Półodwrotna Metoda w Hydrodynamice Płaskiej

The first part of the paper is devoted to generalization of the semi-inverse method of [1]. Some applications are given. Many boundary value problems can easily be solved for regions bounded by the curves plotted in Fig. 2 or 3 and the two radii on the real axis extending to infinity. The curves in...

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Bibliographic Details
Main Author: S.I. Gheorghitza
Format: Article
Language:English
Published: Institute of Fundamental Technological Research 1965-09-01
Series:Engineering Transactions
Online Access:https://et.ippt.pan.pl/index.php/et/article/view/2769
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Summary:The first part of the paper is devoted to generalization of the semi-inverse method of [1]. Some applications are given. Many boundary value problems can easily be solved for regions bounded by the curves plotted in Fig. 2 or 3 and the two radii on the real axis extending to infinity. The curves in Fig. 4 can represent boundaries for motion in channels or in porous media. Some boundary value problems for regions as shown in Fig. 5 by using the method of bipolar coordinates are dealt with in the closing part of the paper.
ISSN:0867-888X
2450-8071