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Probing the Structure and Dynamics of Interfacial Water with Scanning Tunneling Microscopy and Spectroscopy
Published on: May 27, 2018
A study of the ice-water interface using the TIP4P/2005 water model
Jorge Benet1, Luis G MacDowell, Eduardo Sanz
1Departamento de Química Física, Facultad de Ciencias Químicas, Universidad Complutense de Madrid, 28040 Madrid, Spain. esa01@quim.ucm.es.
This study quantifies the ice-water interfacial free energy using molecular simulations, finding an average of 27 mN m⁻¹, consistent with prior research. The interface thickness is estimated at 4-5 molecular diameters.
Area of Science:
- Physical Chemistry
- Materials Science
- Computational Physics
Background:
- The ice-water interface is crucial for diverse natural phenomena and technological applications.
- Accurate quantification of interfacial properties, such as free energy, is essential for understanding phase transitions.
- Previous estimations of ice-water interfacial free energy have varied, necessitating further investigation.
Purpose of the Study:
- To determine the orientationally averaged interfacial free energy of ice in equilibrium with liquid water.
- To calculate the interfacial free energy for specific crystallographic planes of ice (basal, primary prismatic, secondary prismatic).
- To characterize the structural properties, including thickness and phase coexistence, of the ice-water interface.
Main Methods:
- Molecular simulations employing the TIP4P/2005 water model.
- Analysis of capillary fluctuation spectra to measure interfacial free energy, following Hoyt et al.'s methodology.
- Estimation of free energies for distinct crystallographic planes and characterization of interface structure.
Main Results:
- An orientationally averaged interfacial free energy of 27(2) mN m⁻¹ was obtained.
- Specific plane free energies were determined: 27(2) mN m⁻¹ (basal), 28(2) mN m⁻¹ (primary prismatic), and 28(2) mN m⁻¹ (secondary prismatic).
- The ice-water interface was found to be approximately 4-5 molecular diameters thick, with the basal plane exhibiting alternating cubic and hexagonal ice regions.
Conclusions:
- The calculated interfacial free energy aligns well with recent simulation-based estimates.
- The study provides detailed interfacial free energy values for different ice planes.
- Structural analysis reveals the interface's thickness and complex coexistence of ice phases at the basal plane.
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