commit bb7a8af6cd52f924f3ac4f732b13066f8b924e47 parent 70fe90feb583b4e79d193e3bcdb658b1dcfbf891 Author: Anders Damsgaard <anders@adamsgaard.dk> Date: Mon, 16 Dec 2019 18:10:39 +0100 Update reference to SI Text S2 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 @@ -322,7 +322,7 @@ As long as fluid and diffusion properties are constant and the layer is sufficie where $D$ is the hydraulic diffusivity [m$^2$/s] and $P$ [s] is the period of the oscillations. The remaining terms were previously defined. However, as the deformation pattern depends on both hydraulic properties and the forcing amplitude (Fig.~S3), the skin depth alone is insufficient to judge the occurence of deep deformation. -We constrain an analytical solution for diffusive pressure perturbation to find the largest depth $z'$ containing a minimum of effective normal stress over the cause of a pressure-perturbation cycle (see SI Text S1): +We constrain an analytical solution for diffusive pressure perturbation to find the largest depth $z'$ containing a minimum of effective normal stress over the cause of a pressure-perturbation cycle (see Supplementary Information Text S2 for full derivation): \begin{linenomath*} \begin{equation} 0 =