Hi, Wolfgang,
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 with several wellbores. The heat transfer
On 10/22/19 10:41 AM, Xiang Sun wrote:
>
> In step-31, why did you define the residual by multiplying T^(a-1)? What does
> "a" mean? Thank you very much.
I assume you mean here?
https://dealii.org/developer/doxygen/deal.II/step_31.html#Stabilizationweakformandspacediscretizationforthetemperature
Hi Zhidong,
On Monday, October 21, 2019 at 1:42:30 AM UTC+2, Zhidong Brian Zhang wrote:
>
> Thank you very much for your prompt reply, Konrad!
>
> My confusion is the output of cell->id(), for example,
> 0_3:000
> 0_3:200
> 0_3:003
> 0_3:006
> 0_3:406
> 0_3:606
> 0_3:206
> 0_3:007
> 0_3:407
> 0_3:
Hi,
In step-31, why did you define the residual by multiplying T^(a-1)? What
does "a" mean? Thank you very much.
Best,
Xiang
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You received this
Doug,
You are using an image build using spack so everything is installed using
spack instead of the package manager. If you type `spack find` inside a
container, you will see that mpich is installed.
Best,
Bruno
On Monday, October 21, 2019 at 9:53:36 PM UTC-4, Doug Shi-Dong wrote:
>
> Hello
