manus_continuum_granular1

manuscript files for first continuum-till paper
git clone git://src.adamsgaard.dk/manus_continuum_granular1
Log | Files | Refs

commit 4fc3c4fee99da069042e9cac219bc5cb2222bfb7
parent d11cc47f2f2165b487410373ee5cc7876cafddbb
Author: Anders Damsgaard <anders@adamsgaard.dk>
Date:   Mon,  8 Jul 2019 13:34:53 +0200

Update figures to reflect 1d_fd_simple_shear update

Diffstat:
Mcontinuum-granular-manuscript1.tex | 7+++----
Mexperiments/fig1.pdf | 0
Mexperiments/fig2.pdf | 0
Mexperiments/fig3.pdf | 0
Mexperiments/fig4.pdf | 0
Mexperiments/fig5.pdf | 0
Mexperiments/fig6.pdf | 0
7 files changed, 3 insertions(+), 4 deletions(-)

diff --git a/continuum-granular-manuscript1.tex b/continuum-granular-manuscript1.tex @@ -56,8 +56,8 @@ We show that past pulses in water pressure can transfer shear away from the ice- \subsection{Granular flow}% \label{sub:granular_flow} -We expand a steady-state continuum model for granular flow by \citet{Henann2013} with a coupling to pore-pressure diffusion. -The sediment deforms as a highly nonlinear Bingham material with yield beyond the Mohr-Coulomb failure limit for a cohesionless material. +We expand a steady-state continuum model for granular flow by \citet{Henann2013} with material cohesion and a coupling to pore-pressure diffusion. +The sediment deforms as a highly nonlinear Bingham material with yield beyond the Mohr-Coulomb failure limit. We assume that the elasticity is negligible and set the total shear rate $\dot{\gamma}$ to consist of a plastic contribution $\dot{\gamma}^\text{p}$: \begin{equation} \dot{\gamma} \approx \dot{\gamma}^\text{p} = g(\mu_\text{c}, \sigma_\text{n}') \mu, @@ -66,12 +66,11 @@ We assume that the elasticity is negligible and set the total shear rate $\dot{\ where $\mu = \tau/\sigma_\text{n}'$ is the dimensionless ratio between shear stress ($\tau$ [Pa]) and effective normal stress ($\sigma_\text{n}' = \sigma_\text{n} - p_f$ [Pa]). Water pressure is $p_\text{f}$ [Pa] and $g$ [s$^{-1}$] is the granular fluidity. The fluidity consists of local and non-local components. -We expand the fluidity term in \citet{Henann2013} to account for material cohesion. The local fluidity is defined as: \begin{equation} g_\text{local}(\mu, \sigma_\text{n}') = \begin{cases} - \sqrt{d^2 \sigma_\text{n}' / \rho_\text{s}} ((\mu - C/\sigma_\text{n}' - \mu_\text{s})/(b\mu) &\text{if } \mu - C/\sigma_\text{n}') > \mu_\text{s} \text{, and}\\ + \sqrt{d^2 \sigma_\text{n}' / \rho_\text{s}} ((\mu - C/\sigma_\text{n}') - \mu_\text{s})/(b\mu) &\text{if } \mu - C/\sigma_\text{n}' > \mu_\text{s} \text{, and}\\ 0 &\text{if } \mu - C/\sigma_\text{n}' \leq \mu_\text{s}. \end{cases} \label{eq:g_local} diff --git a/experiments/fig1.pdf b/experiments/fig1.pdf Binary files differ. diff --git a/experiments/fig2.pdf b/experiments/fig2.pdf Binary files differ. diff --git a/experiments/fig3.pdf b/experiments/fig3.pdf Binary files differ. diff --git a/experiments/fig4.pdf b/experiments/fig4.pdf Binary files differ. diff --git a/experiments/fig5.pdf b/experiments/fig5.pdf Binary files differ. diff --git a/experiments/fig6.pdf b/experiments/fig6.pdf Binary files differ.