Onset of convection in a fluid saturated porous layer overlying a solid layer which is heated by constant flux

C. Y. Wang

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Onset of convection in a fluid saturated porous layer overlying a solid layer which is heated by constant flux

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摘要

The thermoconvective stability of a porous layer overlying a solid layer is important in seafloor hydrothermal systems and thermal insulation problems. The case for constant flux bottom heating is considered. The critical Rayleigh number for theporous layer is found to increase with the thickness of the solid layer, a result opposite to constant temperature heating.

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《Journal of heat transfer: Transactions of the ASME》 |1999年第4期|1094-1097|共4页
作者
C. Y. Wang;
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收录信息美国《科学引文索引》(SCI);美国《工程索引》(EI);
原文格式 PDF
正文语种英语
中图分类热力工程、热机;
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Onset of convection in a fluid saturated porous layer overlying a solid layer which is heated by constant flux

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