Abstract
AbstractOptical measurements have been made on the water lenses which form under pressure at grain boundaries in polycrystalline ice. Monochromatic light from a point source is focused by the lenses but, because the lenses are microscopic in size, the image is blurred by diffraction. The diffraction pattern observed under a microscope has been compared with the computed diffraction pattern to deduce the angle 2θ at the rim of each lens. This is the dihedral angle for water at a grain boundary in ice, and gives the ratio of the grain-boundary energy to that of an ice-water interface. The most sensitive measurements are those made on the rings of the virtual diffraction pattern formed on the object side of the lens. They give θ = 12.5 ± 0.5° for the grain boundary under observation, which is 26% lower than the previous value for θ found by ignoring diffraction.
References
6
Referenced
20
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Dates
Type | When |
---|---|
Created | 7 years, 11 months ago (Sept. 20, 2017, 6:19 a.m.) |
Deposited | 2 years, 4 months ago (April 3, 2023, 2:35 a.m.) |
Indexed | 1 month, 4 weeks ago (July 2, 2025, 3:30 p.m.) |
Issued | 34 years, 8 months ago (Jan. 1, 1991) |
Published | 34 years, 8 months ago (Jan. 1, 1991) |
Published Online | 8 years, 7 months ago (Jan. 20, 2017) |
Published Print | 34 years, 8 months ago (Jan. 1, 1991) |
@article{Walford_1991, title={Measuring the dihedral angle of water at a grain boundary in ice by an optical diffraction method}, volume={37}, ISSN={1727-5652}, url={http://dx.doi.org/10.3189/s0022143000042854}, DOI={10.3189/s0022143000042854}, number={125}, journal={Journal of Glaciology}, publisher={International Glaciological Society}, author={Walford, M.E.R. and Nye, J.F.}, year={1991}, pages={107–112} }