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Comparing trunk/iceWater/iceWater.tex (file contents):
Revision 3967 by gezelter, Wed Oct 23 20:20:29 2013 UTC vs.
Revision 3968 by plouden, Wed Oct 23 23:25:02 2013 UTC

# Line 443 | Line 443 | boundary conditions.
443   \begin{figure}
444   \includegraphics[width=\linewidth]{bComicStrip}
445   \caption{\label{fig:bComic} The basal interface with a shear rate of
446 <  XXXX.  Lower panel: the local tetrahedral order parameter, $q(z)$,
446 >  1.3 ms\textsuperscript{-1}.  Lower panel: the local tetrahedral order parameter, $q(z)$,
447    (black circles) and the hyperbolic tangent fit (red line).  Middle
448    panel: the imposed thermal gradient required to maintain a fixed
449    interfacial temperature.  Upper panel: the transverse velocity
# Line 455 | Line 455 | boundary conditions.
455   \begin{figure}
456   \includegraphics[width=\linewidth]{pComicStrip}
457   \caption{\label{fig:pComic} The prismatic interface with a shear rate
458 <  of XXXX.  Panel
458 >  of 2.0 ms\textsuperscript{-1}.  Panel
459    descriptions match those in figure \ref{fig:bComic}}
460   \end{figure}
461  
# Line 596 | Line 596 | begin to deviate from their bulk liquid values. We fin
596   $\tau_{middle}$, and $\tau_{long}$ at large displacements from the
597   interface. Second, there appears to be a single distance, $d_{basal}$
598   or $d_{prismatic}$, from the interface at which all three decay times
599 < begin to deviate from their bulk liquid values. We find these
600 < distances to be approximately 15~\AA\ and 8~\AA\, respectively,
601 < although significantly finer binning of the $C_2(t)$ data would be
602 < necessary to provide better estimates of a ``dynamic'' interfacial
603 < thickness.
599 > begin to deviate from their bulk liquid values. To quantify this
600 > distance, each of the decay constant $z$-profiles were fit to
601 > \begin{equation}\label{tauFit}
602 > \tau(z)\approx\tau_{liquid}+(\tau_{solid}-\tau_{liquid})e^{-(z-z_{wall})/d}
603 > \end{equation}
604 > where $\tau_{liquid}$ and $\tau_{solid}$ are the liquid and projected
605 > solid values of the decay constants, $z_{wall}$ is the location of the
606 > interface, and $d$ is the displacement the deviations occur at (see
607 > Figures \ref{fig:basal_Tau_comic_strip} and
608 > \ref{fig:prismatic_Tau_comic_strip}). The displacements $d_{basal}$
609 > and $d_{prismatic}$ were determined for each of the three decay
610 > constants, and then averaged for better statistics.
611 > For the basal system, we found $d_{basal}$ for the control set to be
612 > 2.9 \AA\, and 2.8 \AA\ for a simulation with a shear rate of 1.3
613 > ms\textsuperscript{-1}. We found $d_{prismatic}$ to be slightly
614 > larger than $d_{basal}$ for both the control and an applied shear,
615 > with displacements of 3.6 \AA\ for the control system and 3.5 \AA\ for
616 > a simulation with a 2 ms\textsuperscript{-1} shear rate. From this we
617 > can conclude there is no apparent dependence on the shear rate for the dynamic interface
618 > width.
619  
620 + %%%%%%%%Should we keep this paragraph???%%%%%%%%%%%%%%%
621   Beaglehole and Wilson have measured the ice/water interface using
622   ellipsometry and find a thickness of approximately 10~\AA\ for both
623   the basal and prismatic faces.\cite{Beaglehole93} Structurally, we
624   have found the basal and prismatic interfacial width to be
625 < 3.2~$\pm$~0.4~\AA\ and 3.6~$\pm$~0.2~\AA. However, decomposition of
626 < the spatial dependence of the decay times of $C_2(t)$ indicates that a
627 < somewhat thicker interfacial region exists in which the orientational
628 < dynamics of the water molecules begin to resemble the trapped
629 < interfacial water more than the surrounding liquid.
625 > 3.2~$\pm$~0.4~\AA\ and 3.6~$\pm$~0.2~\AA.  Decomposition of
626 > the spatial dependence of the decay times of $C_2(t)$ shows good
627 > agreement with the structural interfacial width determined by the
628 > local tetrahedrality.
629 > %%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
630  
615 Our results indicate that the dynamics of the water molecules within
616 $d_{basal}$ and $d_{prismatic}$ are being significantly perturbed by
617 the interface, even though the structural width of the interface via
618 analysis of the tetrahedrality profile indicates that bulk liquid
619 structure of water is recovered after about 4 \AA\ from the edge of
620 the ice.
631  
632   \subsection{Coefficient of Friction of the Interface}
633   As liquid water flows over an ice interface, there is a distance from
# Line 700 | Line 710 | phase and the prismatic face is reduced by the empty c
710    liquid (dashed red line) intersects the solid phase velocity (solid
711    black line).  The dotted line indicates the location of the ice as
712    determined by the tetrahedrality profile.  This example is taken
713 <  from the basal-face simulation with an applied shear rate of XXXX.}
713 >  from the basal-face simulation with an applied shear rate of 3.0 ms\textsuperscript{-1}.}
714   \end{figure}
715  
716  
# Line 735 | Line 745 | $d_{prismatic}$ to be approximately 15~\AA\ and 8~\AA\
745   proximity to the interface.  There is also an apparent dynamic
746   interface width, $d_{basal}$ and $d_{prismatic}$, at which these
747   deviations from bulk liquid values begin.  We found $d_{basal}$ and
748 < $d_{prismatic}$ to be approximately 15~\AA\ and 8~\AA\ . This implies
749 < that the dynamics of water molecules which have similar structural
750 < environments to liquid phase molecules are dynamically perturbed by
751 < the presence of the ice interface.
748 > $d_{prismatic}$ to be approximately 2.8~\AA\ and 3.5~\AA\ . This
749 > interfacial width is in good agreement with values determined by the
750 > structural analysis of the interface, by the hyperbolic tangent fit of
751 > the local tetrahedral order parameter.
752  
753   The coefficient of liquid-solid friction for each of the facets was
754   also determined. They were found to be

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