commit c2c9741525cd0077413571d50b6c0bb37404c608 parent bb7a8af6cd52f924f3ac4f732b13066f8b924e47 Author: Anders Damsgaard <anders@adamsgaard.dk> Date: Mon, 16 Dec 2019 18:12:50 +0100 Update caption for skin-depth figure Diffstat:
| M | continuum-granular-manuscript1.tex | | | 6 | ++++-- |
1 file changed, 4 insertions(+), 2 deletions(-)
diff --git a/continuum-granular-manuscript1.tex b/continuum-granular-manuscript1.tex @@ -345,8 +345,10 @@ On the contrary, fine-grained tills are unlikely to undergo deep deformation, bu \begin{center} \includegraphics[width=15cm]{experiments/fig-skin_depth.pdf} \caption{\label{fig:skin_depth}% - Skin depth of pore-pressure fluctuations (Eq.\ 6 in the main text) with forcing frequencies ranging from yearly to hourly periods. - The permeability spans values common for tills \cite{Schwartz2003}. + a) Skin depth of pore-pressure fluctuations (Eq.~\ref{eq:skin_depth}) with forcing frequencies ranging from yearly to hourly periods. + The permeability spans values common for tills \cite{Schwartz2003} + b) Depth of maximum deformation with a water-pressure forcing of $A_\mathrm{f}$ = 10 kPa. + c) Same as (b) but with $A_\mathrm{f}$ = 100 kPa. } \end{center} \end{figure}