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\documentclass{pnastwo} |
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%% ADDITIONAL OPTIONAL STYLE FILES Font specification |
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%\usepackage{PNASTWOF} |
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\usepackage[version=3]{mhchem} |
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\usepackage[round,numbers,sort&compress]{natbib} |
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\usepackage{fixltx2e} |
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\usepackage{booktabs} |
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\usepackage{multirow} |
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\bibpunct{(}{)}{,}{n}{,}{,} |
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\bibliographystyle{pnas2011} |
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\begin{document} |
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|
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%S1-S4 are the z-rnemd profiles |
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\begin{figure} |
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\includegraphics[width=\linewidth]{Pyr_comic_strip} |
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\caption{\label{fig:pyrComic} Properties of the pyramidal interface |
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being sheared through water at 3.8 ms\textsuperscript{-1}. Lower |
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panel: the local tetrahedral order parameter, $q(z)$, (circles) and |
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the hyperbolic tangent fit (turquoise line). Middle panel: the |
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imposed thermal gradient required to maintain a fixed interfacial |
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temperature of 225 K. Upper panel: the transverse velocity gradient |
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that develops in response to an imposed momentum flux. The vertical |
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dotted lines indicate the locations of the midpoints of the two |
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interfaces.} |
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\end{figure} |
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|
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\begin{figure} |
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\includegraphics[width=\linewidth]{SP_comic_strip} |
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\caption{\label{fig:spComic} The secondary prism interface with a shear |
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rate of 3.5 \ |
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ms\textsuperscript{-1}. Panel descriptions match those in figure \ref{fig:pyrComic}.} |
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\end{figure} |
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|
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\begin{figure} |
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\includegraphics[width=\linewidth]{bComicStrip} |
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\caption{\label{fig:spComic} The basal interface with a shear |
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rate of 1.3 \ |
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ms\textsuperscript{-1}. Panel descriptions match those in figure \ref{fig:pyrComic}.} |
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\end{figure} |
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|
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\begin{figure} |
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\includegraphics[width=\linewidth]{pComicStrip} |
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\caption{\label{fig:spComic} The prismatic interface with a shear |
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rate of 2 \ |
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ms\textsuperscript{-1}. Panel descriptions match those in figure \ref{fig:pyrComic}.} |
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\end{figure} |
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|
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%Figures S5-S8 are the z-orientation times |
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\begin{figure} |
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\includegraphics[width=\linewidth]{Pyr-orient} |
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\caption{\label{fig:PyrOrient} The three decay constants of the |
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orientational time correlation function, $C_2(z,t)$, for water as a |
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function of distance from the center of the ice slab. The vertical |
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dashed line indicates the edge of the pyramidal ice slab determined |
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by the local order tetrahedral parameter. The control (circles) and |
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sheared (squares) simulations were fit using shifted-exponential |
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decay (see Eq. 9 in Ref. \citealp{Louden13}).} |
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\end{figure} |
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|
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\begin{figure} |
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\includegraphics[width=\linewidth]{SP-orient} |
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\caption{\label{fig:SPorient} Decay constants for $C_2(z,t)$ at the secondary |
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prism face. Panel descriptions match those in \ref{fig:PyrOrient}.} |
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\end{figure} |
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|
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|
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\begin{figure} |
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\includegraphics[width=\linewidth]{basal_Tau_comic_strip} |
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\caption{\label{fig:SPorient} Decay constants for $C_2(z,t)$ at the basal face. Panel descriptions match those in \ref{fig:PyrOrient}.} |
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\end{figure} |
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|
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\begin{figure} |
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\includegraphics[width=\linewidth]{prismatic_Tau_comic_strip} |
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\caption{\label{fig:SPorient} Decay constants for $C_2(z,t)$ at the |
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prismatic face. Panel descriptions match those in \ref{fig:PyrOrient}.} |
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\end{figure} |
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|
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\end{document} |