SCANNING ELECTRON MICROSCOPY OF EVAPORATING ICE

被引：36

作者：

CROSS, JD

机构：

[1] Physics Department, University of Manchester, Institute of Science and Technology

来源：

SCIENCE | 1969年 / 164卷 / 3876期

关键词：

D O I：

10.1126/science.164.3876.174

中图分类号：

O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];

学科分类号：

07 ; 0710 ; 09 ;

摘要：

Direct observation of evaporating ice with a scanning electron microscope indicates that the surfaces of single-crystal and polycrystattine ice are markedly different. In specimens of single-crystal ice the crystal planes are revealed by evaporation, whereas polycrystalline ice develops a fibrous surface.

引用

页码：174 / &

共 8 条

[1] CROSS JD, UNPUBLISHED WORK
[2] CROSS JH, IN PRESS
[3] THE ELECTRIFICATION OF FROST DEPOSITS
LATHAM, J
[J]. QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, 1963, 89 (380) : 265 - 270
[4] LATHAM J, 1965, J ATMOS SCI, V22, P320, DOI 10.1175/1520-0469(1965)022<0320:EAWTEO>2.0.CO
[5] 2
[6] MUGURUMA J, 1968, INT S IC MUN
[7] MECHANISM FOR MULTIPLICATION OF ATMOSPHERIC ICE CRYSTALS - APPARENT CHARGE DISTRIBUTION ON LABORATORY CRYSTALS
ODENCRANTZ, FK
MCEWAN, WS
STAMAND, P
FINNEGAN, WG
[J]. SCIENCE, 1968, 160 (3834) : 1345 - +
[8] SIKSNA R, 1957, ARK FYS, V11, P495

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