 220 bar). The outer regions, on the other hand, featured densities intermediate between saturated liquid and vapor conditions, as part of a transition from liquid to vapor-like densities at the edge of the droplet. Born-Oppenheimer molecular dynamics simulations at 100 °C show that the gold(I)-bisulfite complex H<ce:inf loc=\"post\">2</ce:inf>O-AuHSO<ce:inf loc=\"post\">3</ce:inf> maintains a near linear solvation structure (θ<ce:inf loc=\"post\">O-Au-S</ce:inf> = 172°-174°) in bulk aqueous fluids and at surface and interior sites of (H<ce:inf loc=\"post\">2</ce:inf>O)<ce:inf loc=\"post\">100</ce:inf> nanodroplets. Distance constrained simulations reveal that, upon extension of the gold(I)-bisulfite Au-S contact (equilibrium <ce:italic>r</ce:italic><ce:inf loc=\"post\">Au-S</ce:inf> = 2.3 Å), HSO<ce:inf loc=\"post\">3</ce:inf><ce:sup loc=\"post\">−</ce:sup> is displaced by a water molecule, forming a two-water solvation shell around Au<ce:sup loc=\"post\">+</ce:sup>. Thermodynamic integration gives gold(I)-bisulfite dissociation energies (ΔG) of 17.65 ± 0.37 kcal/mol (bulk), 20.22 ± 0.38 kcal/mol (nanodroplet surface), and 18.31 ± 0.31 kcal/mol (nanodroplet interior). Our <ce:italic>ab initio</ce:italic> molecular dynamics results demonstrate that water nanodroplets are stable at hydrothermal conditions and would play an important role in the speciation and transport of gold in volcanic and hydrothermal vapors.","PeriodicalId":327,"journal":{"name":"Geochimica et Cosmochimica Acta","volume":"31 1","pages":""},"PeriodicalIF":4.5000,"publicationDate":"2025-01-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Geochimica et Cosmochimica Acta","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.1016/j.gca.2025.01.015","RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
引用次数: 0
Abstract
Water nanodroplets present a unique environment for gold hydrothermal transport, with fluid properties in aqueous nanodroplets distinct from bulk liquid and vapor phases. By performing classical and ab initio molecular dynamics simulations, we have probed the stability of water nanodroplets (H2O)n (n = 100, 1000) at 25 °C and 100 °C. The solvation and complexation of gold(I)-bisulfite AuHSO3 in nanodroplet environments were also examined, with a particular focus on surface and interior solvation. Classical TIP4P/2005 molecular dynamics simulations reveal extreme densities in the interior of (H2O)100 and (H2O)1000 nanodroplets compared to droplet surface regions. At 25 °C, the interior region of (H2O)100 exhibits fluctuating densities at 1.016–1.079 g/cm3, with two maxima at 1.079 g/cm3 and 1.074 g/cm3, corresponding to pressures of ∼ 2.23 kbar and 2.07 kbar, respectively; Reduced densities are predicted for the larger (H2O)1000 systems, these being 1.013 g/cm3 (25 °C, 370 bar) and 0.968 g/cm3 (100 °C, 220 bar). The outer regions, on the other hand, featured densities intermediate between saturated liquid and vapor conditions, as part of a transition from liquid to vapor-like densities at the edge of the droplet. Born-Oppenheimer molecular dynamics simulations at 100 °C show that the gold(I)-bisulfite complex H2O-AuHSO3 maintains a near linear solvation structure (θO-Au-S = 172°-174°) in bulk aqueous fluids and at surface and interior sites of (H2O)100 nanodroplets. Distance constrained simulations reveal that, upon extension of the gold(I)-bisulfite Au-S contact (equilibrium rAu-S = 2.3 Å), HSO3− is displaced by a water molecule, forming a two-water solvation shell around Au+. Thermodynamic integration gives gold(I)-bisulfite dissociation energies (ΔG) of 17.65 ± 0.37 kcal/mol (bulk), 20.22 ± 0.38 kcal/mol (nanodroplet surface), and 18.31 ± 0.31 kcal/mol (nanodroplet interior). Our ab initio molecular dynamics results demonstrate that water nanodroplets are stable at hydrothermal conditions and would play an important role in the speciation and transport of gold in volcanic and hydrothermal vapors.
期刊介绍:
Geochimica et Cosmochimica Acta publishes research papers in a wide range of subjects in terrestrial geochemistry, meteoritics, and planetary geochemistry. The scope of the journal includes:
1). Physical chemistry of gases, aqueous solutions, glasses, and crystalline solids
2). Igneous and metamorphic petrology
3). Chemical processes in the atmosphere, hydrosphere, biosphere, and lithosphere of the Earth
4). Organic geochemistry
5). Isotope geochemistry
6). Meteoritics and meteorite impacts
7). Lunar science; and
8). Planetary geochemistry.