Fix a wording problem.

git-svn-id: https://svn.dealii.org/trunk@19277 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 289c84f2b4db8fe0444fdbc27a0c139ac3382fe9..c8a8ef5b2db14cbc71bc36c0df2319c33298a836 100644 (file)
--- a/deal.II/examples/step-32/doc/intro.dox
+++ b/deal.II/examples/step-32/doc/intro.dox
@@ -351,8 +351,7 @@ SI system) even if we list them here in other units:
   Celsius (see, for example, <a target="_top"
   href="http://en.wikipedia.org/wiki/Mantle_(geology)">this Wikipedia
   entry</a>). In Kelvin, we therefore choose $T_0=(4000+273)\text{K},
-  T_1=(500+273)\text{K}$. These temperatures we choose as boundary
-  conditions at the inner and outer edge.
+  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