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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| Format: | Article |
| Language: | English |
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Institute of Fundamental Technological Research
1965-09-01
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| Series: | Engineering Transactions |
| Online Access: | https://et.ippt.pan.pl/index.php/et/article/view/2769 |
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| _version_ | 1849320983493607424 |
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| author | S.I. Gheorghitza |
| author_facet | S.I. Gheorghitza |
| author_sort | S.I. Gheorghitza |
| collection | DOAJ |
| description | 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. |
| format | Article |
| id | doaj-art-2e36a0dc490c416b94a54ff46b9d0385 |
| institution | Kabale University |
| issn | 0867-888X 2450-8071 |
| language | English |
| publishDate | 1965-09-01 |
| publisher | Institute of Fundamental Technological Research |
| record_format | Article |
| series | Engineering Transactions |
| spelling | doaj-art-2e36a0dc490c416b94a54ff46b9d03852025-08-20T03:49:54ZengInstitute of Fundamental Technological ResearchEngineering Transactions0867-888X2450-80711965-09-01133Półodwrotna Metoda w Hydrodynamice PłaskiejS.I. Gheorghitza0Instytut Matematyczny Rumuńskiej Akademii NaukThe 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.https://et.ippt.pan.pl/index.php/et/article/view/2769 |
| spellingShingle | S.I. Gheorghitza Półodwrotna Metoda w Hydrodynamice Płaskiej Engineering Transactions |
| title | Półodwrotna Metoda w Hydrodynamice Płaskiej |
| title_full | Półodwrotna Metoda w Hydrodynamice Płaskiej |
| title_fullStr | Półodwrotna Metoda w Hydrodynamice Płaskiej |
| title_full_unstemmed | Półodwrotna Metoda w Hydrodynamice Płaskiej |
| title_short | Półodwrotna Metoda w Hydrodynamice Płaskiej |
| title_sort | polodwrotna metoda w hydrodynamice plaskiej |
| url | https://et.ippt.pan.pl/index.php/et/article/view/2769 |
| work_keys_str_mv | AT sigheorghitza połodwrotnametodawhydrodynamicepłaskiej |