Natural Convection Heat Transfer in an Inclined Air Layer Packed with Spherical Particles

Experiments of natural convection heat transfer in an inclined air layer with spherical particles under isothermal heating and cooling conditions were carried out for the ranges of inclination angles (θ=0180°), aspect-ratios (H/W=2.57.9), modified Prandtl numbers (P*r=1.145), ratios of diameter of s...

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Published inTransactions of the Japan Society of Mechanical Engineers Series B Vol. 51; no. 471; pp. 3766 - 3771
Main Authors INABA, Hideo, SUGAWARA, Masahiro, FUKUDA, Takeyuki
Format Journal Article
LanguageJapanese
Published The Japan Society of Mechanical Engineers 25.11.1985
Subjects
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ISSN0387-5016
1884-8346
DOI10.1299/kikaib.51.3766

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Abstract Experiments of natural convection heat transfer in an inclined air layer with spherical particles under isothermal heating and cooling conditions were carried out for the ranges of inclination angles (θ=0180°), aspect-ratios (H/W=2.57.9), modified Prandtl numbers (P*r=1.145), ratios of diameter of spherical particles to width of the porous layer (d/W=0.040.516) and modified Rayleigh numbers (R*a=2.2×101.03×103). According to the inclination angle, the convection heat transfer in the porous layer varied because of the change of the convection flow type. In addition, useful correlations of non-dimensional convection heat transfer were derived in the relations Nusselt number Nu=f[P*r, d/W, R*a cos(θ-60°)] for θ=015°, and Nu=f[P*r, H/W, R*a (θ-60°)] for θ=0120°.
AbstractList Experiments of natural convection heat transfer in an inclined air layer with spherical particles under isothermal heating and cooling conditions were carried out for the ranges of inclination angles (θ=0180°), aspect-ratios (H/W=2.57.9), modified Prandtl numbers (P*r=1.145), ratios of diameter of spherical particles to width of the porous layer (d/W=0.040.516) and modified Rayleigh numbers (R*a=2.2×101.03×103). According to the inclination angle, the convection heat transfer in the porous layer varied because of the change of the convection flow type. In addition, useful correlations of non-dimensional convection heat transfer were derived in the relations Nusselt number Nu=f[P*r, d/W, R*a cos(θ-60°)] for θ=015°, and Nu=f[P*r, H/W, R*a (θ-60°)] for θ=0120°.
Author INABA, Hideo
SUGAWARA, Masahiro
FUKUDA, Takeyuki
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(1) Combarnous, M.A. and Bories, S.A. Adv. Hydosci., 10 (1975), 231.
References_xml – reference: (3) Schneider, K.J.. Proc. 11th. Int. Congr. Refrig. 11-4 (1963), 247.
– reference: (9) Kunii, D. and Smith, J.M., AIChE J., 6-1 (1960), 71.
– reference: (2) Kaneko, T.,ほか2名, Int. J. Heat Mass, Transf., 17-2 (1974), 485.
– reference: (6) Yagi, S. and Kunii. D, Int. Dev. Hert Transf. 4-3 (1962), 750.
– reference: (7) 増岡,機論,37-293(昭46),90.
– reference: (10) 関•ほか2名,機論,45-393-B(昭54), 705.
– reference: (11) Seki, N.ほか2名, Int. J. Heat Mass Transf., 21-10 (1960), 985.
– reference: (8) Schmidt, E. and Silveston, P.L., Chem. Eng. Sym. Ser., 55-29 (1959), 163.
– reference: (1) Combarnous, M.A. and Bories, S.A. Adv. Hydosci., 10 (1975), 231.
– reference: (4) Vlasuk, M.P., Proc. 4th All-Union Heat Mass Transf. Conf., 11-4 (1972). 45.
– reference: (5) Holst, P.H. and Aziz. K., Can. J. Chem. Eng. 50-2 (1972), 232.
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Snippet Experiments of natural convection heat transfer in an inclined air layer with spherical particles under isothermal heating and cooling conditions were carried...
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SubjectTerms Inclined Porous Layer /Experimental Study
Title Natural Convection Heat Transfer in an Inclined Air Layer Packed with Spherical Particles
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