КОЛИВАННЯ ПРИ ОБТІКАННІ ПОТОКОМ ПОВІТРЯ ЗАГЛИБИН НА ГЛАДКІЙ ПОВЕРХНІ

The purpose of the work is to evaluate the intensification of heat transfer using various types of recesses when air flows around heat transfer surfaces with possible minimization of pressure losses. The creation of compact devices for space and the armed forces requires solving similar problems. On...

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Datum:2024
Hauptverfasser: Khalatov, A. A., Kovalenko, G. V.
Format: Artikel
Sprache:Ukrainian
Veröffentlicht: Institute of Engineering Thermophysics of NAS of Ukraine 2024
Online Zugang:https://ihe.nas.gov.ua/index.php/journal/article/view/589
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Назва журналу:Thermophysics and Thermal Power Engineering

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Thermophysics and Thermal Power Engineering
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spelling oai:ojs2.ihenasgovua.s43.yourdomain.com.ua:article-5892025-02-22T18:04:17Z OSCILLATIONS DURING AIR FLOW NEAR DENTS ON A FLAT SURFACE КОЛИВАННЯ ПРИ ОБТІКАННІ ПОТОКОМ ПОВІТРЯ ЗАГЛИБИН НА ГЛАДКІЙ ПОВЕРХНІ Khalatov, A. A. Kovalenko, G. V. The purpose of the work is to evaluate the intensification of heat transfer using various types of recesses when air flows around heat transfer surfaces with possible minimization of pressure losses. The creation of compact devices for space and the armed forces requires solving similar problems. One of the proposed methods is the use of recesses on streamlined heat transfer surfaces. This paper presents the results of experimental studies of flow around surfaces with depressions. Two types of recesses were considered: cylindrical and hemispherical segments. The influence of flow velocity on the formation of vortex structures when flowing around surfaces with depressions was studied. It was shown that at low speeds the flow has a diffuser and confuser character. As the speed increases at the inlet edge of the notch, the flow was been interrupted and a horseshoe-shaped vortex was formed in the notch. In this case, the boundary layer above the depression periodically collapses, and its lower end jumps from one half of the depression to the other, breaks off and turns into a Karman trace. With a further increase in speed, one of the ends of the horseshoe-shaped vortex rises above the depression, turning into a columnar one. The nature of the flow over the depression was been analyzed. It was been noted that part of the shear layer is deflected towards the excavation and hits its rear (aft) wall. The location of the impact is the source of sound vibrations. It was shown, that when the frequency of any harmonic of these oscillations coincides with the frequency of shear layers vortex structures, these two phenomena begin to reinforce each other. Flow fluctuations near and inside the excavation could be divided into classes. Hydrodynamic vibrations arising due to the instability of the shear layer. Oscillations resulting from the interaction of standing pressure waves in the depression and acoustic waves emitted from places where the surface profile changes sharply. Oscillations, when a sharp change in the shape of the surface causes the formation of vortices. It was shown, that the sound pressure caused by the presence of depressions decreases with increasing boundary layer thickness. Визначені залежності коефіцієнтів гідравлічного опору від чисел Рейнольдса при обтіканні повітрям напівсферичних і циліндричних заглибин декількох розмірів Institute of Engineering Thermophysics of NAS of Ukraine 2024-09-27 Article Article application/pdf https://ihe.nas.gov.ua/index.php/journal/article/view/589 10.31472/ttpe.3.2024.1 Thermophysics and Thermal Power Engineering; Vol 46 No 3 (2024): Thermophysics and Thermal Power Engineering; 5-11 Теплофизика и Теплоэнергетика; Vol 46 No 3 (2024): Thermophysics and Thermal Power Engineering; 5-11 Теплофізика та Теплоенергетика; Vol 46 No 3 (2024): Thermophysics and Thermal Power Engineering; 5-11 2663-7235 uk https://ihe.nas.gov.ua/index.php/journal/article/view/589/511 https://creativecommons.org/licenses/by/4.0/deed.ru
institution Thermophysics and Thermal Power Engineering
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datestamp_date 2025-02-22T18:04:17Z
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language Ukrainian
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author Khalatov, A. A.
Kovalenko, G. V.
spellingShingle Khalatov, A. A.
Kovalenko, G. V.
КОЛИВАННЯ ПРИ ОБТІКАННІ ПОТОКОМ ПОВІТРЯ ЗАГЛИБИН НА ГЛАДКІЙ ПОВЕРХНІ
author_facet Khalatov, A. A.
Kovalenko, G. V.
author_sort Khalatov, A. A.
title КОЛИВАННЯ ПРИ ОБТІКАННІ ПОТОКОМ ПОВІТРЯ ЗАГЛИБИН НА ГЛАДКІЙ ПОВЕРХНІ
title_short КОЛИВАННЯ ПРИ ОБТІКАННІ ПОТОКОМ ПОВІТРЯ ЗАГЛИБИН НА ГЛАДКІЙ ПОВЕРХНІ
title_full КОЛИВАННЯ ПРИ ОБТІКАННІ ПОТОКОМ ПОВІТРЯ ЗАГЛИБИН НА ГЛАДКІЙ ПОВЕРХНІ
title_fullStr КОЛИВАННЯ ПРИ ОБТІКАННІ ПОТОКОМ ПОВІТРЯ ЗАГЛИБИН НА ГЛАДКІЙ ПОВЕРХНІ
title_full_unstemmed КОЛИВАННЯ ПРИ ОБТІКАННІ ПОТОКОМ ПОВІТРЯ ЗАГЛИБИН НА ГЛАДКІЙ ПОВЕРХНІ
title_sort коливання при обтіканні потоком повітря заглибин на гладкій поверхні
title_alt OSCILLATIONS DURING AIR FLOW NEAR DENTS ON A FLAT SURFACE
description The purpose of the work is to evaluate the intensification of heat transfer using various types of recesses when air flows around heat transfer surfaces with possible minimization of pressure losses. The creation of compact devices for space and the armed forces requires solving similar problems. One of the proposed methods is the use of recesses on streamlined heat transfer surfaces. This paper presents the results of experimental studies of flow around surfaces with depressions. Two types of recesses were considered: cylindrical and hemispherical segments. The influence of flow velocity on the formation of vortex structures when flowing around surfaces with depressions was studied. It was shown that at low speeds the flow has a diffuser and confuser character. As the speed increases at the inlet edge of the notch, the flow was been interrupted and a horseshoe-shaped vortex was formed in the notch. In this case, the boundary layer above the depression periodically collapses, and its lower end jumps from one half of the depression to the other, breaks off and turns into a Karman trace. With a further increase in speed, one of the ends of the horseshoe-shaped vortex rises above the depression, turning into a columnar one. The nature of the flow over the depression was been analyzed. It was been noted that part of the shear layer is deflected towards the excavation and hits its rear (aft) wall. The location of the impact is the source of sound vibrations. It was shown, that when the frequency of any harmonic of these oscillations coincides with the frequency of shear layers vortex structures, these two phenomena begin to reinforce each other. Flow fluctuations near and inside the excavation could be divided into classes. Hydrodynamic vibrations arising due to the instability of the shear layer. Oscillations resulting from the interaction of standing pressure waves in the depression and acoustic waves emitted from places where the surface profile changes sharply. Oscillations, when a sharp change in the shape of the surface causes the formation of vortices. It was shown, that the sound pressure caused by the presence of depressions decreases with increasing boundary layer thickness.
publisher Institute of Engineering Thermophysics of NAS of Ukraine
publishDate 2024
url https://ihe.nas.gov.ua/index.php/journal/article/view/589
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AT kovalenkogv kolivannâpriobtíkannípotokompovítrâzaglibinnagladkíjpoverhní
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