{"title":"Equilibrium indium isotope fractionation in chloride-rich aqueous solutions using first-principles calculations","authors":"Haochen Duan , Fang Huang","doi":"10.1016/j.gca.2025.01.026","DOIUrl":null,"url":null,"abstract":"<div><div>Aqueous indium (In) speciation and isotope fractionation factors are important to understand the origin and transport of indium during magmatic-hydrothermal and atmosphere-hydrosphere processes. Here, we investigate indium speciation in chloride-rich aqueous solutions and explore their reduced partition function ratios (10<sup>3</sup><em>lnβ</em>) using first-principles calculations. The simulations with initial configurations of InCl(H<sub>2</sub>O)<sub>5</sub><sup>2+</sup>, InCl<sub>2</sub>(H<sub>2</sub>O)<sub>4</sub><sup>+</sup>, InCl<sub>3</sub>(H<sub>2</sub>O)<sub>3</sub>, InCl<sub>4</sub>(H<sub>2</sub>O)<sub>2</sub><sup>−</sup> and InCl<sub>5</sub>(H<sub>2</sub>O)<sup>2−</sup> were performed at 400 and 600 K, respectively. The results show that InCl(H<sub>2</sub>O)<sub>5</sub><sup>2+</sup>, InCl<sub>2</sub>(H<sub>2</sub>O)<sub>4</sub><sup>+</sup>, InCl<sub>3</sub>(H<sub>2</sub>O)<sub>2.4</sub>, InCl<sub>4</sub><sup>−</sup> and InCl<sub>5</sub><sup>2−</sup> are the stable In<sup>3+</sup> species at 400 K, and their 10<sup>3</sup><em>lnβ</em> decreases from 1.00 ‰, 0.89 ‰, 0.83 ‰, 0.75 ‰ to 0.66 ‰. At 600 K, the stable In<sup>3+</sup> species are composed of InCl(H<sub>2</sub>O)<sub>5</sub><sup>2+</sup>, InCl<sub>2</sub>(H<sub>2</sub>O)<sub>3.7</sub><sup>+</sup>, InCl<sub>3</sub>(H<sub>2</sub>O)<sub>1.7</sub>, InCl<sub>4</sub><sup>−</sup> and InCl<sub>5</sub><sup>2−</sup> with their 10<sup>3</sup><em>lnβ</em> decreasing from 0.46 ‰, 0.42 ‰, 0.39 ‰, 0.35 ‰ to 0.31 ‰. These results indicate that 10<sup>3</sup><em>lnβ</em> is negatively correlated with the coordination number and bond length of chlorine ligands in aqueous In<sup>3+</sup> species. Meanwhile, water molecules are gradually removed from the first hydration shell gradually with increasing temperature, such as InCl<sub>2</sub>(H<sub>2</sub>O)<sub>4</sub><sup>+</sup> and InCl<sub>4</sub>(H<sub>2</sub>O)<sub>2</sub><sup>−</sup> to InCl<sub>2</sub>(H<sub>2</sub>O)<sub>3.7</sub><sup>+</sup> and InCl<sub>4</sub><sup>−</sup>, indicating that stable In<sup>3+</sup> species changes with temperature. Hence, estimating the 10<sup>3</sup><em>lnβ</em> of aqueous liquids at different temperatures should consider the potential structure transition of cation species. The calculations of equilibrium indium isotope fractionation factors provide important insights into the mechanism of isotope fractionation in aqueous liquids, and show the potential application of indium isotopes in the geological and supergene processes of indium.</div></div>","PeriodicalId":327,"journal":{"name":"Geochimica et Cosmochimica Acta","volume":"393 ","pages":"Pages 304-317"},"PeriodicalIF":4.5000,"publicationDate":"2025-03-15","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://www.sciencedirect.com/science/article/pii/S0016703725000377","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
Aqueous indium (In) speciation and isotope fractionation factors are important to understand the origin and transport of indium during magmatic-hydrothermal and atmosphere-hydrosphere processes. Here, we investigate indium speciation in chloride-rich aqueous solutions and explore their reduced partition function ratios (103lnβ) using first-principles calculations. The simulations with initial configurations of InCl(H2O)52+, InCl2(H2O)4+, InCl3(H2O)3, InCl4(H2O)2− and InCl5(H2O)2− were performed at 400 and 600 K, respectively. The results show that InCl(H2O)52+, InCl2(H2O)4+, InCl3(H2O)2.4, InCl4− and InCl52− are the stable In3+ species at 400 K, and their 103lnβ decreases from 1.00 ‰, 0.89 ‰, 0.83 ‰, 0.75 ‰ to 0.66 ‰. At 600 K, the stable In3+ species are composed of InCl(H2O)52+, InCl2(H2O)3.7+, InCl3(H2O)1.7, InCl4− and InCl52− with their 103lnβ decreasing from 0.46 ‰, 0.42 ‰, 0.39 ‰, 0.35 ‰ to 0.31 ‰. These results indicate that 103lnβ is negatively correlated with the coordination number and bond length of chlorine ligands in aqueous In3+ species. Meanwhile, water molecules are gradually removed from the first hydration shell gradually with increasing temperature, such as InCl2(H2O)4+ and InCl4(H2O)2− to InCl2(H2O)3.7+ and InCl4−, indicating that stable In3+ species changes with temperature. Hence, estimating the 103lnβ of aqueous liquids at different temperatures should consider the potential structure transition of cation species. The calculations of equilibrium indium isotope fractionation factors provide important insights into the mechanism of isotope fractionation in aqueous liquids, and show the potential application of indium isotopes in the geological and supergene processes of indium.
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.