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
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 (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(-)
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 (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)