Thank you very much.
Best,
Xiang
On Wed, Oct 23, 2019 at 4:42 PM Wolfgang Bangerth
wrote:
>
> > Thank you for your reply. I will try it. The equations are: > [...]
>
> Both step 31 and 32 will be good starting points. The only difference is
> that you have Darcy flow instead of Stokes flow, bu
> Thank you for your reply. I will try it. The equations are: > [...]
Both step 31 and 32 will be good starting points. The only difference is
that you have Darcy flow instead of Stokes flow, but that should be easy
to incorporate into these programs.
Best
W.
--
--
Dr. Turcksin,
Thank you for the answer. Makes sense why I couldn't find it use apt
search. CMake's FindMPI was unable to find it though. Might just need to
give it some hints on the spack MPI location.
Either way, I realised that I'm using some features with bugs that were
fixed in the current
Hi, Wolfgang,
Thank you for your reply. I will try it. The equations are:
[image: image.png]
[image: image.png]
where T is temperature, p is pressure, u is flow rate. K is hydraulic
conductivity which is constant, κ and λ are the coefficients of heat
transfer. T1 means the temperature at boundary
Hi Prof Wolfgang,
Thanks for the insight. I figured a way of implementing it without any
interpolation, but to just use the normal traces of RT_0 in 2d at
different time levels directly to get the normal traces of RT_0 in
3d(2Dspace-1Dtime mesh).
regards,
Manu
On Sunday, October 20, 2019 at
On 10/23/19 3:05 AM, Prateek Sharma wrote:
>
> The problem that I am facing is that even if i extract the component of the
> solution that I want to modify, I can't extract the information about the
> gradient of the other component at the same node. We can extract the value of
> the solution a
On 10/22/19 10:57 PM, Xiang Sun wrote:
>
> Thank you for your reply. I am learning dealii to build up a geothermal
> model,
> which includes a Laplace equation and a heat transfer considering both
> convection and diffusion. The Laplace equation describes a pressure
> distibution in a site wit
Hello
I have a problem with the solution vector grouped into components of
displacement vector and one scalar component.
So esentially my solution vector is - (Ux, Uy, Uz, Scalar)
I want to modify the scalar with the help of the gradients of the
displacement vector after solving the system
