Adhesion of ice, or ice-bonding phenomenon, at temperatures below 0° C was studied from the viewpoint of sintering. The growth rate of necks between ice spheres having radii R < 100 μ was measured in both saturated air and kerosene environments. The results showed that icebonding, or adhesion, takes place as a result of solid diffusion. Many photomicrographs of icebonds were taken by making use of thin-section technique.
CITATION STYLE
Kuroiwa, D. (1961). A Study of Ice Sintering. Tellus A: Dynamic Meteorology and Oceanography, 13(2), 252–259. https://doi.org/10.3402/tellusa.v13i2.9450
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