From: Wolfgang Bangerth Date: Fri, 11 Sep 2009 00:13:01 +0000 (+0000) Subject: Write a couple more paragraphs. X-Git-Tag: v8.0.0~7142 X-Git-Url: https://gitweb.dealii.org/cgi-bin/gitweb.cgi?a=commitdiff_plain;h=40d5de1190b580d034841093cbc60cc0e0b86c0e;p=dealii.git Write a couple more paragraphs. git-svn-id: https://svn.dealii.org/trunk@19431 0785d39b-7218-0410-832d-ea1e28bc413d --- diff --git a/deal.II/examples/step-32/doc/intro.dox b/deal.II/examples/step-32/doc/intro.dox index dc2a418794..d4ffb3cdc6 100644 --- a/deal.II/examples/step-32/doc/intro.dox +++ b/deal.II/examples/step-32/doc/intro.dox @@ -115,7 +115,7 @@ A second reason to do this is discussed in the results section and concerns possible extensions to the model we use here. It has to do with the fact that while the temperature equation we use here does not include a term that contains the pressure. It should, however: -pressure, like gas, heats up as you compress it. Consequently, +rock, like gas, heats up as you compress it. Consequently, material that rises up cools adiabatically, and cold material that sinks down heats adiabatically. We discuss this further below. diff --git a/deal.II/examples/step-32/doc/results.dox b/deal.II/examples/step-32/doc/results.dox index cd6bee3ae8..5e9d3dad23 100644 --- a/deal.II/examples/step-32/doc/results.dox +++ b/deal.II/examples/step-32/doc/results.dox @@ -288,3 +288,44 @@ temperature layering is instable. It then calms down to relatively small values before picking up again in the chaotic stirring regime. There, it remains in the range of 10-40 centimeters per year, quite within the physically expected region. + + + + +

Possibilities for extensions

+ +Apart from the various possibilities for extensions already outlined +in the @ref step_31 "step-31", here are a few more ideas: + + \ No newline at end of file