[cig-commits] r15859 - in doc/geodynamics.org/benchmarks/trunk: long mc
luis at geodynamics.org
luis at geodynamics.org
Wed Oct 21 13:05:56 PDT 2009
Author: luis
Date: 2009-10-21 13:05:55 -0700 (Wed, 21 Oct 2009)
New Revision: 15859
Modified:
doc/geodynamics.org/benchmarks/trunk/long/circular-inclusion.html
doc/geodynamics.org/benchmarks/trunk/long/circular-inclusion.rst
doc/geodynamics.org/benchmarks/trunk/long/divergence.html
doc/geodynamics.org/benchmarks/trunk/long/divergence.rst
doc/geodynamics.org/benchmarks/trunk/long/drucker-prager.html
doc/geodynamics.org/benchmarks/trunk/long/drucker-prager.rst
doc/geodynamics.org/benchmarks/trunk/long/geomod2004.html
doc/geodynamics.org/benchmarks/trunk/long/geomod2004.rst
doc/geodynamics.org/benchmarks/trunk/long/geomod2008.html
doc/geodynamics.org/benchmarks/trunk/long/geomod2008.rst
doc/geodynamics.org/benchmarks/trunk/long/relaxation-topography.html
doc/geodynamics.org/benchmarks/trunk/long/relaxation-topography.rst
doc/geodynamics.org/benchmarks/trunk/mc/index.html
doc/geodynamics.org/benchmarks/trunk/mc/index.rst
Log:
Misc fixes
Modified: doc/geodynamics.org/benchmarks/trunk/long/circular-inclusion.html
===================================================================
--- doc/geodynamics.org/benchmarks/trunk/long/circular-inclusion.html 2009-10-21 20:05:44 UTC (rev 15858)
+++ doc/geodynamics.org/benchmarks/trunk/long/circular-inclusion.html 2009-10-21 20:05:55 UTC (rev 15859)
@@ -32,7 +32,7 @@
v_x &= -\dot{\epsilon}y, \\
v_y &= \dot{\epsilon}x,
\end{align*};]</blockquote>
-<p>for the boundaries, where [;\dot{\epsilon};] is the magnitude of
+<p>for the boundaries, where [;\dot{\epsilon}=1;] is the magnitude of
the shear and [;x;] and [;y;] are the coordinates. This induces an
error of order [;r_i^2/r^2;], where [;r_i=0.1;] is the radius of
the inclusion, and [;r;] is the radius. We have the boundaries
@@ -58,11 +58,11 @@
numerical scheme is not accurate.</p>
<!-- fig:Pressure-Inclusion -->
<div align="center" class="figure">
-<img alt="Pressure Field" src="images/inclusion_r8_p.png" style="width: 80%;" />
+<img alt="Pressure Field" src="images/inclusion_r8_p.png" style="width: 600px;" />
<p class="caption"><span class="target" id="figure-2">Figure 2</span>:
Pressure along the line [;y=x/2;] for resolutions of
-[;128 \times 128;] (blue), [;256 \times 256;] (red),
-and [;512 \times 512;] (black). The inclusion has radius
+128 × 128 (blue), 256 × 256 (red),
+and 512 × 512 (black). The inclusion has radius
[;r_i=0.1;]. Note that the pressure should be zero
inside the inclusion, but the numerical solutions
consistently underestimate the pressure.</p>
@@ -80,18 +80,16 @@
this problem [FD Stokes].</p>
<!-- fig:Pressure-Error -->
<div align="center" class="figure">
-<img alt="Pressure Error" src="images/inclusion_r8_p_error.png" style="width: 80%;" />
+<img alt="Pressure Error" src="images/inclusion_r8_p_error.png" style="width: 600px;" />
<p class="caption"><span class="target" id="figure-3">Figure 3</span>:
Error in the pressure outside the inclusion along
-the line [;y=x/2;] for resolutions of
-[;128 \times 128;] (blue),
-[;256 \times 256;] (red), and
-[;512 \times 512;] (black).
+the line [;y=x/2;] for resolutions of 128 × 128 (blue),
+256 × 256 (red), and 512 × 512 (black).
The inclusion has radius [;r_i=0.1;].</p>
</div>
<!-- fig:Scaled-pressure-error -->
<div align="center" class="figure">
-<img alt="Scaled Pressure Error" src="images/inclusion_r8_p_scaled_error.png" style="width: 80%;" />
+<img alt="Scaled Pressure Error" src="images/inclusion_r8_p_scaled_error.png" style="width: 600px;" />
<p class="caption"><span class="target" id="figure-4">Figure 4</span>:
As in <a class="reference internal" href="#figure-3">Figure 3</a>, but with the error scaled with [;h;].
So the medium-resolution error is multiplied by 2 and the
Modified: doc/geodynamics.org/benchmarks/trunk/long/circular-inclusion.rst
===================================================================
--- doc/geodynamics.org/benchmarks/trunk/long/circular-inclusion.rst 2009-10-21 20:05:44 UTC (rev 15858)
+++ doc/geodynamics.org/benchmarks/trunk/long/circular-inclusion.rst 2009-10-21 20:05:55 UTC (rev 15859)
@@ -1,4 +1,3 @@
-
Circular Inclusion
==================
@@ -28,7 +27,7 @@
v_y &= \\dot{\\epsilon}x,
\\end{align*};]
-for the boundaries, where [;\\dot{\\epsilon};] is the magnitude of
+for the boundaries, where [;\\dot{\\epsilon}=1;] is the magnitude of
the shear and [;x;] and [;y;] are the coordinates. This induces an
error of order [;r_i^2/r^2;], where [;r_i=0.1;] is the radius of
the inclusion, and [;r;] is the radius. We have the boundaries
@@ -60,12 +59,12 @@
.. figure:: images/inclusion_r8_p.png
:alt: Pressure Field
:align: center
- :width: 80%
+ :width: 600
_`Figure 2`:
Pressure along the line [;y=x/2;] for resolutions of
- [;128 \\times 128;] (blue), [;256 \\times 256;] (red),
- and [;512 \\times 512;] (black). The inclusion has radius
+ 128 |times| 128 (blue), 256 |times| 256 (red),
+ and 512 |times| 512 (black). The inclusion has radius
[;r_i=0.1;]. Note that the pressure should be zero
inside the inclusion, but the numerical solutions
consistently underestimate the pressure.
@@ -87,14 +86,12 @@
.. figure:: images/inclusion_r8_p_error.png
:alt: Pressure Error
:align: center
- :width: 80%
+ :width: 600
_`Figure 3`:
Error in the pressure outside the inclusion along
- the line [;y=x/2;] for resolutions of
- [;128 \\times 128;] (blue),
- [;256 \\times 256;] (red), and
- [;512 \\times 512;] (black).
+ the line [;y=x/2;] for resolutions of 128 |times| 128 (blue),
+ 256 |times| 256 (red), and 512 |times| 512 (black).
The inclusion has radius [;r_i=0.1;].
@@ -102,11 +99,11 @@
.. figure:: images/inclusion_r8_p_scaled_error.png
:alt: Scaled Pressure Error
:align: center
- :width: 80%
+ :width: 600
_`Figure 4`:
As in `Figure 3`_, but with the error scaled with [;h;].
So the medium-resolution error is multiplied by 2 and the
high-resolution error is multiplied by 4.
-
+.. |times| unicode:: U+00D7
Modified: doc/geodynamics.org/benchmarks/trunk/long/divergence.html
===================================================================
--- doc/geodynamics.org/benchmarks/trunk/long/divergence.html 2009-10-21 20:05:44 UTC (rev 15858)
+++ doc/geodynamics.org/benchmarks/trunk/long/divergence.html 2009-10-21 20:05:55 UTC (rev 15859)
@@ -37,7 +37,7 @@
a finite number of particles.</p>
<!-- fig:Divergence_v_sri -->
<div align="center" class="figure">
-<img alt="images/divergence_v.png" src="images/divergence_v.png" style="width: 60%;" />
+<img alt="images/divergence_v.png" src="images/divergence_v.png" style="width: 450px;" />
<p class="caption"><span class="target" id="figure-1">Figure 1</span>:
Velocity and Strain Rate Invariant solution
for the 2D Divergence benchmark. The variation
Modified: doc/geodynamics.org/benchmarks/trunk/long/divergence.rst
===================================================================
--- doc/geodynamics.org/benchmarks/trunk/long/divergence.rst 2009-10-21 20:05:44 UTC (rev 15858)
+++ doc/geodynamics.org/benchmarks/trunk/long/divergence.rst 2009-10-21 20:05:55 UTC (rev 15859)
@@ -32,7 +32,7 @@
.. fig:Divergence_v_sri
.. figure:: images/divergence_v.png
:align: center
- :width: 60%
+ :width: 450
_`Figure 1`:
Velocity and Strain Rate Invariant solution
Modified: doc/geodynamics.org/benchmarks/trunk/long/drucker-prager.html
===================================================================
--- doc/geodynamics.org/benchmarks/trunk/long/drucker-prager.html 2009-10-21 20:05:44 UTC (rev 15858)
+++ doc/geodynamics.org/benchmarks/trunk/long/drucker-prager.html 2009-10-21 20:05:55 UTC (rev 15859)
@@ -46,7 +46,7 @@
any confounding effects they may cause.</p>
<!-- fig:Mohr-Coulomb-setup -->
<div align="center" class="figure">
-<img alt="images/Mohr_Coulomb_setup.png" src="images/Mohr_Coulomb_setup.png" style="width: 40%;" />
+<img alt="images/Mohr_Coulomb_setup.png" src="images/Mohr_Coulomb_setup.png" style="width: 400px;" />
<p class="caption"><span class="target" id="figure-1">Figure 1</span>:
The setup for the shortening experiment.
The box is 1 unit on a side, and the low viscosity region
@@ -65,7 +65,7 @@
our Drucker-Prager implementation gives the correct results.</p>
<!-- fig:Mohr-Coulomb-sri -->
<div align="center" class="figure">
-<img alt="images/Mohr_coulomb_resolutions.png" src="images/Mohr_coulomb_resolutions.png" style="width: 80%;" />
+<img alt="images/Mohr_coulomb_resolutions.png" src="images/Mohr_coulomb_resolutions.png" style="width: 400px;" />
<p class="caption"><span class="target" id="figure-2">Figure 2</span>:
Strain rate invariant for the shortening experiment where
[;\varphi=45^{\circ};] with three different resolutions:
Modified: doc/geodynamics.org/benchmarks/trunk/long/drucker-prager.rst
===================================================================
--- doc/geodynamics.org/benchmarks/trunk/long/drucker-prager.rst 2009-10-21 20:05:44 UTC (rev 15858)
+++ doc/geodynamics.org/benchmarks/trunk/long/drucker-prager.rst 2009-10-21 20:05:55 UTC (rev 15859)
@@ -44,7 +44,7 @@
.. fig:Mohr-Coulomb-setup
.. figure:: images/Mohr_Coulomb_setup.png
:align: center
- :width: 40%
+ :width: 400
_`Figure 1`:
The setup for the shortening experiment.
@@ -68,7 +68,7 @@
.. fig:Mohr-Coulomb-sri
.. figure:: images/Mohr_coulomb_resolutions.png
:align: center
- :width: 80%
+ :width: 400
_`Figure 2`:
Strain rate invariant for the shortening experiment where
Modified: doc/geodynamics.org/benchmarks/trunk/long/geomod2004.html
===================================================================
--- doc/geodynamics.org/benchmarks/trunk/long/geomod2004.html 2009-10-21 20:05:44 UTC (rev 15858)
+++ doc/geodynamics.org/benchmarks/trunk/long/geomod2004.html 2009-10-21 20:05:55 UTC (rev 15859)
@@ -33,7 +33,7 @@
calculations for other codes.</p>
<!-- fig:Extension-model-setup -->
<div align="center" class="figure">
-<img alt="images/Extension_setup.png" src="images/Extension_setup.png" style="width: 90%;" />
+<img alt="images/Extension_setup.png" src="images/Extension_setup.png" style="width: 650px;" />
<p class="caption">Extension model setup. Reproduced, with permission, from Buiter et al.
[Buiter et al Numerical Sandbox]</p>
</div>
@@ -47,7 +47,7 @@
character of the solution.</p>
<!-- fig:Comparison-extension -->
<div align="center" class="figure">
-<img alt="images/Extension_comparision.png" src="images/Extension_comparision.png" style="width: 80%;" />
+<img alt="images/Extension_comparision.png" src="images/Extension_comparision.png" style="width: 600px;" />
<p class="caption">Strain rate invariant for the numerical extension models after 5 cm of
extension. The resolutions of the various models are:
I2ELVIS: 400 × 75,
@@ -61,7 +61,7 @@
</div>
<!-- fig:extension-convergence -->
<div align="center" class="figure">
-<img alt="images/extension_sensitivity.png" src="images/extension_sensitivity.png" style="width: 80%;" />
+<img alt="images/extension_sensitivity.png" src="images/extension_sensitivity.png" style="width: 600px;" />
<p class="caption">Strain rate invariant for the extension model after 5 cm of extension
for four different resolutions: (a) 128 × 16, (b) 256 × 32,
(c) 512 × 64, and (d) 1024 × 128.</p>
@@ -81,7 +81,7 @@
not prescribed by the benchmark, so we have used 10<sup>12</sup> Pa-s.</p>
<!-- fig:Shortening-model-setup -->
<div align="center" class="figure">
-<img alt="images/Shortening_setup.png" src="images/Shortening_setup.png" style="width: 90%;" />
+<img alt="images/Shortening_setup.png" src="images/Shortening_setup.png" style="width: 650px;" />
<p class="caption">Shortening model setup. Reproduced, with permission, from Buiter et al.
[Buiter et al Numerical Sandbox].</p>
</div>
@@ -93,7 +93,7 @@
marked differences in behavior as we increase resolution.</p>
<!-- fig:shortening-compare -->
<div align="center" class="figure">
-<img alt="images/Shortening_comparison.png" src="images/Shortening_comparison.png" style="width: 80%;" />
+<img alt="images/Shortening_comparison.png" src="images/Shortening_comparison.png" style="width: 600px;" />
<p class="caption">Strain rate invariant for the numerical shortening models after 14 cm
of shortening. The resolutions of the various models are:
I2ELVIS: 900 × 75,
@@ -106,7 +106,7 @@
</div>
<!-- fig:shortening-convergence -->
<div align="center" class="figure">
-<img alt="images/shortening_sensitivity.png" src="images/shortening_sensitivity.png" style="width: 80%;" />
+<img alt="images/shortening_sensitivity.png" src="images/shortening_sensitivity.png" style="width: 600px;" />
<p class="caption">Strain rate invariant for the shortening model after 14 cm of
shortening for three different resolutions: (a) 128 × 32,
(b) 256 × 64, (c) 512 × 128.</p>
Modified: doc/geodynamics.org/benchmarks/trunk/long/geomod2004.rst
===================================================================
--- doc/geodynamics.org/benchmarks/trunk/long/geomod2004.rst 2009-10-21 20:05:44 UTC (rev 15858)
+++ doc/geodynamics.org/benchmarks/trunk/long/geomod2004.rst 2009-10-21 20:05:55 UTC (rev 15859)
@@ -1,5 +1,3 @@
-.. |times| unicode:: U+00D7
-.. |diffusion-units| replace:: m\ :sup:`2` s\ :sup:`-1`
===========
Geomod 2004
@@ -32,7 +30,7 @@
.. fig:Extension-model-setup
.. figure:: images/Extension_setup.png
:align: center
- :width: 90%
+ :width: 650
Extension model setup. Reproduced, with permission, from Buiter et al.
[Buiter et al Numerical Sandbox]
@@ -49,7 +47,7 @@
.. fig:Comparison-extension
.. figure:: images/Extension_comparision.png
:align: center
- :width: 80%
+ :width: 600
Strain rate invariant for the numerical extension models after 5 cm of
extension. The resolutions of the various models are:
@@ -65,7 +63,7 @@
.. fig:extension-convergence
.. figure:: images/extension_sensitivity.png
:align: center
- :width: 80%
+ :width: 600
Strain rate invariant for the extension model after 5 cm of extension
for four different resolutions: (a) 128 |times| 16, (b) 256 |times| 32,
@@ -90,7 +88,7 @@
.. fig:Shortening-model-setup
.. figure:: images/Shortening_setup.png
:align: center
- :width: 90%
+ :width: 650
Shortening model setup. Reproduced, with permission, from Buiter et al.
[Buiter et al Numerical Sandbox].
@@ -105,7 +103,7 @@
.. fig:shortening-compare
.. figure:: images/Shortening_comparison.png
:align: center
- :width: 80%
+ :width: 600
Strain rate invariant for the numerical shortening models after 14 cm
of shortening. The resolutions of the various models are:
@@ -120,9 +118,12 @@
.. fig:shortening-convergence
.. figure:: images/shortening_sensitivity.png
:align: center
- :width: 80%
+ :width: 600
Strain rate invariant for the shortening model after 14 cm of
shortening for three different resolutions: (a) 128 |times| 32,
(b) 256 |times| 64, (c) 512 |times| 128.
+.. |times| unicode:: U+00D7
+.. |diffusion-units| replace:: m\ :sup:`2` s\ :sup:`-1`
+
Modified: doc/geodynamics.org/benchmarks/trunk/long/geomod2008.html
===================================================================
--- doc/geodynamics.org/benchmarks/trunk/long/geomod2008.html 2009-10-21 20:05:44 UTC (rev 15858)
+++ doc/geodynamics.org/benchmarks/trunk/long/geomod2008.html 2009-10-21 20:05:55 UTC (rev 15859)
@@ -54,7 +54,7 @@
</div>
<!-- fig:Stable_sri -->
<div align="center" class="figure">
-<img alt="images/Stable_wedge_sri.png" src="images/Stable_wedge_sri.png" style="width: 80%;" />
+<img alt="images/Stable_wedge_sri.png" src="images/Stable_wedge_sri.png" style="width: 600px;" />
<p class="caption">Strain rate invariant for the stable wedge benchmark within the wedge.
Outside the wedge, the strain rates are large because of the air's low
viscosity. The resolution is 512 × 128, and the wedge has translated
@@ -62,7 +62,7 @@
</div>
<!-- fig:Stable_particles -->
<div align="center" class="figure">
-<img alt="images/Stable_wedge_particles.png" src="images/Stable_wedge_particles.png" style="width: 80%;" />
+<img alt="images/Stable_wedge_particles.png" src="images/Stable_wedge_particles.png" style="width: 600px;" />
<p class="caption">Material particles for the stable wedge benchmark. The deformation at
the tip is caused by a finite boundary cohesion, although the actual
structure is not resolved. The resolution is 512 × 128, and the
@@ -70,7 +70,7 @@
</div>
<!-- fig:Stable_unstable -->
<div align="center" class="figure">
-<img alt="images/Stable_wedge_unstable.png" src="images/Stable_wedge_unstable.png" style="width: 80%;" />
+<img alt="images/Stable_wedge_unstable.png" src="images/Stable_wedge_unstable.png" style="width: 600px;" />
<p class="caption">Strain rate invariant and velocity arrows for the stable wedge
benchmark, but with the friction angle reduced to 1°. Note that
the strain rates are much higher than in Figure [fig:Stable_sri]. The
@@ -99,42 +99,42 @@
</div>
<!-- fig:unstable_sri_128 -->
<div align="center" class="figure">
-<img alt="images/Geomod2008_unstable_sri128x32.png" src="images/Geomod2008_unstable_sri128x32.png" style="width: 80%;" />
+<img alt="images/Geomod2008_unstable_sri128x32.png" src="images/Geomod2008_unstable_sri128x32.png" style="width: 600px;" />
<p class="caption">Strain rate invariant for the unstable shortening benchmark with a
resolution of 128 × 32. The snapshots are taken
at 0, 2.5, 5, 7.5, and 10 cm of shortening.</p>
</div>
<!-- fig:unstable_sri_256 -->
<div align="center" class="figure">
-<img alt="images/Geomod2008_unstable_sri256x64.png" src="images/Geomod2008_unstable_sri256x64.png" style="width: 80%;" />
+<img alt="images/Geomod2008_unstable_sri256x64.png" src="images/Geomod2008_unstable_sri256x64.png" style="width: 600px;" />
<p class="caption">Strain rate invariant for the unstable shortening benchmark with a
resolution of 256 × 64. The snapshots are taken
at 0, 2.5, 5, 7.5, and 10 cm of shortening.</p>
</div>
<!-- fig:unstable_sri_512 -->
<div align="center" class="figure">
-<img alt="images/Geomod2008_unstable_sri512x128.png" src="images/Geomod2008_unstable_sri512x128.png" style="width: 80%;" />
+<img alt="images/Geomod2008_unstable_sri512x128.png" src="images/Geomod2008_unstable_sri512x128.png" style="width: 600px;" />
<p class="caption">Strain rate invariant for the unstable shortening benchmark with a
resolution of 512 × 128. The snapshots are taken
at 0, 2.5, 5, 7.5, and 10 cm of shortening.</p>
</div>
<!-- fig:unstable_particles_128 -->
<div align="center" class="figure">
-<img alt="images/Geomod2008_unstable_particles128x32.png" src="images/Geomod2008_unstable_particles128x32.png" style="width: 80%;" />
+<img alt="images/Geomod2008_unstable_particles128x32.png" src="images/Geomod2008_unstable_particles128x32.png" style="width: 600px;" />
<p class="caption">Material particles for the unstable shortening benchmark with a
resolution of 128 × 32. The snapshots are taken
at 0, 2.5, 5, 7.5, and 10 cm of shortening.</p>
</div>
<!-- fig:unstable_particles_256 -->
<div align="center" class="figure">
-<img alt="images/Geomod2008_unstable_particles256x64.png" src="images/Geomod2008_unstable_particles256x64.png" style="width: 80%;" />
+<img alt="images/Geomod2008_unstable_particles256x64.png" src="images/Geomod2008_unstable_particles256x64.png" style="width: 600px;" />
<p class="caption">Material particles for the unstable shortening benchmark with a
resolution of 256 × 64. The snapshots are taken
at 0, 2.5, 5, 7.5, and 10 cm of shortening.</p>
</div>
<!-- fig:unstable_particles_512 -->
<div align="center" class="figure">
-<img alt="images/Geomod2008_unstable_particles512x128.png" src="images/Geomod2008_unstable_particles512x128.png" style="width: 80%;" />
+<img alt="images/Geomod2008_unstable_particles512x128.png" src="images/Geomod2008_unstable_particles512x128.png" style="width: 600px;" />
<p class="caption">Material particles for the unstable shortening benchmark with a
resolution of 512 × 128. The snapshots are taken
at 0, 2.5, 5, 7.5, and 10 cm of shortening.</p>
@@ -162,42 +162,42 @@
</div>
<!-- fig:brittle_sri_128 -->
<div align="center" class="figure">
-<img alt="images/Geomod2008_brittle_sri128x32.png" src="images/Geomod2008_brittle_sri128x32.png" style="width: 80%;" />
+<img alt="images/Geomod2008_brittle_sri128x32.png" src="images/Geomod2008_brittle_sri128x32.png" style="width: 600px;" />
<p class="caption">Strain rate invariant for the brittle shortening benchmark with a
resolution of 128 × 32. The snapshots are taken
at 0, 2.5, 5, 7.5, and 10 cm of shortening.</p>
</div>
<!-- fig:brittle_sri_256 -->
<div align="center" class="figure">
-<img alt="images/Geomod2008_brittle_sri256x64.png" src="images/Geomod2008_brittle_sri256x64.png" style="width: 80%;" />
+<img alt="images/Geomod2008_brittle_sri256x64.png" src="images/Geomod2008_brittle_sri256x64.png" style="width: 600px;" />
<p class="caption">Strain rate invariant for the brittle shortening benchmark with a
resolution of 256 × 64. The snapshots are taken
at 0, 2.5, 5, 7.5, and 10 cm of shortening.</p>
</div>
<!-- fig:brittle_sri_512 -->
<div align="center" class="figure">
-<img alt="images/Geomod2008_brittle_sri512x128.png" src="images/Geomod2008_brittle_sri512x128.png" style="width: 80%;" />
+<img alt="images/Geomod2008_brittle_sri512x128.png" src="images/Geomod2008_brittle_sri512x128.png" style="width: 600px;" />
<p class="caption">Strain rate invariant for the brittle shortening benchmark with a
resolution of 512 × 128. The snapshots are taken
at 0, 2.5, 5, 7.5, and 10 cm of shortening.</p>
</div>
<!-- fig:brittle_particles_128 -->
<div align="center" class="figure">
-<img alt="images/Geomod2008_brittle_particles128x32.png" src="images/Geomod2008_brittle_particles128x32.png" style="width: 80%;" />
+<img alt="images/Geomod2008_brittle_particles128x32.png" src="images/Geomod2008_brittle_particles128x32.png" style="width: 600px;" />
<p class="caption">Material particles for the brittle shortening benchmark with a
resolution of 128 × 32. The snapshots are taken
at 0, 2.5, 5, 7.5, and 10 cm of shortening.</p>
</div>
<!-- fig:brittle_particles_256 -->
<div align="center" class="figure">
-<img alt="images/Geomod2008_brittle_particles256x64.png" src="images/Geomod2008_brittle_particles256x64.png" style="width: 80%;" />
+<img alt="images/Geomod2008_brittle_particles256x64.png" src="images/Geomod2008_brittle_particles256x64.png" style="width: 600px;" />
<p class="caption">Material particles for the brittle shortening benchmark with a
resolution of 256 × 64. The snapshots are taken
at 0, 2.5, 5, 7.5, and 10 cm of shortening.</p>
</div>
<!-- fig:brittle_particles_512 -->
<div align="center" class="figure">
-<img alt="images/Geomod2008_brittle_particles512x128.png" src="images/Geomod2008_brittle_particles512x128.png" style="width: 80%;" />
+<img alt="images/Geomod2008_brittle_particles512x128.png" src="images/Geomod2008_brittle_particles512x128.png" style="width: 600px;" />
<p class="caption">Material particles for the brittle shortening benchmark with a
resolution of 512 × 128. The snapshots are taken
at 0, 2.5, 5, 7.5, and 10 cm of shortening.</p>
Modified: doc/geodynamics.org/benchmarks/trunk/long/geomod2008.rst
===================================================================
--- doc/geodynamics.org/benchmarks/trunk/long/geomod2008.rst 2009-10-21 20:05:44 UTC (rev 15858)
+++ doc/geodynamics.org/benchmarks/trunk/long/geomod2008.rst 2009-10-21 20:05:55 UTC (rev 15859)
@@ -55,7 +55,7 @@
.. fig:Stable_sri
.. figure:: images/Stable_wedge_sri.png
:align: center
- :width: 80%
+ :width: 600
Strain rate invariant for the stable wedge benchmark within the wedge.
Outside the wedge, the strain rates are large because of the air's low
@@ -66,7 +66,7 @@
.. fig:Stable_particles
.. figure:: images/Stable_wedge_particles.png
:align: center
- :width: 80%
+ :width: 600
Material particles for the stable wedge benchmark. The deformation at
the tip is caused by a finite boundary cohesion, although the actual
@@ -76,7 +76,7 @@
.. fig:Stable_unstable
.. figure:: images/Stable_wedge_unstable.png
:align: center
- :width: 80%
+ :width: 600
Strain rate invariant and velocity arrows for the stable wedge
benchmark, but with the friction angle reduced to 1\ |deg|. Note that
@@ -111,7 +111,7 @@
.. fig:unstable_sri_128
.. figure:: images/Geomod2008_unstable_sri128x32.png
:align: center
- :width: 80%
+ :width: 600
Strain rate invariant for the unstable shortening benchmark with a
resolution of 128 |times| 32. The snapshots are taken
@@ -120,7 +120,7 @@
.. fig:unstable_sri_256
.. figure:: images/Geomod2008_unstable_sri256x64.png
:align: center
- :width: 80%
+ :width: 600
Strain rate invariant for the unstable shortening benchmark with a
resolution of 256 |times| 64. The snapshots are taken
@@ -129,7 +129,7 @@
.. fig:unstable_sri_512
.. figure:: images/Geomod2008_unstable_sri512x128.png
:align: center
- :width: 80%
+ :width: 600
Strain rate invariant for the unstable shortening benchmark with a
resolution of 512 |times| 128. The snapshots are taken
@@ -138,7 +138,7 @@
.. fig:unstable_particles_128
.. figure:: images/Geomod2008_unstable_particles128x32.png
:align: center
- :width: 80%
+ :width: 600
Material particles for the unstable shortening benchmark with a
resolution of 128 |times| 32. The snapshots are taken
@@ -147,7 +147,7 @@
.. fig:unstable_particles_256
.. figure:: images/Geomod2008_unstable_particles256x64.png
:align: center
- :width: 80%
+ :width: 600
Material particles for the unstable shortening benchmark with a
resolution of 256 |times| 64. The snapshots are taken
@@ -156,7 +156,7 @@
.. fig:unstable_particles_512
.. figure:: images/Geomod2008_unstable_particles512x128.png
:align: center
- :width: 80%
+ :width: 600
Material particles for the unstable shortening benchmark with a
resolution of 512 |times| 128. The snapshots are taken
@@ -189,7 +189,7 @@
.. fig:brittle_sri_128
.. figure:: images/Geomod2008_brittle_sri128x32.png
:align: center
- :width: 80%
+ :width: 600
Strain rate invariant for the brittle shortening benchmark with a
resolution of 128 |times| 32. The snapshots are taken
@@ -198,7 +198,7 @@
.. fig:brittle_sri_256
.. figure:: images/Geomod2008_brittle_sri256x64.png
:align: center
- :width: 80%
+ :width: 600
Strain rate invariant for the brittle shortening benchmark with a
resolution of 256 |times| 64. The snapshots are taken
@@ -207,7 +207,7 @@
.. fig:brittle_sri_512
.. figure:: images/Geomod2008_brittle_sri512x128.png
:align: center
- :width: 80%
+ :width: 600
Strain rate invariant for the brittle shortening benchmark with a
resolution of 512 |times| 128. The snapshots are taken
@@ -216,7 +216,7 @@
.. fig:brittle_particles_128
.. figure:: images/Geomod2008_brittle_particles128x32.png
:align: center
- :width: 80%
+ :width: 600
Material particles for the brittle shortening benchmark with a
resolution of 128 |times| 32. The snapshots are taken
@@ -225,7 +225,7 @@
.. fig:brittle_particles_256
.. figure:: images/Geomod2008_brittle_particles256x64.png
:align: center
- :width: 80%
+ :width: 600
Material particles for the brittle shortening benchmark with a
resolution of 256 |times| 64. The snapshots are taken
@@ -234,7 +234,7 @@
.. fig:brittle_particles_512
.. figure:: images/Geomod2008_brittle_particles512x128.png
:align: center
- :width: 80%
+ :width: 600
Material particles for the brittle shortening benchmark with a
resolution of 512 |times| 128. The snapshots are taken
Modified: doc/geodynamics.org/benchmarks/trunk/long/relaxation-topography.html
===================================================================
--- doc/geodynamics.org/benchmarks/trunk/long/relaxation-topography.html 2009-10-21 20:05:44 UTC (rev 15858)
+++ doc/geodynamics.org/benchmarks/trunk/long/relaxation-topography.html 2009-10-21 20:05:55 UTC (rev 15859)
@@ -32,7 +32,7 @@
simulate half of the wavelength.</p>
<!-- fig:Strain-topo -->
<div align="center" class="figure">
-<img alt="images/Paraview_topography.png" src="images/Paraview_topography.png" style="width: 90%;" />
+<img alt="images/Paraview_topography.png" src="images/Paraview_topography.png" style="width: 350px;" />
<p class="caption">Strain rate and velocities for a sinusoidal topography relaxing
under gravity.</p>
</div>
Modified: doc/geodynamics.org/benchmarks/trunk/long/relaxation-topography.rst
===================================================================
--- doc/geodynamics.org/benchmarks/trunk/long/relaxation-topography.rst 2009-10-21 20:05:44 UTC (rev 15858)
+++ doc/geodynamics.org/benchmarks/trunk/long/relaxation-topography.rst 2009-10-21 20:05:55 UTC (rev 15859)
@@ -27,7 +27,7 @@
.. fig:Strain-topo
.. figure:: images/Paraview_topography.png
:align: center
- :width: 90%
+ :width: 350
Strain rate and velocities for a sinusoidal topography relaxing
under gravity.
Modified: doc/geodynamics.org/benchmarks/trunk/mc/index.html
===================================================================
--- doc/geodynamics.org/benchmarks/trunk/mc/index.html 2009-10-21 20:05:44 UTC (rev 15858)
+++ doc/geodynamics.org/benchmarks/trunk/mc/index.html 2009-10-21 20:05:55 UTC (rev 15859)
@@ -15,17 +15,17 @@
<div class="section" id="d-cartesian-compressible-convection-benchmarks">
<h1>2D Cartesian Compressible Convection Benchmarks</h1>
-<p><a class="reference external" href="2d-cartesian/index.html">General description of the 2D cartesian mantle convection benchmarks</a></p>
+<p><a class="reference external" href="2d-cartesian/index_html">General description of the 2D cartesian mantle convection benchmarks</a></p>
<ul class="simple">
-<li><a class="reference external" href="2d-cartesian/suite1.html">Suite 1</a></li>
-<li><a class="reference external" href="2d-cartesian/suite2.html">Suite 2</a></li>
-<li><a class="reference external" href="2d-cartesian/suite3.html">Suite 3</a></li>
-<li><a class="reference external" href="2d-cartesian/suite4.html">Suite 4</a></li>
+<li><a class="reference external" href="2d-cartesian/suite1">Suite 1</a></li>
+<li><a class="reference external" href="2d-cartesian/suite2">Suite 2</a></li>
+<li><a class="reference external" href="2d-cartesian/suite3">Suite 3</a></li>
+<li><a class="reference external" href="2d-cartesian/suite4">Suite 4</a></li>
</ul>
</div>
<div class="section" id="d-spherical-mantle-convection-benchmarks">
<h1>3D Spherical Mantle Convection Benchmarks</h1>
-<p><a class="reference external" href="3d-spherical/index.html">General description of the 3D spherical mantle convection benchmarks</a></p>
+<p><a class="reference external" href="3d-spherical/index_html">General description of the 3D spherical mantle convection benchmarks</a></p>
<ul class="simple">
<li>BM1{A-H}</li>
<li>BM2{A-H}</li>
Modified: doc/geodynamics.org/benchmarks/trunk/mc/index.rst
===================================================================
--- doc/geodynamics.org/benchmarks/trunk/mc/index.rst 2009-10-21 20:05:44 UTC (rev 15858)
+++ doc/geodynamics.org/benchmarks/trunk/mc/index.rst 2009-10-21 20:05:55 UTC (rev 15859)
@@ -10,18 +10,18 @@
2D Cartesian Compressible Convection Benchmarks
-----------------------------------------------
-`General description of the 2D cartesian mantle convection benchmarks <2d-cartesian/index.html>`_
+`General description of the 2D cartesian mantle convection benchmarks <2d-cartesian/index_html>`_
-* `Suite 1 <2d-cartesian/suite1.html>`_
-* `Suite 2 <2d-cartesian/suite2.html>`_
-* `Suite 3 <2d-cartesian/suite3.html>`_
-* `Suite 4 <2d-cartesian/suite4.html>`_
+* `Suite 1 <2d-cartesian/suite1>`_
+* `Suite 2 <2d-cartesian/suite2>`_
+* `Suite 3 <2d-cartesian/suite3>`_
+* `Suite 4 <2d-cartesian/suite4>`_
3D Spherical Mantle Convection Benchmarks
-----------------------------------------
-`General description of the 3D spherical mantle convection benchmarks <3d-spherical/index.html>`_
+`General description of the 3D spherical mantle convection benchmarks <3d-spherical/index_html>`_
* BM1{A-H}
* BM2{A-H}
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