Three-Dimensional Morphology of Natural Snow Crystals

被引:12
作者
Shimada, Wataru [1 ]
Ohtake, Kazuki [2 ]
机构
[1] Toyama Univ, Fac Sci, 3190 Gofuku, Toyama 9308555, Japan
[2] Toyama Univ, Grad Sch Sci & Engn Educ, 3190 Gofuku, Toyama 9308555, Japan
关键词
ICE CRYSTALS; GROWTH; MODEL;
D O I
10.1021/acs.cgd.6b01263
中图分类号
O6 [化学];
学科分类号
0703 ;
摘要
We reveal that the external form of a snow crystal consists of the combination,of one basal plane and, an intricate 3D rounded surface. Snow crystals have various morphologies including needles, plates, sectors, and dendrites. Many of these snow-crystal shapes are planar, and thus are often treated as a two-dimensional or a faceted crystal consisting of. only basal and prism planes despite their complex three-dimensional (3D) features. In, this study, we directly measure the 3D morphology of natural snow crystals using a, Michelson interferometer combined with a reflecting microscope. The 3D morphologies of both stellar With sectors and dendrite are analyzed from the;distribution Of interference fringes, observed on then surfaces. Additionally, dendrite crystal has a thickness of only several micrometers at the middle of the branch and no prism. face. On the non-basal surfaces, there are ridges and sub-ridges, similar to those in Mountain topography.
引用
收藏
页码:5603 / 5605
页数:3
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