Generation of Thermogravitational Convection and Convective Diffusion in a Radiation-Heated Region

IF 0.6 4区 工程技术 Q4 MECHANICS Fluid Dynamics Pub Date : 2025-04-06 DOI:10.1134/S0015462824604650
B. V. Borisov, G. V. Kuznetsov, V. I. Maksimov, T. A. Nagornova, F. Yu. Salikhov
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Abstract

We present the results of the numerical investigation of the generation of thermogravitational convection and convective diffusion as a result of the radiation flux action on the internal boundaries of the walls of a closed rectangular region filled with the air. The conditions of the development and the characteristics of hydrodynamic and thermophysical processes occurring as a result of the heating of surface layers of the walls during the radiation heating are established. The relationship between the radiation heating strength and the convective heat and mass transfer is derived. The time-dependent fields of the temperature and the concentrations of anthropogenic gas admixture illustrate a considerably greater intensity of the heat transfer generated by the radiation heat flux compared with the conductive heat transfer and the convective diffusion compared with molecular diffusion.

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辐射加热区热重对流和对流扩散的产生
本文给出了辐射通量作用于充满空气的封闭矩形壁面内边界所产生的热重对流和对流扩散的数值研究结果。建立了辐射加热过程中由于墙体表层受热而产生的水动力和热物理过程的发展条件和特征。导出了辐射加热强度与对流传热传质之间的关系。温度场和人为气体混合物浓度随时间变化的场表明,辐射热流产生的换热强度远大于传导换热强度,对流扩散产生的换热强度远大于分子扩散。
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来源期刊
Fluid Dynamics
Fluid Dynamics MECHANICS-PHYSICS, FLUIDS & PLASMAS
CiteScore
1.30
自引率
22.20%
发文量
61
审稿时长
6-12 weeks
期刊介绍: Fluid Dynamics is an international peer reviewed journal that publishes theoretical, computational, and experimental research on aeromechanics, hydrodynamics, plasma dynamics, underground hydrodynamics, and biomechanics of continuous media. Special attention is given to new trends developing at the leading edge of science, such as theory and application of multi-phase flows, chemically reactive flows, liquid and gas flows in electromagnetic fields, new hydrodynamical methods of increasing oil output, new approaches to the description of turbulent flows, etc.
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