--- trunk/iceiPaper/iceiPaper.tex	2004/12/01 17:35:14	1812
+++ trunk/iceiPaper/iceiPaper.tex	2004/12/01 17:44:08	1814
@@ -118,8 +118,8 @@ down the (001) crystal face. The rows of water tetrame
 \begin{figure}
 \includegraphics[width=\linewidth]{orderedIcei.eps}
 \caption{Image of a proton ordered crystal of Ice-{\it i} looking 
-down the (001) crystal face. The rows of water tetramers surrounded by
-octagonal pores leads to a crystal structure that is significantly
+down the (001) crystal face.  The rows of water tetramers surrounded
+by octagonal pores leads to a crystal structure that is significantly
 less dense than ice $I_h$.}
 \label{protOrder}
 \end{figure}
@@ -231,7 +231,7 @@ body-frame {\it z}-axis. $K_\theta$ and $K_\omega$ are
 \caption{Possible orientational motions for a restrained molecule. 
 $\theta$ angles correspond to displacement from the body-frame {\it
 z}-axis, while $\omega$ angles correspond to rotation about the
-body-frame {\it z}-axis. $K_\theta$ and $K_\omega$ are spring
+body-frame {\it z}-axis.  $K_\theta$ and $K_\omega$ are spring
 constants for the harmonic springs restraining motion in the $\theta$
 and $\omega$ directions.}
 \label{waterSpring}
@@ -293,9 +293,9 @@ variety of common water models. All calculations used 
 \begin{center}
 
 \caption{Calculated free energies for several ice polymorphs with a 
-variety of common water models. All calculations used a cutoff radius
-of 9 \AA\ and were performed at 200 K and $\sim$1 atm. Units are
-kcal/mol. Calculated error of the final digits is in parentheses.}
+variety of common water models.  All calculations used a cutoff radius
+of 9 \AA\ and were performed at 200 K and $\sim$1 atm.  Units are
+kcal/mol.  Calculated error of the final digits is in parentheses.}
 
 \begin{tabular}{lcccc}
 \hline 
@@ -406,8 +406,9 @@ with TIP3P using 12 and 13.5 \AA\ cutoff radii were om
 cutoff radius and show some degree of converge at large cutoff radii.
 Inclusion of a long-range correction reduces the cutoff radius
 dependence of the free energy for all the models.  Data for ice I$_c$
-with TIP3P using 12 and 13.5 \AA\ cutoff radii were omitted being that
-the crystal was prone to distortion and melting at 200 K.}
+with TIP3P using both 12 and 13.5 \AA\ cutoffs were omitted because
+the crystal was prone to distortion and melting at 200 K.  Ice-{\it
+i}$^\prime$ is the form of Ice-{\it i} used in the SPC/E simulations.}
 \label{incCutoff}
 \end{figure}