PLANE STOKES-FLOW DRIVEN BY CAPILLARITY ON A FREE-SURFACE .2. FURTHER DEVELOPMENTS

被引:44
作者
HOPPER, RW
机构
[1] Chemistry and Materials Science Department, Lawrence Livermore National Laboratory, Livermore, CA
关键词
D O I
10.1017/S0022112091000824
中图分类号
O3 [力学];
学科分类号
08 ; 0801 ;
摘要
For the free creeping viscous incompressible plane flow of a finite region, bounded by a simple smooth closed curve and driven solely by surface tension, analyzed previously, the shape evolution was described in terms of a time-dependent mapping function z = OMEGA(zeta, t) of the unit circle, conformal on \zeta\ less-than-or-equal-to 1. An equation giving the time evolution of the map, typically in parametric form, was derived. In this article, the flow of the infinite region exterior to a hypotrochoid is given. This includes the elliptic hole, which shrinks at a constant rate with a constant aspect ratio. The theory is extended to a class of semi-infinite regions, mapped from Im zeta less-than-or-equal-to 0, and used to solve the flow in a half-space bounded by a certain groove. The depth of the groove ultimately decays inversely with time.
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页码:355 / 364
页数:10
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