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Natural convection and entropy generation of ultrafine atmospheric aerosols in the presence of hydrodynamic partial slip and thermal radiation due to solar energy

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Figure

Figure 1. Physical conguration of studied problem and Cartesian coordinates, where L = 1.
Table 1. Thermo-physical properties of base 
uid and suspended nanoparticles [6].
Figure 2. Comparison of the average temperature on the mid plane of the cavity obtained by the present method and results of Khanafer et al
Figure 3a. Streamlines evolution by hydrodynamic partial slip coecient and solid volume fraction of nanoparticles, when Ri = 10 and Rd = 0.
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