Article ID Journal Published Year Pages File Type
6437851 Geochimica et Cosmochimica Acta 2015 13 Pages PDF
Abstract
Cu(II) complexation by chloride is relevant to the transport of copper in near-surface geologic environments, yet the existence of high-order Cu(II) chloro-complexes still remains in dispute. In this study, the structure characteristics and stabilities of [CuClx]2−xaq (x = 3, 4, 5) complexes have been investigated using density functional theory (DFT) methods and molecular dynamics (MD) simulations. [CuCl3]− and [CuCl4]2− species can both be tracked, while the [CuCl5]3−aq complex cannot be recorded during MD simulations of trace Cu2+ in chloride-rich brines. DFT calculations indicate that contact ion pair (CIP) conformers of [CuCl3]− species are less stable than its solvent separated ion pair (SSIP) conformers, in which one Cl− stays in the second coordination sphere of the centered Cu2+. MD simulations also reveal that the SSIP conformer is apt to appear in the aqueous solution than its CIP conformer. It seems that the third Cl− is more likely in the second coordination shell of center Cu2+ in [CuCl3]−. Meanwhile, the characteristic peak around 385 nm resolved in UV-Vis spectra experiments, which was attributed to the [CuCl3]− complex, could also be resulted from some SSIP structures of the [CuCl3]− complex. In MD simulations, the complex [CuCl4]2−aq is found more stable than [CuCl3]−aq. The surrounding water molecules around [CuClx]2−xaq (x = 3, 4) enhance their stabilities in Cl− brines, especially for [CuCl4]2−aq. The hydration shell of [CuCl4]2−aq species is more intact than that of [CuCl3]2−aq, and the residence time of a water molecule in the second coordination sphere of Cu ion in the [CuCl4]2−aq complex is also obviously longer than that of [CuCl3]−aq. The [CuCl4]2−aq complex can even be recorded in the less concentrated (6.33 m) Cl− solution, while the [CuCl3]−aq complex is tracked only in the 16.32 m Cl− brine. Meanwhile, the possibilities of [CuCl3]−aq and [CuCl4]2−aq complexes found in 16.32 m Cl− solutions both decrease with increasing temperature, [CuCl3]−aq cannot be recorded during our simulations at 373 K and 423 K, and only few [CuCl4]2−aq at 423 K.
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Geochemistry and Petrology
Authors
, , ,