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Probing atomic-scale processes at the ferrihydrite-water interface with reactive molecular dynamics
Ardalan Hayatifar1, Simon Gravelle2, Beatriz D Moreno3
1Department of Geological Sciences, University of Saskatchewan, Saskatoon, SK, S7N 5E2, Canada. ardalan.hayatifar@usask.ca.
Reactive molecular dynamics simulations reveal how ferrihydrite restructures at the mineral-water interface. This dynamic restructuring influences contaminant and nutrient mobility, impacting ecosystem health and refining surface complexation models.
Area of Science:
- Environmental Science
- Geochemistry
- Computational Chemistry
Background:
- Mineral-water interfaces govern nutrient and contaminant behavior in natural systems.
- Understanding these interfaces is crucial for ecosystem health and Earth's co-evolution.
- Ferrihydrite is a key metal (oxyhydr)oxide phase in soils and sediments.
Purpose of the Study:
- To investigate molecular-scale interfacial processes in ferrihydrite-water systems.
- To study surface complexation dynamics using reactive molecular dynamics simulations.
- To validate simulation methods by comparing with experimental surface complexation models.
Main Methods:
- Reactive molecular dynamics simulations were employed.
- Synchrotron X-ray spectroscopy and high-resolution X-ray diffraction were used for validation.
- Umbrella sampling was utilized to calculate free energy landscapes.
Main Results:
- Ferrihydrite restructures into a more disordered phase upon hydration and adsorption.
- Surface charge equilibration and interfacial water dynamics were observed.
- Simulated adsorption free energies and deprotonation values agreed well with experimental data.
Conclusions:
- Reactive molecular dynamics accurately captures mineral-water interface dynamics.
- This approach refines surface complexation models beyond static assumptions.
- Findings enhance understanding of contaminant and nutrient mobility at interfaces.
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