Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
6437851 | Geochimica et Cosmochimica Acta | 2015 | 13 Pages |
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]2âxaq (x = 3, 4, 5) complexes have been investigated using density functional theory (DFT) methods and molecular dynamics (MD) simulations. [CuCl3]â and [CuCl4]2â species can both be tracked, while the [CuCl5]3âaq 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]â species are less stable than its solvent separated ion pair (SSIP) conformers, in which one Clâ 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 Clâ is more likely in the second coordination shell of center Cu2+ in [CuCl3]â. Meanwhile, the characteristic peak around 385 nm resolved in UV-Vis spectra experiments, which was attributed to the [CuCl3]â complex, could also be resulted from some SSIP structures of the [CuCl3]â complex. In MD simulations, the complex [CuCl4]2âaq is found more stable than [CuCl3]âaq. The surrounding water molecules around [CuClx]2âxaq (x = 3, 4) enhance their stabilities in Clâ brines, especially for [CuCl4]2âaq. The hydration shell of [CuCl4]2âaq species is more intact than that of [CuCl3]2âaq, and the residence time of a water molecule in the second coordination sphere of Cu ion in the [CuCl4]2âaq complex is also obviously longer than that of [CuCl3]âaq. The [CuCl4]2âaq complex can even be recorded in the less concentrated (6.33 m) Clâ solution, while the [CuCl3]âaq complex is tracked only in the 16.32 m Clâ brine. Meanwhile, the possibilities of [CuCl3]âaq and [CuCl4]2âaq complexes found in 16.32 m Clâ solutions both decrease with increasing temperature, [CuCl3]âaq cannot be recorded during our simulations at 373 K and 423 K, and only few [CuCl4]2âaq at 423 K.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Hui-Ji Li, Hai-Bo Yi, Jia-Jia Xu,