manus_continuum_granular1

commit ce244767b430d79e535f17cc90998af6fd0493e7
parent de920fc47d5424b1eb9f229727795c1d8c1039d2
Author: Anders Damsgaard <anders@adamsgaard.dk>
Date:   Mon, 15 Jul 2019 13:46:26 +0200

Add unit to skin depth

Diffstat:
M
continuum-granular-manuscript1.tex
 | 
2
+-

1 file changed, 1 insertion(+), 1 deletion(-)
diff --git a/continuum-granular-manuscript1.tex b/continuum-granular-manuscript1.tex
@@ -289,7 +289,7 @@ The shear velocities during the first cycle ($t<1$ d) is slightly different from
 
 The water pressure variations vary with the same periodocity as the forcing, but with exponential decay in amplitude and increasing lag at depth.
 The skin depth is defined as the distance where the fluctuation amplitude decreases to $1/e$ of its surface value \citep[e.g.][]{Cuffey2010}.
-As long as fluid and diffusion properties are constant, an analytical solution to skin depth $d_\text{s}$ in our system follows the form \citep[after Eq.~4.90 in][]{Turcotte2002},
+As long as fluid and diffusion properties are constant, an analytical solution to skin depth $d_\text{s}$ [m] in our system follows the form \citep[after Eq.~4.90 in][]{Turcotte2002},
 \begin{equation}
 	d_\text{s}
 	= \sqrt{ \frac{D P}{\pi} }