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Agenda
l Introduction
l Background material
l Self-Organized Criticality Defined
l Examples in Nature
l Experiments
l Conclusion
Obey the Law!
l Single components in a system are governedby rules that dictate how the componentinteracts with others
System in Balance
l Predictable
l States of equilibrium– Stable, small disturbances in system have only local
impact
Self-Organized Criticality: Defined
l Self-Organized Criticality can be considered asa characteristic state of criticality which isformed by self-organization in a long transientperiod at the border of stability and chaos
Characteristics
l Open dissipative systems
l The components in the system are governedby simple rules
Characteristics (continued)
l Thresholds exists within the system
l Pressure builds in the system until it exceedsthreshold
Characteristics (Continued)
l Naturally Progresses towards critical statel Small agitations in system can lead to system effects called
avalanches
l This happens regardless of the initial state of the system
Domino Effect: System wide events
l The same perturbation may lead to smallavalanches up to system wide avalanches
Characteristics (continued)
l Most changes occurs through catastrophicevent rather than a gradual change
l Punctuations, large catastrophic events that effect theentire system
Nature can be viewed as a system
l It has many individual components workingtogether
l Each component is governed by lawsl e.g, basic laws of physics
Fractals:
l Geometric structures with features of all lengthscales (e.g. scale free)
l Ubiquitous in nature
l Snowflakes
l Coast lines
Can SOC be the common link?
l Ubiquitous phenomenal No self-tuning
l Must be self-organized
l Is there some underlying link
Sand Pile Model
l An MxN grid Z
l Energy enters the model by randomly addingsand to the model
l We want to measure the avalanches causedby adding sand to the model
Example Sand pile grid
l Grey border representsthe edge of the pile
l Each cell, represents acolumn of sand
Model Rules
l Drop a single grain of sand at a randomlocation on the grid
l Random (x,y)
l Update model at that point: Z(x,y) ‡ Z(x,y)+1
l If Z(x,y) > Threshold, spark an avalanchel Threshold = 3
Adding Sand to pile
l Chose Random (x,y)position on grid
l Increment that celll Z(x,y) ‡ Z(x,y)+1
l Number of sand grainsindicated by colour code
By: Maslov [6]
Avalanches
l When threshold hasbeen exceeded, anavalanche occurs
l If Z(x,y) > 3l Z(x,y) ‡ Z(x,y) – 4
l Z(x+-1,y) ‡ Z(x+-1,y) +1
l Z(x,y) ‡ Z(x,y+-1) +1
By: Maslov [6]
Observances
l Transient/stable phase
l Progresses towards Critical phasel At which avalanches of all sizes and durations
l Critical state was robustl Various initial states. Random, not random
l Measured events follow the desired Power Law
Sandpile: Model Variations
l Rotating Drum
l Done by Heinrich Jaeger
l Sand pile forms alongthe outside of the drum
Rotating Drum
Conclusion
l Shortfallsl Does not explain why or how things self-organize into the
critical state
l Cannot mathematically prove that systems follow thepower law
l Benefitsl Gives us a new way of looking at old problems
References:
l [1] P. Bak, How Nature Works. Springer -Verlag, NY,1986.
l [2] H.J.Jensen. Self-Organized Criticality – EmergentComplex Behavior in Physical and Biological Systems.Cambridge University Press, NY, 1998.
l [3] T. Krink, R. Tomsen. Self-Organized Criticality andMass Extinction in Evolutionary Algorithms. Proc. IEEEint. Conf, on Evolutionary Computing 2001: 1155-1161.
l [4] P.Bak, C. Tang, K. WiesenFeld. Self-OrganizedCriticality: An Explanation of 1/f Noise. PhysicalReview Letters. Volume 59, Number 4, July 1987.
References Continued
l [5] P.Bak. C. Tang. Kurt Wiesenfeld. Self-OrganizedCriticality. A Physical Review. Volume 38, Number 1.July 1988.
l [6]S. Maslov. Simple Model of a limit order-drivenmarket. Physica A. Volume 278, pg 571-578. 2000.
l [7] P.Bak. Website: http://cmth.phy.bnl.gov/~maslov/Sandpile.htm.Downloaded on March 15th 2003.
l [8] Website:http://platon.ee.duth.gr/~soeist7t/Lessons/lessons4.htm.Downloaded March 3rd 2003.