传热与热能专业大挑战

L. Dombrovsky
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引用次数: 1

摘要

众所周知,对热的产生和传播过程的研究,以及它转化为其他类型的能量,导致了基本物理定律的发现。首先,我们应该记住热辐射定律,这一定律的发现仅仅在一个多世纪前就从根本上改变了作为一门科学的物理学,并成为令人难以置信的技术进步的基础。理论物理学的革命极大地促进了传热的研究和各种应用,特别是在热工方面。教科书通常区分三种传热方式:传导、对流和热辐射。然而,解决实际问题的尝试表明,当不同的传热模式相互作用时,我们通常处理联合传热。在我看来,热辐射更接近基础科学,似乎比其他传热方式更具有全球性。这甚至不是我们星球上的生命之所以存在是因为来自太阳的热辐射,而这种辐射延伸1.5亿公里到达地球。与普遍的看法相反,热辐射在任何温度和任何距离都很重要,其光谱包括用于海洋表面遥感的微波范围。这就解释了为什么我们关注辐射和复合传热,以及涉及的各种问题是如此之多。所考虑的研究课题主要涉及半透明散射介质中辐射传输的各种问题。例如,这种介质是带有悬浮颗粒的气体或液体,以及各种分散的材料和带有微裂纹或气泡的固体。研究的自然对象包括地球的大气和海洋、雪和冰、粉末或灰尘和普通的沙子,甚至是具有光学异质活细胞的生物组织。在热能工程中,这些是含有烟尘和飞灰颗粒的燃烧产物,多孔陶瓷和热屏蔽材料,热化学反应堆中的颗粒和可能发生严重核反应堆事故的熔融液滴。一组远不完整的例子表明,研究辐射在散射介质中的传播具有重要的实际意义。因此,我们的编辑团队主要由从事分散系统辐射传热和组合传热领域的研究人员组成。这种介质中辐射传递的经典理论是基于积分微分方程,该方程是上世纪初由Orest Khvolson和Subrahmanyan Chandrasekhar在研究恒星光球中的辐射传递时独立导出的(Chandrasekhar 1960;罗森博格1977)。在Howell等人(2021)和Modest和Mazumder(2021)的教科书中可以找到辐射传热理论的现代系统描述,而在Dombrovsky和Baillis(2010)中讨论了分散系统中辐射传热和组合传热建模的工程方法。散射介质中的辐射传递方程没有考虑电磁辐射的波动性质,当辐射被粒子散射时,这种波动性质表现得最强烈
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Specialty Grand Challenge for Heat Transfer and Thermal Power
It is known that the study of the processes of heat generation and propagation, as well as its transformation into other types of energy, led to the discovery of fundamental physical laws. We should remember, first of all, the laws of thermal radiation, the discovery of which just over a century ago radically changed physics as a science and became the basis of incredible technical advances. The revolution in theoretical physics has greatly accelerated research in heat transfer and various applications, especially in thermal engineering. Textbooks usually distinguish three ways of heat transfer: conduction, convection, and thermal radiation. However, attempts to solve real problems show that we are usually dealing with combined heat transfer, when different modes of heat transfer interact with each other. In my opinion, thermal radiation is closer to fundamental science and appears to be a more global phenomenon than other modes of heat transfer. It is not even the fact that life on our planet exists because of thermal radiation from the Sun, and this radiation extends 150million kilometers to reach the Earth. Contrary to popular belief, thermal radiation turns out to be important at any temperature and at any distance, and its spectrum includes the microwave range used in remote sensing of the ocean surface. This explains why we focus on radiative and combined heat transfer, and the variety of problems involved is so great. The research topics under consideration are mainly related to various problems of radiation transfer in semitransparent scattering media. Such media are, for example, gases or liquids with suspended particles, as well as various dispersed materials and solids with microcracks or bubbles. Natural objects of study include the Earth’s atmosphere and ocean, snow and ice, powders or dust and ordinary sand, and even biological tissues with optically heterogeneous living cells. In thermal engineering these are combustion products containing soot and fly ash particles, porous ceramics and heat-shielding materials, particles in thermochemical reactors and melt droplets from a possible severe nuclear reactor accident. A far from complete set of given examples leaves no doubt about the practical importance of studying radiation propagation in scattering media. Therefore, our editorial team was formed mainly from researchers working in the field of radiative and combined heat transfer in disperse systems. The classical theory of radiative transfer in such media is based on the integrodifferential equation, which was independently derived early last century by Orest Khvolson and Subrahmanyan Chandrasekhar in connection with the study of radiative transfer in stellar photospheres (Chandrasekhar 1960; Rosenberg 1977). A modern systematic account of the theory of radiative heat transfer can be found in textbooks by Howell et al. (2021) and Modest and Mazumder (2021), and an engineering approach tomodeling radiative and combined heat transfer in disperse systems is discussed in Dombrovsky and Baillis (2010). The radiative transfer equation in a scattering medium does not take into account the wave nature of electromagnetic radiation, which appears most strongly when the radiation is scattered by particles Edited and reviewed by: Xianguo Li, University of Waterloo, Canada
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