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This document discusses natural convection and mass transfer. It defines natural convection as the transfer of heat from a solid surface to a fluid due to density variations in the fluid caused by temperature gradients. This causes hot air to rise and cooler, denser air to take its place, driving fluid motion. The Grashof and Rayleigh numbers are introduced to characterize natural convection, with Grashof number representing the ratio of buoyancy to viscous forces and Rayleigh number representing the produc

Author

Cheppanu Brother

Language

EN