com5SnowSlide: Snow slide
The com5SnowSlide computational module provides the option to add an elastic cohesion force between particles based on com1DFA. This can be used for example to simulate small snow slides.
The cohesion between particles is modeled using elastic bonds with maximum strain rate. This means that the cohesion force \(\mathbf{F}_{lk}\) exerted by \(l\) on \(k\) is expressed by:
Where \(L\) and \(L_0\) are the distances between the particles \(k\) and \(l\) at a time t and at rest (initial time step), \(E\) is the elastic modulus of the material, \(A_{kl}\) is the contact area between particles \(k\) and \(l\) and \(\mathbf{e_{kl}}\) is the unit vector
represents the strain (\(\epsilon\) is positive in the case of elongation and negative in compression). If the strain exceeds a critical value \(\epsilon_c\) the bond between the particles \(k\) and \(l\) breaks.
The contact area \(A_{kl}\) between particles \(k\) and \(l\) reads:
\(h_{kl}\) represents the height of the contact surface and \(d_{kl}\) represents the length of the contact surface in the horizontal plane assuming that each particle has 6 neighbours.
Input
The standard inputs required to perform a simulation run using com1DFA
can be found here: Input.
There is a run script to perform a snow slide com1DFA run: runCom5SnowSlide.py
,
and the configuration settings can be found in com5SnowSlide/com5SnowSlideCfg.ini
.
The snow slide-specific parameters are:
snowSlide is activated by setting
snowSlide
to 1the maximum strain before breaking of the bond
cohesionMaxStrain
the Young modulus in N/m²
cohesiveSurfaceTension
However, also several other parameters, for example the particle initialization method,
friction model and parameters, are changed compared to the default configuration of com1DFA
and listed
in the com5SnowSlide/com5SnowSlideCfg.ini
in the com1DFA_override section.
Please note that the provided default setup for snow slide calculation is defined with the following premises:
slope gradient in the release area from approx. 28° to approx. 50°.
a return level for hazard mapping of 150-yr of snow depth as the initial value.
movement as an intact unit without turbulence
height difference from approx. 30 m to max. 60-80 m
valid for altitude levels > 500 m and < 1,500 m sea level
Initialization of bonds
If the elastic cohesion (snowSlide
set to 1) is activated, the bonds between particles are initialized.
The construction of the bonds is done by building a triangular mesh on the particles
(used as a point cloud) and the Delaunay triangulation function
from matplotlib.
The length \(L_0\) of the bonds at rest (initial distance between two bonded particles) is also initialized here.
Note
It is recommended to use the triangular (triangular
) initialization option (Initialize particles)
rather than the random or the uniform one in the case where cohesion is activated.
To run
first go to
AvaFrame/avaframe
copy
avaframeCfg.ini
tolocal_avaframeCfg.ini
and set your desired avalanche directory namecreate an avalanche directory with required input files - for this task you can use Initialize Project
copy
com5SnowSlide/com5SnowSlideCfg.ini
tocom5SnowSlide/local_com5SnowSlideCfg.ini
and if desired change configuration settingsif you are on a develop installation, make sure you have an updated compilation, see installation:Update AvaFrame
run:
python3 runCom5SnowSlide.py