From d90b3c46d052c847d4c2030335751e59ac63246f Mon Sep 17 00:00:00 2001 From: heister Date: Tue, 27 Sep 2011 14:01:48 +0000 Subject: [PATCH] fix some typos git-svn-id: https://svn.dealii.org/trunk@24449 0785d39b-7218-0410-832d-ea1e28bc413d --- deal.II/examples/step-32/doc/intro.dox | 8 ++++---- 1 file changed, 4 insertions(+), 4 deletions(-) diff --git a/deal.II/examples/step-32/doc/intro.dox b/deal.II/examples/step-32/doc/intro.dox index bdd4871880..78a0777172 100644 --- a/deal.II/examples/step-32/doc/intro.dox +++ b/deal.II/examples/step-32/doc/intro.dox @@ -810,8 +810,8 @@ the following quantities: 500 and 900 degrees Celsius, whereas at its bottom it is around 4000 degrees Celsius (see, for example, this Wikipedia - entry). In Kelvin, we therefore choose $T_0=(4000+273)\text{K}, - T_1=(500+273)\text{K}$ as boundary conditions at the inner and outer edge. + entry). In Kelvin, we therefore choose $T_0=(4000+273)\text{K}$, + $T_1=(500+273)\text{K}$ as boundary conditions at the inner and outer edge. In addition to this, we also have to specifiy some initial conditions for the temperature field. The real temperature field of the earth is quite @@ -978,7 +978,7 @@ the following quantities: & \text{for} \ \|\mathbf x\|The density of the earth mantle varies spatially, but not by very -- 2.39.5