tUpdate paths to figures - cngf-pf - continuum model for granular flows with pore-pressure dynamics (renamed from 1d_fd_simple_shear) (HTM) git clone git://src.adamsgaard.dk/cngf-pf (DIR) Log (DIR) Files (DIR) Refs (DIR) README (DIR) LICENSE --- (DIR) commit ee6d39f13719a5caa467250340c53c2d9e25991c (DIR) parent b4d0fe9bca8b613877734f7e28f87c20aa37b3e8 (HTM) Author: Anders Damsgaard <anders@adamsgaard.dk> Date: Fri, 28 Jun 2019 11:18:39 +0200 Update paths to figures Diffstat: M README.md | 10 +++++----- 1 file changed, 5 insertions(+), 5 deletions(-) --- (DIR) diff --git a/README.md b/README.md t@@ -59,7 +59,7 @@ probably be improved further. | Discrete-element model | Continuum Model | | ----------------------- | --------------- | | Damsgaard et al. 2013 | | -| ![damsgaard2013-fig8.png](https://gitlab.com/admesg/1d_fd_simple_shear/raw/master/damsgaard2013-fig8.png) | ![1d_fd_simple_shear.png](https://gitlab.com/admesg/1d_fd_simple_shear/raw/master/1d_fd_simple_shear.png) | +| ![damsgaard2013-fig8.png](https://gitlab.com/admesg/1d_fd_simple_shear/raw/master/doc/damsgaard2013-fig8.png) | ![1d_fd_simple_shear.png](https://gitlab.com/admesg/1d_fd_simple_shear/raw/master/test/1d_fd_simple_shear.png) | ### Stress and strain rate The rheology is of Bingham type, where no deformation occurs beneath the t@@ -71,15 +71,15 @@ have *b* = 0.94 ([Forterre and Pouliquen | Real material (laboratory or field study) | Continuum Model | | -------------------------------------------- | --------------- | | Upstream-B ([Kamb 1991](https://doi.org/10.1029/91jb00946)): | | -| ![kamb1991-fig1.png](https://gitlab.com/admesg/1d_fd_simple_shear/raw/master/kamb1991-fig1.png) | ![1d_fd_simple_shear_rheology_kamb.png](https://gitlab.com/admesg/1d_fd_simple_shear/raw/master/1d_fd_simple_shear_rheology_kamb.png) | +| ![kamb1991-fig1.png](https://gitlab.com/admesg/1d_fd_simple_shear/raw/master/doc/kamb1991-fig1.png) | ![1d_fd_simple_shear_rheology_kamb.png](https://gitlab.com/admesg/1d_fd_simple_shear/raw/master/test/1d_fd_simple_shear_rheology_kamb.png) | | Various subglacial tills ([Iverson 2010](https://doi.org/10.3189/002214311796406220)): | | -| ![iverson2010-fig2a.png](https://gitlab.com/admesg/1d_fd_simple_shear/raw/master/iverson2010-fig2a.png) | ![1d_fd_simple_shear_rheology_iverson.png](https://gitlab.com/admesg/1d_fd_simple_shear/raw/master/1d_fd_simple_shear_rheology_iverson.png) | +| ![iverson2010-fig2a.png](https://gitlab.com/admesg/1d_fd_simple_shear/raw/master/doc/iverson2010-fig2a.png) | ![1d_fd_simple_shear_rheology_iverson.png](https://gitlab.com/admesg/1d_fd_simple_shear/raw/master/test/1d_fd_simple_shear_rheology_iverson.png) | | Whillans Ice Plain ([Tulaczyk 2006](https://doi.org/10.3189/172756506781828601)): | | -| ![tulaczyk2006-fig1.png](https://gitlab.com/admesg/1d_fd_simple_shear/raw/master/tulaczyk2006-fig1.png) | ![1d_fd_simple_shear_rheology_tulaczyk.png](https://gitlab.com/admesg/1d_fd_simple_shear/raw/master/1d_fd_simple_shear_rheology_tulaczyk.png) | +| ![tulaczyk2006-fig1.png](https://gitlab.com/admesg/1d_fd_simple_shear/raw/master/doc/tulaczyk2006-fig1.png) | ![1d_fd_simple_shear_rheology_tulaczyk.png](https://gitlab.com/admesg/1d_fd_simple_shear/raw/master/test/1d_fd_simple_shear_rheology_tulaczyk.png) | ### Variable water pressure The model is expanded from the Henann and Kamrin 2013 model by including a diffusive porewater pressure parameterization. Below is an example of diurnal water-pressure variations that gradually propagate into the bed. -![diurnal.gif](https://gitlab.com/admesg/1d_fd_simple_shear/raw/master/diurnal.gif) +![diurnal.gif](https://gitlab.com/admesg/1d_fd_simple_shear/raw/master/test/diurnal.gif)