A mechanism of ion exchange by interface-coupled dissolution-precipitation in the presence of an aqueous fluid
- 1Institut für Mineralogie, University of Münster, Münster, Germany
- 2School of Molecular and Life Sciences, Curtin University, Perth, Australia
- 3School of Earth and Planetary Sciences, Curtin University, Perth, Australia
The equilibration of minerals in the presence of an aqueous fluid phase, with which it is out of equilibrium, has been described in terms of a number of potential mechanisms, specifically mainly either by solid state exchange of elements within the solid phase and the aqueous solution, or by interface-coupled dissolution-precipitation where equilibration is approached by the incremental dissolution of the parent solid and the coupled precipitation of a new product solid (Ruiz-Agudo et al., 2014). The conditions determining the equilibration mechanism can be defined by the specific chemical potential differences at the mineral interface, the kinetics of potential reactions, the solubility of the solid phase in the specific fluid and physical properties such as the mineral: fluid ratio as well as the surface area: fluid ratio, temperature and pressure. We focus on the mechanism of ion exchange in a range of minerals and in most cases ion-exchange in the presence of an aqueous solution occurs by interface-coupled dissolution-precipitation (Putnis and Putnis, 2022).
References
Putnis C.V. and Putnis A. 2022. A mechanism of ion exchange by interface-coupled dissolution-precipitation in the presence of an aqueous fluid. J. Crystal Growth, 600, 126840
Ruiz-Agudo E., Putnis C.V., Putnis A. 2014. Coupled dissolution and precipitation at mineral-fluid interfaces. Chemical Geology 383, 132-146.
How to cite: Putnis, C. V. and Putnis, A.: A mechanism of ion exchange by interface-coupled dissolution-precipitation in the presence of an aqueous fluid, EGU General Assembly 2023, Vienna, Austria, 24–28 Apr 2023, EGU23-3792, https://doi.org/10.5194/egusphere-egu23-3792, 2023.
