The following codes is about global_displacement from ex8. I change "displacement" in .get_vector() using my variables' name. I can get the corresponding values of my variables by using different variables' name? However,
how to know the corresponding relationship between the index of this vector and the global index of point in the mesh, global degree of freedom number in parallel?
dof_no may not be local in parallel runs, so we may need a global displacement vector
std::vector<Number> global_displacement(displacement.size ());
Write nodal results to file. The results can then be viewed with e.g. gnuplot (run gnuplot and type 'plot "pressure_node.res" with lines' in the command line)
res_out << t_time << "\t"
In addition, regarding the codes from build_discontious_solution_vector();
I think that
update_globle_solution() for geting all solutions on one processor. ?
00602 for (unsigned int i=0; i<dof_indices.size(); i++)
00603 elem_soln[i] = sys_soln[dof_indices[i]];
for dispatching the values to the corresponding point of variable.?
00605 FEInterface::nodal_soln (dim,
Is it right?
thanks a lot.
On Thu, 4 Oct 2007, Yujie wrote:
> Because I have several variables in my system.
The code I previously suggested will work just fine no matter how many
variables are in your system.
> I think the following codes should be better. It is from
That code doesn't do what you asked, though; you said you wanted to
get the solution all on one processor. If what you really want is a
nodal interpolant of the solution all on one processor, then the code
we use for generating visualization output will work fine too.
> I always want to confirm whether the reference element in FE:inverse_map()
> is isoparameter element?
No. The shape functions are determined by your FEType; the mapping
functions are determined by your Elem type. Elements may be iso,
super, or subparametric.
> We will integrate on the isoparameter element. The
> integrate results on the physical element can be obtained by the values
> times Jacobian. Inverse_map() want to get point (physical element)'s
> position (reference element).
inverse_map() may be used to simplify the code when integrating on
element sides; but not on element interiors. On element interiors the
reference points are generated directly by the quadrature rule and
only forward maps are ever needed (if you get_xyz()).
> if the FEtype is first-order lagrange. I think it is simple to get
> such corresponding relationship. If the FEtype is complicated, it
> will be difficulat to perform inverse_map(). Is it right?
An inverse_map() requires a Newton iteration, which will take more
than a step or two if you're not using linear geometric elements, but
it's hardly difficult, and as far as your code is concerned it's all