Fluid motion in the natural convection heat transfer between a solid
surface and a fluid in contact with it, results from the
(A) Existence of thermal boundary layer
(B) Temperature gradient produced due to density difference
(C) Buoyancy of the bubbles produced at active nucleation site
(D) None of these
surface and a fluid in contact with it, results from the
(A) Existence of thermal boundary layer
(B) Temperature gradient produced due to density difference
(C) Buoyancy of the bubbles produced at active nucleation site
(D) None of these