Crossref journal-article
AIP Publishing
The Journal of Chemical Physics (317)
Abstract

The thermal contraction of ice single crystals between 0 and −50 °C has been measured by the use of silicon strain gauges frozen on the crystal basal surface. The experimental results cannot be explained without assuming the existence of a Newtonian viscous layer at the ice-strain-gauge interface; this layer has a thickness which changes in temperature as predicted by Fletcher, and a viscosity intermediate between that of ice and that of supercooled water. The activation energy of the viscosity, (0.36±0.04) eV, seems to indicate that it is controlled by a vacancy mechanism in which only the vacancy migration is effective.

Bibliography

Mantovani, S., Valeri, S., Loria, A., & del Pennino, U. (1980). Viscosity of the ice surface layer. The Journal of Chemical Physics, 72(2), 1077–1083.

Authors 4
  1. S. Mantovani (first)
  2. S. Valeri (additional)
  3. A. Loria (additional)
  4. U. del Pennino (additional)
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Dates
Type When
Created 22 years, 5 months ago (Feb. 28, 2003, 3 p.m.)
Deposited 1 year, 6 months ago (Feb. 9, 2024, 3:42 p.m.)
Indexed 1 year, 6 months ago (Feb. 9, 2024, 7:02 p.m.)
Issued 45 years, 7 months ago (Jan. 15, 1980)
Published 45 years, 7 months ago (Jan. 15, 1980)
Published Print 45 years, 7 months ago (Jan. 15, 1980)
Funders 0

None

@article{Mantovani_1980, title={Viscosity of the ice surface layer}, volume={72}, ISSN={1089-7690}, url={http://dx.doi.org/10.1063/1.439248}, DOI={10.1063/1.439248}, number={2}, journal={The Journal of Chemical Physics}, publisher={AIP Publishing}, author={Mantovani, S. and Valeri, S. and Loria, A. and del Pennino, U.}, year={1980}, month=jan, pages={1077–1083} }