Reactive force fields for aqueous and interfacial magnesium carbonate formation.
Siavash Zare1, Mohammad Javad Abdolhosseini Qomi1
1Department of Civil and Environmental Engineering, University of California, Irvine, CA, USA. mjaq@uci.edu.
We developed new ReaxFF force fields for magnesium in water and at mineral interfaces. These models explain fast magnesite formation by showing how carbonate attaches to magnesium surfaces.
Area of Science:
- Computational chemistry
- Materials science
- Geochemistry
Background:
- Developing accurate force fields for magnesium (Mg) is crucial for understanding mineral-water interactions.
- Existing models often struggle to capture the complex behavior of Mg ions and their interactions with water and mineral surfaces.
Purpose of the Study:
- To create robust ReaxFF parameter sets for Mg/C/O/H systems in both aqueous and interfacial environments.
- To investigate the behavior of magnesium-containing minerals and their interfaces with water, particularly focusing on ion interactions and surface adsorption.
Main Methods:
- Developed two ReaxFF force fields: an aqueous one for Mg ions and an interfacial one for minerals.
- Parameterized and validated force fields against various Mg-bearing crystals and Mg2+-water binding energies.
- Applied the force fields to simulate forsterite-water and brucite-water interfaces, including bicarbonate interactions.
Main Results:
- Observed long-range proton transfer deprotonating bicarbonate to carbonate at mineral-water interfaces.
- Calculated an energy barrier (0.22 eV) for carbonate attachment to Mg surfaces, consistent with aqueous ion pairing.
- Found anisotropic and heterogeneous diffusion of hydroxide ions on mineral surfaces.
Conclusions:
- The new ReaxFF force fields accurately model Mg interactions in diverse chemical environments.
- The findings provide mechanistic insights into the experimentally observed rapid magnesite nucleation and growth under specific conditions.
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