Strength of Bonds between Ice Grains after Short Contact Times
Open Access
- 1 January 1982
- journal article
- Published by International Glaciological Society in Journal of Glaciology
- Vol. 28 (100) , 457-473
- https://doi.org/10.3189/s0022143000005050
Abstract
The tensile force required to break bonds between ice grains after short contact times (1–500 s) is measured as a function of temperature and contact pressure. The results indicate a sharp increase of the tensile load capacity of bonds alter short contact times near the melting point and a maximum rate of increase of the load capacity at −5 °C. The initial state or sintering is modelled, assuming viscous surface flow and plastic deformation as the main mechanisms.Keywords
This publication has 17 references indexed in Scilit:
- A model of the “liquid-like” layer between ice and a substrate with applications to wire regelation and particle migrationJournal of Colloid and Interface Science, 1979
- The surface of ice near 0°C studied by 100 keV proton channelingPhysics Letters A, 1977
- The mobile water phase on ice surfacesSurface Science, 1974
- Surface structure of water and icePhilosophical Magazine, 1968
- The sintering and adhesion of IcePhilosophical Magazine, 1964
- Surface structure of water and icePhilosophical Magazine, 1962
- A Study of Ice SinteringTellus, 1961
- A Study of Ice SinteringTellus A: Dynamic Meteorology and Oceanography, 1961
- Regelation, Surface Diffusion, and Ice SinteringJournal of Applied Physics, 1960
- Surface structure of water and some of its physical and chemical manifestationsJournal of Colloid Science, 1951