<!DOCTYPE html>
The governing equation is now:
(7.1) |
along with the mass conservation equation 6.2. Here Re represents the Reynolds number, and the dimensional pressure has been nondimensionalized by .
Multiplied by a test function and integrated over the domain. the -component of equation 7.1 is:
(7.2) |
Recall the expansion for (equation 6.8, the first term on the left of 7.2is:
(7.3) |
for each element (), define advection element matrices as:
(7.4) |
These matrices can be evaluated initially, and reused throughout the calculation. For an element with baseline oriented an angle relative to the -axis: The corresponding is:
(7.5) |
If the base of an element is not parallel to the -axis (as illustrated in figure LABEL:Fi:C4S12triangles, form the matrix
(7.6) |
Then
(7.7) |
Assembling global matrices such as mass and stiffness proceeds in the usual fashion, adding contributions from each element cookie-cutter style. The global advection matrix has elements
(7.8) |
This matric is also assembled element by element, and has to be re-evaluated each time the velocity is re-evaluated.
Following chapter 6 the global problem can now be written
(7.9) |
The Dirichlet boundary conditions are handled as in the previous chapter:
(7.10) |
The new issue is that since is a priori unknown, an iterative method is needed. For these solution, the solution is computed first, then is evaluated based on the viscous solution. The process is repeated until convergence.