Using the integral relations from Problem 19.17, and assuming the velocity and temperature profiles of the form
where δ is the thickness of both the hydrodynamic and thermal boundary layers, show that the solution in terms of δ and vx from each integral equation reduce to
Next, assuming that both δ and vx vary with x according to
show that the resulting expression for δ becomes
and that the local Nusselt number is
Problem 19.17
Show that, for the case of natural convection adjacent to a plane vertical wall, the appropriate integral equations for the hydrodynamic and thermal boundary layers are
We need at least 10 more requests to produce the solution.
0 / 10 have requested this problem solution
The more requests, the faster the answer.