Generalization of the Fourier problem of temperature waves in half-space

Anatoly M. Afanasyev, Y. Bakhracheva
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Abstract

The problem of asymptotic fluctuations of temperature and moisture content in a half-space whose boundary is blown by an air flow with a temperature varying according to the harmonic law is solved by the method of complex amplitudes. The material filling the half-space consists of a solid base (capillary-porous body) and water. The well-known Fourier solution for temperature fluctuations in half-space in the absence of moisture and under the boundary conditions of heat exchange ofthefirst kind is generalized to the case of a wet material under the boundary conditions of Newton for temperature and Dalton for moisture content. The results of the work can be used in geocryology to model seasonal changes in the thermophysical state offrozen rocks and soils, in the theory of building structures to study the thermal regime of indoor premises with fluctuations in ambient temperature, in the theory of drying by electromagnetic radiation to study the processes of heat and mass transfer inoscillating modes.
半空间温度波傅里叶问题的推广
用复振幅法求解了边界受温度随调和律变化的气流吹入的半空间内温度和湿度的渐近波动问题。填充半空间的材料由固体基底(毛细管多孔体)和水组成。已知的无水分和第一类热交换边界条件下半空间温度波动的傅里叶解推广到温度为牛顿边界条件和水分含量为道尔顿边界条件下的湿材料的情况。研究结果可用于地学中模拟冻土热物理状态的季节变化,用于建筑结构理论中研究环境温度波动下室内场所的热状态,用于电磁辐射干燥理论中研究振荡模式下的传热传质过程。
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