The basic regularities of stationary heat transfer throughout the space of an infiltrated granular bed in radiative heat supply in cocurrent-flow (solar collector 1) and counterflow (solar collector 2) regimes have been investigated within the framework of a two-temperature model. The boundary layer of the third kind for the skeleton of particles at exit from the bed has been formulated; this condition allows for the degree of turbulence of the heat-transfer-agent flow. A quasihomogeneity criterion making it possible to evaluate the thermal state of a two-phase system has been introduced. The approximation dependences for calculation of the active-portion length, the bed’s resistance, the solar-collector efficiency, and the average relative phase-temperature difference have been established.
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Translated from Inzhenerno-Fizicheskii Zhurnal, Vol. 83, No. 3, pp. 544–553, May–June, 2010.
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Teplitskii, Y.S., Kovenskii, V.I. Heat transfer in granular beds in radiative heat supply. J Eng Phys Thermophy 83, 578–588 (2010). https://doi.org/10.1007/s10891-010-0379-2
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DOI: https://doi.org/10.1007/s10891-010-0379-2