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Lead and selenite adsorption at water-goethite interfaces from first principles
Kevin Leung1, Louise J Criscenti1
1Sandia National Laboratories, MS 1415, & 0754, Albuquerque, NM 87185 United States of America.
Density functional theory molecular dynamics simulations reveal how lead ions and lead-selenite pairs bind to goethite mineral surfaces. Findings agree with experimental data and aid future binding constant calculations.
Area of Science:
- Geochemistry
- Environmental Science
- Materials Science
Background:
- Complexation of toxic ions on mineral surfaces is crucial for geochemistry.
- Understanding lead (Pb(II)) and selenite (SeO3(2-)) interactions with iron oxides like goethite is vital for environmental remediation.
Purpose of the Study:
- To investigate the coordination and adsorption mechanisms of Pb(II) and Pb(II)/selenite ion pairs on goethite surfaces using computational methods.
- To compare simulation results with experimental data, specifically EXAFS measurements, for validation.
Main Methods:
- Applying periodic-boundary-conditions density functional theory (DFT) molecular dynamics simulations.
- Examining Pb(II) coordination to goethite (101) and (210) surfaces, including FeOH deprotonation effects.
- Analyzing Pb(II)/selenite contact ion pair interactions and stability.
Main Results:
- DFT simulations accurately predict Fe-Pb distances when Pb(II) coordinates to three FeO/FeOH groups, aligning with EXAFS data.
- Pb(II) coordination to fewer surface groups shows greater Pb-O distance fluctuations.
- Pb(II)/selenite ion pairs are metastable on goethite (210) surfaces with monodentate Se-O-Fe bonds.
Conclusions:
- DFT molecular dynamics provide a foundation for calculating Pb(II) and Pb(II)/selenite binding constants.
- The study clarifies adsorption sites and mechanisms for lead and selenite on goethite.
- Accurate simulation of ion-surface interactions is essential for predicting contaminant behavior in geological systems.
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