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Uranyl adsorption at the muscovite (mica)/water interface studied by second harmonic generation
Sarah A Saslow Gomez1, David S Jordan, Julianne M Troiano
1Department of Chemistry, Northwestern University, 2145 Sheridan Road, Evanston, Illinois 60208, USA.
Uranyl ions strongly adsorb to muscovite (mica) surfaces, influencing contaminant transport models. This study quantifies uranyl binding constants and surface charge density at the mica-water interface.
Area of Science:
- Environmental Science
- Geochemistry
- Surface Chemistry
Background:
- Understanding uranyl adsorption at mineral-water interfaces is crucial for predicting contaminant transport.
- Muscovite (mica) is a common environmental mineral, making its interaction with uranyl ions significant.
- Previous studies have lacked precise measurements of uranyl adsorption parameters at the muscovite interface.
Purpose of the Study:
- To quantify uranyl adsorption at the muscovite/water interface.
- To determine uranyl binding constants and surface charge density.
- To provide benchmark data for improving contaminant transport models.
Main Methods:
- Second harmonic generation (SHG) spectroscopy was employed to study uranyl adsorption.
- Nonresonant χ(3) and resonantly enhanced SHG experiments were used.
- The Gouy-Chapman model was applied to determine surface charge density.
Main Results:
- The initial surface charge density of muscovite was determined to be -0.022(1) C/m(2) at pH 6 with dissolved carbonate.
- A uranyl binding constant of 3(1) × 10(7) M(-1) was measured, corresponding to a Gibbs free energy of -52.6(8) kJ/mol.
- Maximum surface charge density at monolayer coverage was 0.028(3) C/m(2), indicating strong interactions.
Conclusions:
- Uranyl ions exhibit favorable adsorption to the muscovite interface via ion-dipole or hydrogen bonding.
- A 1:1 uranyl ion to surface site ratio suggests binding of monovalent cations and neutral uranyl species.
- The findings provide essential data for refining environmental contaminant transport models.
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