| Literature DB >> 17799336 |
Abstract
Direct observation of evaporating ice with a scanning electron microscope indicates that the surfaces of single-crystal and polycrystalline ice are markedly different. In specimens of single-crystal ice the crystal planes are revealed by evaporation, whereas polycrystalline ice develops a fibrous surface.Year: 1969 PMID： 17799336 DOI： 10.1126/science.164.3876.174
Source DB: PubMed Journal: Science ISSN： 0036-8075 Impact factor: 47.728