THE THICKNESS OF SURFACE-TENSION-GRADIENT-DRIVEN SPREADING FILMS

被引:46
作者
CARLES, P [1 ]
CAZABAT, AM [1 ]
机构
[1] COLL FRANCE,PHYS MAT CONDENSEE LAB,11 PL MARCELIN BERTHELOT,F-75231 PARIS 05,FRANCE
关键词
D O I
10.1006/jcis.1993.1176
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
We present here a new interpretation of the origin of the thickness of surface-tension-gradient-driven spreading films. Besides the already known regime, where this thickness is controlled by the influence of gravity and is proportional to the surface tension gradient, we show the existence of another regime, where the curvature of the meniscus, out of which the film climbs, must be taken into account, and the thickness is proportional to the square of the surface tension gradient. This situation corresponds to low surface tension gradients, or equivalently to highly curved menisci. This theory is successfully used to explain the differences observed between two previously published papers (Ludviksson and Lightfoot, AIChE J. 17, 1166 (1971); Cazabat et al., Nature 346, 824 (1990)), and its predictions are checked by new experiments. © 1993 Academic Press, Inc.
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页码:196 / 201
页数:6
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