aboutsummaryrefslogtreecommitdiff
path: root/doc
diff options
context:
space:
mode:
authorbmundim <bmundim@c83d129a-5a75-4d5a-9c4d-ed3a5855bf45>2012-05-18 05:17:13 +0000
committerbmundim <bmundim@c83d129a-5a75-4d5a-9c4d-ed3a5855bf45>2012-05-18 05:17:13 +0000
commit38c73944d2e4cd7a22261278313274791b076848 (patch)
tree3f5ee2faa57e3b5f7a9f775d2ba389f46e90d665 /doc
parent9eaaeff77102591f18987eacc3fdc0ac5583d1cf (diff)
Correct S_i conserved variable index.
git-svn-id: http://svn.einsteintoolkit.org/cactus/EinsteinEvolve/GRHydro/trunk@338 c83d129a-5a75-4d5a-9c4d-ed3a5855bf45
Diffstat (limited to 'doc')
-rw-r--r--doc/documentation.tex8
1 files changed, 4 insertions, 4 deletions
diff --git a/doc/documentation.tex b/doc/documentation.tex
index 9387fbf..b6f3ff9 100644
--- a/doc/documentation.tex
+++ b/doc/documentation.tex
@@ -308,8 +308,8 @@ the flux conservative form
where ${\bf q}$ is a set of {\it conserved variables}, ${\bf f}^{(i)}
({\bf q})$ the fluxes and ${\bf s} ({\bf q})$ the source
terms.
-The five conserved variables are labeled $D$, $S^i$, and $\tau$, where
-$D$ is the generalized particle number density, $S^i$ are the generalized
+The five conserved variables are labeled $D$, $S_i$, and $\tau$, where
+$D$ is the generalized particle number density, $S_i$ are the generalized
momenta in each direction, and $\tau$ is an internal energy term.
These conserved variables are composed from a set of {\it primitive variables},
which are $\rho$, the rest-mass density, $p$, the
@@ -334,7 +334,7 @@ energy, and $W$, the Lorentz factor, via the following relations
\begin{eqnarray}
\label{eq:prim2con}
D &=& \sqrt{\gamma}W\rho \nonumber \\
- S^i &=& \sqrt{\gamma} \rho h W^2 v^i \nonumber \\
+ S_i &=& \sqrt{\gamma} \rho h W^2 v_i \nonumber \\
\tau &=& \sqrt{\gamma}\left( \rho h W^2 - p\right) - D,
\end{eqnarray}
where $\gamma$ is the determinant of the spatial 3-metric $\gamma_{ij}$ and
@@ -1796,7 +1796,7 @@ used in three separate places. These are
attempt is made to convert to primitive variables. If the iterative
algorithm returns a negative (and hence unphysical) value of $\rho$,
then $\rho$ is reset to the atmosphere value, the velocities are set
- to zero, and $P$, $\epsilon$, $S^i$ and $\tau$ are reset to be
+ to zero, and $P$, $\epsilon$, $S_i$ and $\tau$ are reset to be
consistent with $\rho$ (and $D$). Note that even though the
polytropic equation of state gives us sufficient information to
calculate a consistent value of $D$, this is not done.