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Comparing trunk/nonperiodicVSS/nonperiodicVSS.tex (file contents):
Revision 3977 by gezelter, Fri Nov 22 22:27:38 2013 UTC vs.
Revision 3978 by kstocke1, Tue Nov 26 20:33:01 2013 UTC

# Line 89 | Line 89 | boundary between materials.
89   boundary between materials.
90  
91   \begin{figure}
92 < \includegraphics[width=\linewidth]{VSS2}
92 > \includegraphics[width=\linewidth]{figures/VSS}
93   \caption{Schematics of periodic (left) and non-periodic (right)
94    Velocity Shearing and Scaling RNEMD. A kinetic energy or momentum
95    flux is applied from region B to region A. Thermal gradients are
# Line 237 | Line 237 | of rectangular slabs. A temperature profile along the
237   of rectangular slabs. A temperature profile along the $r$ coordinate is created by recording the average temperature of concentric spherical shells.
238  
239   \begin{figure}
240 <        \center{\includegraphics[width=7in]{figures/VSS}}
240 >        \center{\includegraphics[width=7in]{figures/npVSS2}}
241          \caption{Schematics of periodic (left) and nonperiodic (right) Velocity Shearing and Scaling RNEMD. A kinetic energy or momentum flux is applied from region B to region A. Thermal gradients are depicted by a color gradient. Linear or angular velocity gradients are shown as arrows.}
242          \label{fig:VSS}
243   \end{figure}
# Line 427 | Line 427 | Calculated values for the thermal conductivity of a cl
427   \begin{longtable}{ccc}
428   \caption{Caption.}
429   \\ \hline \hline
430 < {Nanoparticle Radius} & {$\boldsymbol \lambda$}\\
431 < {\small(\AA)} & {\small(W m$^{-1}$ K$^{-1}$)}\\ \hline
432 < 20 & 59.66\\
433 < 30 & 57.88\\
434 < 40 & \\
435 < $\infty$ & \\
430 > {Nanoparticle Radius} & $J_r$ & {G}\\
431 > {\small(\AA)} & {\small(kcal fs$^{-1}$ \AA$^{-2}$)}  & {\small(W m$^{-2}$ K$^{-1}$)}\\ \hline
432 > 20 & & 59.66 \\
433 > 30 & & 57.88 \\
434 > 40 & & 37.48 \\
435 > $\infty$ & & 30.2 \\
436   \hline \hline
437 < \label{table:waterconductivity}
437 > \label{table:interfacialconductance}
438   \end{longtable}
439  
440   %%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%

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