[cig-commits] commit: Reverting back equation, description to latex format.
Mercurial
hg at geodynamics.org
Tue Mar 23 10:36:01 PDT 2010
changeset: 830:c731a9489a82
branch: 1.4.x
tag: 1.4.0
parent: 814:847af1136f99
user: JericoRevote
date: Tue Feb 02 14:46:17 2010 +1100
files: Rheology/src/Arrhenius.meta Rheology/src/DepthDependentViscosity.meta Rheology/src/Director.meta Rheology/src/DruckerPrager.meta Rheology/src/FrankKamenetskii.meta Rheology/src/MultiRheologyMaterial.meta Rheology/src/NonNewtonian.meta Rheology/src/StrainWeakening.meta Rheology/src/VonMises.meta
description:
Reverting back equation, description to latex format.
diff -r 847af1136f99 -r c731a9489a82 Rheology/src/Arrhenius.meta
--- a/Rheology/src/Arrhenius.meta Wed Jan 20 12:29:35 2010 +1100
+++ b/Rheology/src/Arrhenius.meta Tue Feb 02 14:46:17 2010 +1100
@@ -14,7 +14,7 @@
<param name="Reference">...</param>
<param name="Summary">...</param>
<param name="Description">A temperature dependent rheology.</param>
- <param name="Equation">$\eta = \eta_0 \exp \\left( \frac {E + V d} {T + T_0} \right)$</param>
+ <param name="Equation">$\eta = \eta_0 \exp \left( \frac {E + V d} {T + T_0} \right)$</param>
<!--Now the interesting stuff-->
<list name="Params">
diff -r 847af1136f99 -r c731a9489a82 Rheology/src/DepthDependentViscosity.meta
--- a/Rheology/src/DepthDependentViscosity.meta Wed Jan 20 12:29:35 2010 +1100
+++ b/Rheology/src/DepthDependentViscosity.meta Tue Feb 02 14:46:17 2010 +1100
@@ -14,7 +14,7 @@
<param name="Reference">...</param>
<param name="Summary">...</param>
<param name="Description">A rheology that varies exponentially in one direction.</param>
- <param name="Equation">$\eta = \eta_0 \exp \\left( \\gamma ( y - y_0 ) \right)$</param>
+ <param name="Equation">$\eta = \eta_0 \exp \left( \gamma ( y - y_0 ) \right)$</param>
<!--Now the interesting stuff-->
<list name="Params">
@@ -34,7 +34,7 @@
<param name="Name">gamma</param>
<param name="Type">Double</param>
<param name="Default">0.0</param>
- <param name="Description">This is the $\\gamma$ in the equation above.</param>
+ <param name="Description">This is the $\gamma$ in the equation above.</param>
</struct>
<struct>
<param name="Name">referencePoint</param>
diff -r 847af1136f99 -r c731a9489a82 Rheology/src/Director.meta
--- a/Rheology/src/Director.meta Wed Jan 20 12:29:35 2010 +1100
+++ b/Rheology/src/Director.meta Tue Feb 02 14:46:17 2010 +1100
@@ -14,7 +14,7 @@
<param name="Reference">...</param>
<param name="Summary">...</param>
<param name="Description">This component allows to add a vector to a material points and to update it with respect to the deformation.</param>
- <param name="Equation">Director Evolution Equation: $\\dot n_i = -L_{ji} n_j, n_i \rightarrow \frac{n_i}{|n|}$</param>
+ <param name="Equation">Director Evolution Equation: $\dot n_i = -L_{ji} n_j, n_i \rightarrow \frac{n_i}{|n|}$</param>
<!--Now the interesting stuff-->
<list name="Params">
diff -r 847af1136f99 -r c731a9489a82 Rheology/src/DruckerPrager.meta
--- a/Rheology/src/DruckerPrager.meta Wed Jan 20 12:29:35 2010 +1100
+++ b/Rheology/src/DruckerPrager.meta Tue Feb 02 14:46:17 2010 +1100
@@ -14,7 +14,7 @@
<param name="Reference">...</param>
<param name="Summary">...</param>
<param name="Description">Implements a Drucker-Prager yield Rheology. The parameters of this criterion are calibrated so that the yield surface coincides with the Mohr Coulomb one for the condition of a compression test. </param>
- <param name="Equation">Yield Surface: $f = \\sqrt{3} \bar{\tau} - \alpha p - k \\le 0, \alpha = \frac{6 \\sin\varphi}{3 - \\sin\varphi}, k = \frac{6 c \\cos\varphi}{3 - \\sin\varphi}$</param>
+ <param name="Equation">Yield Surface: $f = \sqrt{3} \bar{\tau} - \alpha p - k \le 0, \alpha = \frac{6 \sin\varphi}{3 - \sin\varphi}, k = \frac{6 c \cos\varphi}{3 - \sin\varphi}$</param>
<!--Now the interesting stuff-->
diff -r 847af1136f99 -r c731a9489a82 Rheology/src/FrankKamenetskii.meta
--- a/Rheology/src/FrankKamenetskii.meta Wed Jan 20 12:29:35 2010 +1100
+++ b/Rheology/src/FrankKamenetskii.meta Tue Feb 02 14:46:17 2010 +1100
@@ -14,7 +14,7 @@
<param name="Reference">...</param>
<param name="Summary">...</param>
<param name="Description">An approximation to the Arrhenius temperature dependent rheology.</param>
- <param name="Equation">$\eta = \eta_0 \exp\\left(-\theta T\right)$</param>
+ <param name="Equation">$\eta = \eta_0 \exp\left(-\theta T\right)$</param>
<!--Now the interesting stuff-->
diff -r 847af1136f99 -r c731a9489a82 Rheology/src/MultiRheologyMaterial.meta
--- a/Rheology/src/MultiRheologyMaterial.meta Wed Jan 20 12:29:35 2010 +1100
+++ b/Rheology/src/MultiRheologyMaterial.meta Tue Feb 02 14:46:17 2010 +1100
@@ -13,7 +13,7 @@
<param name="Parent">RheologyMaterial</param>
<param name="Reference">...</param>
<param name="Summary">...</param>
- <param name="Description">This allows for multiple rheologies to be applied to a material. The resultant isotropic material will have a effective viscosity defined as $\frac{1}{n_{eff}} = \\sum_{i=0}^n \frac{1}{n_{i}}$, where $n_i$ is the isotropic vicosities of the input rheologies. <br/><br/>
+ <param name="Description">This allows for multiple rheologies to be applied to a material. The resultant isotropic material will have a effective viscosity defined as $\frac{1}{n_{eff}} = \sum_{i=0}^n \frac{1}{n_{i}}$, where $n_i$ is the isotropic vicosities of the input rheologies. <br/><br/>
The input rheologies must be defined in a rheology list, see example</param>
<list name="Params">
diff -r 847af1136f99 -r c731a9489a82 Rheology/src/NonNewtonian.meta
--- a/Rheology/src/NonNewtonian.meta Wed Jan 20 12:29:35 2010 +1100
+++ b/Rheology/src/NonNewtonian.meta Tue Feb 02 14:46:17 2010 +1100
@@ -14,7 +14,7 @@
<param name="Reference">...</param>
<param name="Summary">...</param>
<param name="Description">Models rheology with dislocation creep (non-Newtonian Stress Dependent viscosity)</param>
- <param name="Equation">Constitutive Equation: $\eta = \eta_{0} \tau^{1-n}$.\\* How this is implemented in the code: $\eta = (2\\dot\epsilon)^\frac{1-n}{n} \eta_{0}^\frac{1}{n}$</param>
+ <param name="Equation">Constitutive Equation: $\eta = \eta_{0} \tau^{1-n}$.\* How this is implemented in the code: $\eta = (2\dot\epsilon)^\frac{1-n}{n} \eta_{0}^\frac{1}{n}$</param>
<!--Now the interesting stuff-->
<list name="Params">
@@ -31,7 +31,7 @@
<param name="Essential">True</param>
<param name="Name">StrainRateInvariantField</param>
<param name="Type">FeVariable</param>
- <param name="Description">The field that provides the $\\dot\epsilon$ in the equation above.</param>
+ <param name="Description">The field that provides the $\dot\epsilon$ in the equation above.</param>
</struct>
</list>
diff -r 847af1136f99 -r c731a9489a82 Rheology/src/StrainWeakening.meta
--- a/Rheology/src/StrainWeakening.meta Wed Jan 20 12:29:35 2010 +1100
+++ b/Rheology/src/StrainWeakening.meta Tue Feb 02 14:46:17 2010 +1100
@@ -42,7 +42,7 @@
<param name="Type">Double</param>
<param name="Default">-1.0</param>
<param name="Description">This parameter is used to set the way the initial randomly oriented damage is distributed in space
- $\\phi = \\cos^2 k_I x_I$. The way the damage evolves often makes it a good idea to keep shear bands away from boundaries,
+ $\phi = \cos^2 k_I x_I$. The way the damage evolves often makes it a good idea to keep shear bands away from boundaries,
especially where the mesh-stretching boundary condition is applied. In this case, make sure $k_I = n / L_I$ where $n$ is
an integer, and $L_I$ is the length of the box in the $I$ direction.</param>
</struct>
@@ -51,7 +51,7 @@
<param name="Type">Double</param>
<param name="Default">-1.0</param>
<param name="Description">This parameter is used to set the way the initial randomly oriented damage is distributed in space
- $\\phi = \\sin^2 k_I x_I$. The way the damage evolves often makes it a good idea to keep shear bands away from boundaries,
+ $\phi = \sin^2 k_I x_I$. The way the damage evolves often makes it a good idea to keep shear bands away from boundaries,
especially where the mesh-stretching boundary condition is applied. In this case, make sure $k_I = n / L_I$ where $n$ is
an integer, and $L_I$ is the length of the box in the $I$ direction.</param>
</struct>
@@ -60,7 +60,7 @@
<param name="Type">Double</param>
<param name="Default">-1.0</param>
<param name="Description">This parameter is used to set the way the initial randomly oriented damage is distributed in space
- $\\phi = \\cos^2 k_I x_I$. The way the damage evolves often makes it a good idea to keep shear bands away from boundaries,
+ $\phi = \cos^2 k_I x_I$. The way the damage evolves often makes it a good idea to keep shear bands away from boundaries,
especially where the mesh-stretching boundary condition is applied. In this case, make sure $k_I = n / L_I$ where $n$ is
an integer, and $L_I$ is the length of the box in the $I$ direction.</param>
</struct>
@@ -69,7 +69,7 @@
<param name="Type">Double</param>
<param name="Default">-1.0</param>
<param name="Description">>This parameter is used to set the way the initial randomly oriented damage is distributed in space
- $\\phi = \\sin^2 k_K x_K$. The way the damage evolves often makes it a good idea to keep shear bands away from boundaries,
+ $\phi = \sin^2 k_K x_K$. The way the damage evolves often makes it a good idea to keep shear bands away from boundaries,
especially where the mesh-stretching boundary condition is applied. In this case, make sure $k_K = n / L_K$ where $n$ is
an integer, and $L_K$ is the length of the box in the $K$ direction.</param>
</struct>
@@ -78,7 +78,7 @@
<param name="Type">Double</param>
<param name="Default">-1.0</param>
<param name="Description">This parameter is used to set the way the initial randomly oriented damage is distributed in space
- $\\phi = \\cos^2 k_K x_K$. The way the damage evolves often makes it a good idea to keep shear bands away from boundaries,
+ $\phi = \cos^2 k_K x_K$. The way the damage evolves often makes it a good idea to keep shear bands away from boundaries,
especially where the mesh-stretching boundary condition is applied. In this case, make sure $k_K = n / L_K$ where $n$ is
an integer, and $L_K$ is the length of the box in the $K$ direction.</param>
</struct>
diff -r 847af1136f99 -r c731a9489a82 Rheology/src/VonMises.meta
--- a/Rheology/src/VonMises.meta Wed Jan 20 12:29:35 2010 +1100
+++ b/Rheology/src/VonMises.meta Tue Feb 02 14:46:17 2010 +1100
@@ -43,7 +43,7 @@
<param name="Essential">True</param>
<param name="Name">StrainRateField</param>
<param name="Type">FeVariable</param>
- <param name="Description">The field that provides the $\\dot\epsilon$ in the equation above.</param>
+ <param name="Description">The field that provides the $\dot\epsilon$ in the equation above.</param>
</struct>
</list>
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