Quote: Originally posted by annaandherdad | I have a lot of questions, but let me just start with one. Why are the boundary conditions at x=R1, dT/dx=0? If I have a slab with different
temperatures on each side, for example, the wall of your house in winter, then the temperature profile inside the slab is just a straight line going
from T0 at one side to T1 at the other (modelling the wall as if it were a uniform material). My point is that dT/dx is not zero at the interface.
The boundary conditions are given by the two temperatures, not the derivatives of temperatures. |
Actually, with the temperature profile of a wall, from inside to outside, the outside temperature of the wall is not T1 either, see here:
http://web.mit.edu/16.unified/www/FALL/thermodynamics/notes/...
You start from the assumption that the edge of the fin is at T<sub>∞</sub> but that <i>simply isn’t true</i>.
If you stick one end of a poker (rod) into an open fire, do you expect the ‘cold’ end to be at room temperature? I sure as hell hope not
because otherwise you’re going to get a lot of burnt fingers! The
edge temperature of the rod tends to T<sub>∞</sub> only for rods with length L = ∞ (all other things being equal). It's the
same for radial fins.
What IS true is that at the edge of the fin no more heat is conducted (because there is no more fin!) and by Fourrier that means that at x =
R<sub>1</sub>, the temperature gradient (dT/dx)<sub>x=R1</sub> = 0. The only error we’re making is that we neglect that
little bit of convection heat that comes off the edge of the fin, which would be 2 π R<sub>1</sub> h t (T<sub>1</sub> -
T<sub>∞</sub>. For very 'stubby' fins that would be a concern.
[Edited on 7-5-2015 by blogfast25] |