Hydrothermal wave in a shallow liquid layer
The oscillatory thermocapillary convection and hydrothermal wave in a shallow liquid layer, where a temperature difference is applied between two parallel sidewalls, have been numerically investigated in a two-dimensional model. The oscillatory thermocapillary convection and hydrothermal wave appear...
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Veröffentlicht in: | Microgravity science and technology 2005-03, Vol.16 (1-4), p.253-258 |
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description | The oscillatory thermocapillary convection and hydrothermal wave in a shallow liquid layer, where a temperature difference is applied between two parallel sidewalls, have been numerically investigated in a two-dimensional model. The oscillatory thermocapillary convection and hydrothermal wave appear if the Marangoni number is larger than a critical value. The critical phase speed and critical wave number of the hydrothermal wave agree with the ones given analytically by Smith and Davis in the microgravity environment, and it travels in the direction opposed to the surface flow. Another wave traveled downstream in addition to the hydrothermal wave traveled upstream was observed in the case of earth gravity condition. |
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Another wave traveled downstream in addition to the hydrothermal wave traveled upstream was observed in the case of earth gravity condition.</description><subject>Convection</subject><subject>Earth gravitation</subject><subject>Heat transfer</subject><subject>Microgravity</subject><subject>Phase velocity</subject><subject>Studies</subject><subject>Surface flow</subject><subject>Thermocapillary convection</subject><subject>Two dimensional models</subject><issn>0938-0108</issn><issn>1875-0494</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2005</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><recordid>eNp10M1Kw0AUBeBBFIzVjU8QdKdE773zv9RirVBw032YJhOakjbtTGLJ2xup4MrV2XycA4exW4QnBNDPrzMgK6Q16owlaLTMQFhxzhKw3GSAYC7ZVYwbAEUoKGGP86EMbbf2Yeua9Oi-fFrvUpfGtWua9pg29aGvy7Rxgw_X7KJyTfQ3vzlhy9nbcjrPFp_vH9OXRVZwoi7jkhsrtZJVsZJKOkQHQltlHVkoPWniDg0SWqRKrzgvqXAVcaUra0TBJ-zuVLsP7aH3scs3bR9242JuUZHkwsoR3f-HSBsNWgGpUT2cVBHaGIOv8n2oty4MOUL-c1j-dxj_BvW7WVc</recordid><startdate>20050301</startdate><enddate>20050301</enddate><creator>Tang, Z. 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M.</au><au>Hu, W. R.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Hydrothermal wave in a shallow liquid layer</atitle><jtitle>Microgravity science and technology</jtitle><date>2005-03-01</date><risdate>2005</risdate><volume>16</volume><issue>1-4</issue><spage>253</spage><epage>258</epage><pages>253-258</pages><issn>0938-0108</issn><eissn>1875-0494</eissn><abstract>The oscillatory thermocapillary convection and hydrothermal wave in a shallow liquid layer, where a temperature difference is applied between two parallel sidewalls, have been numerically investigated in a two-dimensional model. The oscillatory thermocapillary convection and hydrothermal wave appear if the Marangoni number is larger than a critical value. The critical phase speed and critical wave number of the hydrothermal wave agree with the ones given analytically by Smith and Davis in the microgravity environment, and it travels in the direction opposed to the surface flow. 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subjects | Convection Earth gravitation Heat transfer Microgravity Phase velocity Studies Surface flow Thermocapillary convection Two dimensional models |
title | Hydrothermal wave in a shallow liquid layer |
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