Ice revisited: No proton tunneling observed in a quasielastic neutron scattering experiment
Abstract
A large broadening ($${\sim}0.4\mathrm{meV}$$) of quasielastic neutron scattering (QENS) signal in $${\mathrm{H}}_{2}\mathrm{O}$$ ice $${I}_{h}$$ at $$T=5\mathrm{K}$$ was observed by Bove et al. [Phys. Rev. Lett. 103, 165901 (2009)] and explained by a model of concerted proton tunneling. This result was rather unexpected, as prior studies never showed significant mobility in water at low temperatures and ambient pressure. There were a few attempts of theoretical understanding of the effect. Recent path-integral simulations as well as quantum lattice-gauge theory supported the possibility of the collective tunneling of protons in ice $${I}_{h}$$, however other studies stated that concerted tunneling in ice $${I}_{h}$$ should have very low frequency. In this paper, we report on QENS measurements of $${\mathrm{H}}_{2}\mathrm{O}$$ ice $${I}_{h}$$ at 1.8 and 5 K by using neutron scattering spectrometers with the energy resolution similar to and four times better than the energy resolution in the original experiment of Bove and co-workers. We did not observe any QENS broadening, and the measured spectra for the ice $${I}_{h}$$ and the reference vanadium sample were almost identical. Therefore, we conclude that there is no proton tunneling in ice $${I}_{h}$$ at temperatures down to 1.8 K measurable on an energy scale of 3.5 $${\mu}\mathrm{eV}$$ and above. Finally, the literature data on low-temperature heat capacity of ice $${I}_{h}$$ support this conclusion.
- Authors:
-
- Oak Ridge National Lab. (ORNL), Oak Ridge, TN (United States). Neutron Scattering Division
- Oak Ridge National Lab. (ORNL), Oak Ridge, TN (United States). Neutron Technologies Division
- Publication Date:
- Research Org.:
- Oak Ridge National Lab. (ORNL), Oak Ridge, TN (United States)
- Sponsoring Org.:
- USDOE Office of Science (SC), Basic Energy Sciences (BES)
- OSTI Identifier:
- 1463998
- Alternate Identifier(s):
- OSTI ID: 1463212
- Grant/Contract Number:
- AC05-00OR22725
- Resource Type:
- Accepted Manuscript
- Journal Name:
- Physical Review B
- Additional Journal Information:
- Journal Volume: 98; Journal Issue: 6; Journal ID: ISSN 2469-9950
- Publisher:
- American Physical Society (APS)
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 72 PHYSICS OF ELEMENTARY PARTICLES AND FIELDS; quasi-elastic neutron scattering
Citation Formats
Kolesnikov, Alexander I., Ehlers, Georg, Mamontov, Eugene, and Podlesnyak, Andrey. Ice Ih revisited: No proton tunneling observed in a quasielastic neutron scattering experiment. United States: N. p., 2018.
Web. doi:10.1103/PhysRevB.98.064301.
Kolesnikov, Alexander I., Ehlers, Georg, Mamontov, Eugene, & Podlesnyak, Andrey. Ice Ih revisited: No proton tunneling observed in a quasielastic neutron scattering experiment. United States. https://doi.org/10.1103/PhysRevB.98.064301
Kolesnikov, Alexander I., Ehlers, Georg, Mamontov, Eugene, and Podlesnyak, Andrey. Tue .
"Ice Ih revisited: No proton tunneling observed in a quasielastic neutron scattering experiment". United States. https://doi.org/10.1103/PhysRevB.98.064301. https://www.osti.gov/servlets/purl/1463998.
@article{osti_1463998,
title = {Ice Ih revisited: No proton tunneling observed in a quasielastic neutron scattering experiment},
author = {Kolesnikov, Alexander I. and Ehlers, Georg and Mamontov, Eugene and Podlesnyak, Andrey},
abstractNote = {A large broadening (${\sim}0.4\mathrm{meV}$) of quasielastic neutron scattering (QENS) signal in ${\mathrm{H}}_{2}\mathrm{O}$ ice ${I}_{h}$ at $T=5\mathrm{K}$ was observed by Bove et al. [Phys. Rev. Lett. 103, 165901 (2009)] and explained by a model of concerted proton tunneling. This result was rather unexpected, as prior studies never showed significant mobility in water at low temperatures and ambient pressure. There were a few attempts of theoretical understanding of the effect. Recent path-integral simulations as well as quantum lattice-gauge theory supported the possibility of the collective tunneling of protons in ice ${I}_{h}$, however other studies stated that concerted tunneling in ice ${I}_{h}$ should have very low frequency. In this paper, we report on QENS measurements of ${\mathrm{H}}_{2}\mathrm{O}$ ice ${I}_{h}$ at 1.8 and 5 K by using neutron scattering spectrometers with the energy resolution similar to and four times better than the energy resolution in the original experiment of Bove and co-workers. We did not observe any QENS broadening, and the measured spectra for the ice ${I}_{h}$ and the reference vanadium sample were almost identical. Therefore, we conclude that there is no proton tunneling in ice ${I}_{h}$ at temperatures down to 1.8 K measurable on an energy scale of 3.5 ${\mu}\mathrm{eV}$ and above. Finally, the literature data on low-temperature heat capacity of ice ${I}_{h}$ support this conclusion.},
doi = {10.1103/PhysRevB.98.064301},
journal = {Physical Review B},
number = 6,
volume = 98,
place = {United States},
year = {Tue Aug 07 00:00:00 EDT 2018},
month = {Tue Aug 07 00:00:00 EDT 2018}
}
Web of Science
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