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Updated: Apr 5, 2026

A Microfluidic Approach for the Study of Ice and Clathrate Hydrate Crystallization
Published on: August 18, 2022
Evolution of Hydrogen Dynamics in Amorphous Ice with Density
A Parmentier1, J J Shephard2,3, G Romanelli1
1†Dipartimento di Fisica and NAST Centre, Università degli Studi di Roma Tor Vergata, Via della Ricerca Scientifica 1, 00133 Roma, Italy.
Deep inelastic neutron scattering (DINS) and inelastic neutron scattering (INS) reveal how hydrogen atoms move in amorphous ices. Higher density weakens hydrogen bonds and increases hydrogen kinetic energy, with DINS offering superior insights into O-H stretching dynamics.
Area of Science:
- Condensed matter physics
- Materials science
- Physical chemistry
Background:
- Amorphous ices are technologically relevant materials.
- Understanding single-particle dynamics is crucial for characterizing material properties.
- Hydrogen bonding significantly influences the behavior of amorphous ices.
Purpose of the Study:
- To investigate the single-particle dynamics of hydrogen atoms in amorphous ices.
- To determine the effect of density on hydrogen kinetic energy and bonding.
- To compare the capabilities of DINS, INS, and Raman spectroscopy for probing O-H stretching modes.
Main Methods:
- Deep inelastic neutron scattering (DINS)
- Inelastic neutron scattering (INS)
- Analysis of hydrogen kinetic energies and vibrational potentials
Main Results:
- Mean kinetic energies of hydrogen nuclei increase with density.
- Increasing density weakens hydrogen bonds and leads to more harmonic potentials.
- DINS reveals more significant changes in O-H stretching kinetic energy than INS or Raman spectroscopy.
- Anharmonicity constants for O-H stretching modes were determined.
Conclusions:
- DINS is a powerful technique for accurate ground-state kinetic energy determination beyond the harmonic approximation.
- The study provides benchmark kinetic energy data for path-integral Monte Carlo simulations.
- Density plays a critical role in modifying hydrogen bonding and dynamics in amorphous ices.
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