ROUGHENING TRANSITION OBSERVED ON THE PRISM FACET OF ICE

被引：53

作者：

ELBAUM, M

机构：

[1] Department of Physics, FM-15, University of Washington, Seattle

来源：

PHYSICAL REVIEW LETTERS | 1991年 / 67卷 / 21期

关键词：

D O I：

10.1103/PhysRevLett.67.2982

中图分类号：

O4 [物理学];

学科分类号：

0702 ;

摘要：

Single crystals of ice are grown from vapor, and viewed by means of an interference microscope. The basal facet persists until melting, but the prism facet disappears above about -2-degrees-C, the surface taking a dome shape. With the temperature dropping from near 0-degrees-C, a facet reappears at -1.35-degrees-C. The measured curvature just above the transition is consistent with the prediction of a "universal curvature jump" by Jayaprakash, Saam, and Teitel. The surface curvature near the facet edge is also measured.

引用

页码：2982 / 2985

页数：4

共 23 条

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Andreev A. F., 1981, ZH EKSP TEOR FIZ, V53, P1063

[2]

[Anonymous], 1982, PISMA ZH EKSP TEOR F, V35, P362

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