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Updated: Mar 13, 2026

Probing the Structure and Dynamics of Interfacial Water with Scanning Tunneling Microscopy and Spectroscopy
Published on: May 27, 2018
Precise determination of water exchanges on a mineral surface
Andrew G Stack1, Jose M Borreguero2, Timothy R Prisk1
1Chemical Sciences Division, Oak Ridge National Laboratory, USA. stackag@ornl.gov.
Water dynamics on barite nanoparticles were studied using quasi-elastic neutron scattering (QENS) and molecular dynamics (MD). MD simulations validated by QENS reveal complex water exchange rates on mineral surfaces.
Area of Science:
- Surface chemistry
- Materials science
- Neutron scattering
Background:
- Solvent exchange on surfaces and ions is crucial for chemical reactions.
- Fast exchange rates are difficult to measure accurately.
- Understanding water dynamics on mineral surfaces is key.
Purpose of the Study:
- To investigate water diffusional motions on barite nanoparticles.
- To determine water exchange rates on different surface sites.
- To validate molecular dynamics simulations with experimental data.
Main Methods:
- Quasi-elastic neutron scattering (QENS) at varying temperatures and momentum transfer.
- Classical molecular dynamics (MD) simulations.
- Fitting QENS data using scattering functions from MD trajectories.
Main Results:
- MD simulations accurately reproduced experimental QENS data at ambient temperatures.
- Water exchange rates varied significantly across different barite surface sites.
- Calculated residence times for water on barite surfaces were comparable to aqueous ions.
Conclusions:
- Molecular dynamics is a reliable method for studying solvent exchange reactions when validated by QENS.
- Complex water dynamics exist on mineral surfaces.
- This study provides quantitative insights into water-surface interactions.
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