[cig-commits] r20802 - in short/3D/PyLith/branches/v1.7-trunk/doc/userguide: . materials runpylith
brad at geodynamics.org
brad at geodynamics.org
Mon Oct 1 17:27:12 PDT 2012
Author: brad
Date: 2012-10-01 17:27:11 -0700 (Mon, 01 Oct 2012)
New Revision: 20802
Modified:
short/3D/PyLith/branches/v1.7-trunk/doc/userguide/materials/materials.lyx
short/3D/PyLith/branches/v1.7-trunk/doc/userguide/runpylith/runpylith.lyx
short/3D/PyLith/branches/v1.7-trunk/doc/userguide/userguide.lyx
Log:
Proofreading.
Modified: short/3D/PyLith/branches/v1.7-trunk/doc/userguide/materials/materials.lyx
===================================================================
--- short/3D/PyLith/branches/v1.7-trunk/doc/userguide/materials/materials.lyx 2012-10-01 23:55:29 UTC (rev 20801)
+++ short/3D/PyLith/branches/v1.7-trunk/doc/userguide/materials/materials.lyx 2012-10-02 00:27:11 UTC (rev 20802)
@@ -1215,11 +1215,11 @@
\end_layout
\begin_layout Standard
-PyLith computes the stable time step for both quasi-static and dynamic simulatio
-ns.
+PyLith computes the stable time step in both quasi-static and dynamic simulation
+s.
In quasi-static simulations the stability of the implicit time stepping
- scheme does not depend on the time step, instead the stable time step is
- associated with the accuracy of the solution.
+ scheme does not depend on the time step; instead, the stable time step
+ is associated with the accuracy of the solution.
In purely elastic materials, the accuracy is independent of the time step,
so the stable time step is infinite.
For viscoelastic materials we ser the stable time step to be 1/5 of the
Modified: short/3D/PyLith/branches/v1.7-trunk/doc/userguide/runpylith/runpylith.lyx
===================================================================
--- short/3D/PyLith/branches/v1.7-trunk/doc/userguide/runpylith/runpylith.lyx 2012-10-01 23:55:29 UTC (rev 20801)
+++ short/3D/PyLith/branches/v1.7-trunk/doc/userguide/runpylith/runpylith.lyx 2012-10-02 00:27:11 UTC (rev 20802)
@@ -5797,7 +5797,11 @@
\begin_layout Description
filename_pattern Filename pattern in C/Python format for creating filename
for each fault.
- Default is
+ Default is
+\begin_inset Newline newline
+\end_inset
+
+
\family typewriter
output/fault_%s.h5
\family default
@@ -5805,7 +5809,7 @@
\end_layout
\begin_layout Description
-snapshots Array of timestamps for slip snapshosts (-1 means use last time
+snapshots Array of timestamps for slip snapshosts ([-1] means use last time
step in file, which is the default).
\end_layout
@@ -5828,7 +5832,7 @@
\end_layout
\begin_layout Standard
-This utility generates Xdmf files from HDF5 files conforming to the layout
+This utility generates Xdmf files from HDF5 files that conform to the layout
used by PyLith.
It is a simple Python script with a single command line argument, the HDF5
file for input.
@@ -5853,7 +5857,7 @@
\series default
If the HDF5 files contain external datasets, then this utility should be
- run from the relative path as when the HDF5 files were created.
+ run from the same relative path to the HDF5 files as when they were created.
For example, if a PyLith simulation was run from directory
\family typewriter
work
Modified: short/3D/PyLith/branches/v1.7-trunk/doc/userguide/userguide.lyx
===================================================================
--- short/3D/PyLith/branches/v1.7-trunk/doc/userguide/userguide.lyx 2012-10-01 23:55:29 UTC (rev 20801)
+++ short/3D/PyLith/branches/v1.7-trunk/doc/userguide/userguide.lyx 2012-10-02 00:27:11 UTC (rev 20802)
@@ -512,8 +512,7 @@
\end_inset
-Courant, R.
- and K.
+Courant, R., K.
Friedrichs and H.
Lewy (1967), On the Partial Differential Equations of Mathematical Physics,
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