Note: This discussion is about an older version of the COMSOL Multiphysics® software. The information provided may be out of date.
Discussion Closed This discussion was created more than 6 months ago and has been closed. To start a new discussion with a link back to this one, click here.
How Does a "Temperature Boundary" Handle Heat Flux?
Posted Aug 1, 2015, 12:57 p.m. EDT Heat Transfer & Phase Change, Modeling Tools & Definitions, Parameters, Variables, & Functions Version 4.4 1 Reply
Please login with a confirmed email address before reporting spam
In my problem, I am letting a hot body of magma cool in the Earth's crust.
The far lateral boundary in the 2D axi-symmetric setup is prescribed a depth dependent T.
I SEE that when I run the model ... even for millions of years ... the crust retains that temperature prescription. Which is good.
But how is the "temperature boundary" actually handling it when heat from my hot body fluxes over to it?
It doesn't seem the insulate / accumulate
Is there a flux through the boundary?
Is the heat actually just "deleted" when it arrives, since the Temperature cannot be altered?
The far lateral boundary in the 2D axi-symmetric setup is prescribed a depth dependent T.
I SEE that when I run the model ... even for millions of years ... the crust retains that temperature prescription. Which is good.
But how is the "temperature boundary" actually handling it when heat from my hot body fluxes over to it?
It doesn't seem the insulate / accumulate
Is there a flux through the boundary?
Is the heat actually just "deleted" when it arrives, since the Temperature cannot be altered?
1 Reply Last Post Aug 3, 2015, 2:06 a.m. EDT