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- W2022346989 abstract "Observed frequently in a natural snowfall at temperatures lower than -20°C, the crossed-plate crystal is an assemblage of two to four thin basal plates, each plate extending along a CSL grain boundary with a relation of 70.3°/[1120]. A possible growth mechanism is proposed to account for the characteristics growth in the direction of the axis [1120]. If two or more grain boundary dislocation (GBD) structures are contained at a CSL grain boundary, growth layers will overflow alternately on the (1010) planes of each component crystal at the intersection of these planes. Thus, the distinctive structure of the CSL grain boundary, like the feature of a screw dislocation step, will induce the preferential growth in this direction." @default.
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- W2022346989 date "1978-12-01" @default.
- W2022346989 modified "2023-09-27" @default.
- W2022346989 title "On the growth mechanism of polycrystalline snow crystals with a specific grain boundary" @default.
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- W2022346989 doi "https://doi.org/10.1016/0022-0248(78)90415-3" @default.
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