[cig-commits] r7723 - cs/cigma/branches/cigma-0.9b1/doc/manual

sue at geodynamics.org sue at geodynamics.org
Fri Jul 20 11:35:24 PDT 2007


Author: sue
Date: 2007-07-20 11:35:22 -0700 (Fri, 20 Jul 2007)
New Revision: 7723

Modified:
   cs/cigma/branches/cigma-0.9b1/doc/manual/cigma.lyx
   cs/cigma/branches/cigma-0.9b1/doc/manual/cigma.pdf
Log:
final pdf; changed 0,10,50,100 to 0,1,5,10; minor typos

Modified: cs/cigma/branches/cigma-0.9b1/doc/manual/cigma.lyx
===================================================================
--- cs/cigma/branches/cigma-0.9b1/doc/manual/cigma.lyx	2007-07-20 17:14:55 UTC (rev 7722)
+++ cs/cigma/branches/cigma-0.9b1/doc/manual/cigma.lyx	2007-07-20 18:35:22 UTC (rev 7723)
@@ -745,10 +745,6 @@
 \end_layout
 
 \begin_layout Standard
-(TODO: place image and equations side by side..)
-\end_layout
-
-\begin_layout Standard
 \noindent
 \align center
 \begin_inset Float figure
@@ -766,20 +762,12 @@
 \align center
 \begin_inset Graphics
 	filename figures/reference-tet4.png
-	lyxscale 40
-	width 40page%
+	lyxscale 35
+	width 35page%
 
 \end_inset
 
 
-\end_layout
-
-\end_inset
-
-
-\end_layout
-
-\begin_layout Standard
 \begin_inset Formula \begin{eqnarray*}
 TN_{a} & = & \frac{1}{2}(-1-x-y-z)\\
 TN_{b} & = & \frac{1}{2}(1+x)\\
@@ -791,6 +779,11 @@
 
 \end_layout
 
+\end_inset
+
+
+\end_layout
+
 \begin_layout Standard
 
 \newpage
@@ -804,10 +797,6 @@
 \end_layout
 
 \begin_layout Standard
-(TODO: place image and equations side by side..)
-\end_layout
-
-\begin_layout Standard
 \noindent
 \align center
 \begin_inset Float figure
@@ -825,20 +814,12 @@
 \align center
 \begin_inset Graphics
 	filename figures/reference-hex8.png
-	lyxscale 40
-	width 40page%
+	lyxscale 35
+	width 35page%
 
 \end_inset
 
 
-\end_layout
-
-\end_inset
-
-
-\end_layout
-
-\begin_layout Standard
 \begin_inset Formula \begin{eqnarray*}
 HN_{a} & = & \frac{1}{8}\left(1-x\right)\left(1-y\right)\left(1-z\right)\\
 HN_{b} & = & \frac{1}{8}\left(1+x\right)\left(1-y\right)\left(1-z\right)\\
@@ -854,6 +835,11 @@
 
 \end_layout
 
+\end_inset
+
+
+\end_layout
+
 \begin_layout Chapter
 Running Cigma
 \end_layout
@@ -863,7 +849,8 @@
 \end_layout
 
 \begin_layout Standard
-Comparing two arbitrary finite element fields can be accomplished with 
+Comparing two arbitrary finite element fields can be accomplished with the
+ 
 \family typewriter
 cigma-compare
 \family default
@@ -1055,7 +1042,7 @@
 
 \begin_layout Description
 MeshID a universally unique identifier (uuid) assigned to the mesh for easily
- distinguishing identical meshes
+ distinguishing identical meshes.
 \end_layout
 
 \begin_layout Description
@@ -1074,12 +1061,11 @@
 
 \begin_layout Standard
 In its source distribution, Cigma provides two examples for importing data
- from two different codes into its standard HDF5 format
-\newline
+ from two different codes into its standard HDF5 format.
+\end_layout
 
-\newline
-Mesh coordinates
- can be specified in the following format
+\begin_layout Standard
+Mesh coordinates can be specified in the following format
 \end_layout
 
 \begin_layout LyX-Code
@@ -1335,7 +1321,7 @@
 
 \begin_layout Standard
 In both cases we solve for the displacement and vector fields at various
- time steps, namely 0, 10, 50, and 100 years.
+ time steps, namely 0, 1, 5, and 10 years.
  In the plots below, we show the distribution of the squared local residuals
  on each cell.
 \end_layout
@@ -1346,14 +1332,14 @@
 
 \begin_layout Standard
 In this section, we show ten equally spaced isosurfaces of the displacement
- field residuals for the strike-slip benchmark (0 and 100 years shown).
+ field residuals for the strike-slip benchmark (0 and 10 years shown).
  In Figure 
 \begin_inset LatexCommand \ref{fig:PyLith-solution}
 
 \end_inset
 
 , we see that the differences are very localized at t=0 years.
- There is not much difference between time steps at t=10, 50 and 100 years,
+ There is not much difference between time steps at t=1, 5 and 10 years,
  so we are only showing the last time step.
  Note that the maximum errors are localized to the interface between the
  two layers on the symmetric boundary.
@@ -1395,7 +1381,7 @@
 
 \begin_layout Caption
 Strike-slip: PyLith-GeoFEST comparison of displacement residuals on a 500m
- resolution mesh (left: t=0 years, right: t=100 years).
+ resolution mesh (left: t=0 years, right: t=10 years).
 \end_layout
 
 \end_inset
@@ -1408,7 +1394,7 @@
  Shown here are ten equally spaced isosurfaces at each time step, where
  each isosurface is displayed as a point distribution to reveal the inner
  structure.
- Note that after 100 years, most of the disagreement occurs inside the bottom
+ Note that after 10 years, most of the disagreement occurs inside the bottom
  viscoelastic layer, centered around the fault's interior sharp corner.
 \end_layout
 
@@ -1448,7 +1434,7 @@
 
 \begin_layout Caption
 Strike-slip: PyLith-GeoFEST comparison of velocity residuals on a 500m resolutio
-n mesh (left: t=0 years, right: t=10 years).
+n mesh (left: t=0 years, right: t=1 year).
 \end_layout
 
 \end_inset
@@ -1492,7 +1478,7 @@
 
 \begin_layout Caption
 Strike-slip: PyLith-GeoFEST comparison of velocity residuals on a 500m resolutio
-n mesh (left: t=50 years, right: t=100 years).
+n mesh (left: t=5 years, right: t=10 years).
  
 \end_layout
 
@@ -1596,7 +1582,7 @@
 
 \begin_layout Caption
 Reverse-slip: PyLith-GeoFEST comparison of velocity residuals on a 500m
- resolution mesh (left: t=0 years, right: t=10 years).
+ resolution mesh (left: t=0 years, right: t=1 year).
 \end_layout
 
 \end_inset
@@ -1640,7 +1626,7 @@
 
 \begin_layout Caption
 Reverse-slip: PyLith-GeoFEST comparison of velocity residuals on a 500m
- resolution mesh (left: t=50 years, right: t=100 years).
+ resolution mesh (left: t=5 years, right: t=10 years).
 \end_layout
 
 \end_inset
@@ -1651,8 +1637,8 @@
 \begin_layout Standard
 Finally, below we display ten equally spaced isosurfaces over the displacement
  field residuals of the reverse-slip benchmark.
- Note that after 10 years, most of the disagreement occurs in the bottom
- viscoelastic layer.
+ Note that after 1 year, most of the disagreement occurs in the bottom viscoelas
+tic layer.
 \end_layout
 
 \begin_layout Standard
@@ -1691,7 +1677,7 @@
 
 \begin_layout Caption
 Reverse-slip: PyLith-GeoFEST comparison of displacement residuals on a 500m
- resolution mesh (left: t=0 years, right: t=10 years).
+ resolution mesh (left: t=0 years, right: t=1 year).
 \end_layout
 
 \end_inset
@@ -1735,7 +1721,7 @@
 
 \begin_layout Caption
 Reverse-slip: PyLith-GeoFEST comparison of displacement residuals on a 500m
- resolution mesh (left: t=50 years, right: t=100 years).
+ resolution mesh (left: t=5 years, right: t=10 years).
 \end_layout
 
 \end_inset
@@ -1765,6 +1751,7 @@
 \begin_layout Standard
 \begin_inset Graphics
 	filename figures/cigma-abcd-triangle.jpg
+	lyxscale 25
 	scale 25
 
 \end_inset

Modified: cs/cigma/branches/cigma-0.9b1/doc/manual/cigma.pdf
===================================================================
(Binary files differ)



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