commit bb8550a628303aff9d1bed83c638fdca602e5c70
parent 19efac2b0ade7b41c99feab353446eb1e6902c31
Author: Anders Damsgaard <anders@adamsgaard.dk>
Date: Mon, 8 Jul 2019 15:17:21 +0200
Update figures for water compressibility at 0 deg C
Diffstat:
7 files changed, 1 insertion(+), 1 deletion(-)
diff --git a/continuum-granular-manuscript1.tex b/continuum-granular-manuscript1.tex
@@ -230,7 +230,7 @@ For the first experiment with variable water pressure, we apply a water-pressure
% Our model has a representative grain diameter, but tills are polydisperse
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.
+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},
\begin{equation}
d_\text{s}
diff --git a/experiments/fig1.pdf b/experiments/fig1.pdf
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diff --git a/experiments/fig3.pdf b/experiments/fig3.pdf
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diff --git a/experiments/fig4.pdf b/experiments/fig4.pdf
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diff --git a/experiments/fig5.pdf b/experiments/fig5.pdf
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diff --git a/experiments/fig6.pdf b/experiments/fig6.pdf
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