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(Created page with "= Avalanches and BGW process= = Fully connected model foor the cellular automata (mean field)= Let's study the mean field version of the cellular automata introduced in the previous lecture. * The elastic coupling is with all neighbours <center><math> \sigma_i= h_{CM} - h_i + m^2(w-h_i), \quad </math></center>. * The local random threshold are all equal: <center> <math> \sigma_i^{th}=1, \quad \forall i </math></center>. Instead of following the evoluion...")
 
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= Avalanches and BGW process=
= Avalanches and Bienaymé-Galton-Watson process=
 
<Strong> Goal: </Strong> We solve the mean field version of the cellular automaton, derive its avalanche statistics and make a connection with the Bienaymé-Galton-Watson process used to describe an epidemic outbreak.


= Fully connected model foor the cellular automata (mean field)=
= Fully connected model foor the cellular automata (mean field)=

Revision as of 15:09, 29 February 2024

Avalanches and Bienaymé-Galton-Watson process

Goal: We solve the mean field version of the cellular automaton, derive its avalanche statistics and make a connection with the Bienaymé-Galton-Watson process used to describe an epidemic outbreak.

Fully connected model foor the cellular automata (mean field)

Let's study the mean field version of the cellular automata introduced in the previous lecture.

  • The elastic coupling is with all neighbours

.

  • The local random threshold are all equal:

.



Instead of following the evoluion of the , it is useful to introduce the distance from threshold

Hence, an unstable point, , is stabilized to a value drawn from . The stress redistribution induced on each bloch is


In the limit we define the distribution and write its evolution equation.

  • Drive: Changing gives
  • Instability: This shift is stable far from the origin, however for a fraction of the points of the interface is unstable. Due to the stress drop, their distance to instability will be . Hence, one writes
  • Stress redistribution: as a consequence all points move to the origin of

where

  • Avalanche: Let us call we can write

and finally:

Stationary solution

Increasing the drive the distribution converge to the fixed point:

  • Determne using
  • Show