[cig-commits] r8103 - doc/CitcomS/manual
tan2 at geodynamics.org
tan2 at geodynamics.org
Wed Oct 10 17:05:16 PDT 2007
Author: tan2
Date: 2007-10-10 17:05:16 -0700 (Wed, 10 Oct 2007)
New Revision: 8103
Modified:
doc/CitcomS/manual/citcoms.lyx
Log:
Minor fix
Modified: doc/CitcomS/manual/citcoms.lyx
===================================================================
--- doc/CitcomS/manual/citcoms.lyx 2007-10-11 00:03:40 UTC (rev 8102)
+++ doc/CitcomS/manual/citcoms.lyx 2007-10-11 00:05:16 UTC (rev 8103)
@@ -630,9 +630,9 @@
n dependent viscosity and heat generation by Thorsten Becker; (7) compressed
ASCII output by Thorsten Becker; (8) an easier way for mesh refinement
for the radial coordinate by Thorsten Becker; (9) an exchanger package
- for solver coupling; (10) removing the rigid rotation component from the
- velocity by Shijie Zhong; and (11) an option to disable monitoring of maximum
- temperature.
+ for solver coupling; (10) removing the rigid body rotation component from
+ the velocity by Shijie Zhong; and (11) an option to disable monitoring
+ of maximum temperature.
Additional backward incompatible changes include: (1) the viscosity field
at element level is not smoothed (this might slow down the convergence
but will represent the viscosity field more accurately); (2) the Lenardic
@@ -9875,8 +9875,8 @@
The numerical solution of the velocity and stress fields can be compared
with semi-analytical solutions.
The Stokes solver is benchmarked and validated.
- However, no analytical solution exits for the benchmark on the energy equation
- solver, which is nonlinear.
+ However, no analytical solution exists for the benchmark on the energy
+ equation solver, which is nonlinear.
The steady-state solution is usually used for the comparison with other
numerical solutions.
@@ -16654,6 +16654,9 @@
\begin_inset Text
\begin_layout Standard
+
+\family typewriter
+\size small
uzawa=cg
\end_layout
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