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18 - Simulations, complexity, and laws of nature

Published online by Cambridge University Press:  05 June 2012

Joseph L. McCauley
Affiliation:
University of Houston
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Summary

Integrability, chaos, and complexity

Phase space flows divide into two basic classes: completely integrable and ‘nonintegrable’ (incompletely integrable). In the first case the motion is equivalent to a single time-translation for all finite times (chapter 3). In the second case singularities of the conservation laws prevent this degree of simplicity (section 13.2).

Nonintegrable systems can be divided further into two classes: those that are in principle predictable for all times, and those that are not. The first class includes deterministic dynamics where there is a generating partition. An example, the asymmetric tent map, was given in chapter 14. A chaotic dynamical system generates infinitely many different statistical distributions through the variation of classes of initial conditions. Only the differentiable distribution (corresponding to the invariant density) is generated by initial data that occur with measure one. The fragmented statistical distributions, including multifractal ones, occur for the measure zero set of initial conditions.

Whenever a dynamical system is computable (McCauley, 1993), which is the only case that can be used computationally and empirically, then the measure zero initial conditions are of dominant importance. There is, as yet, no known case in nature where the differentiable probability distribution describes the experiments or observations performed on a driven-dissipative chaotic dynamical system. The generating partition forms the support of every probability distribution that occurs mathematically, and can be discovered (when it exists) through backward iteration of the Poincaré map.

Type
Chapter
Information
Classical Mechanics
Transformations, Flows, Integrable and Chaotic Dynamics
, pp. 441 - 452
Publisher: Cambridge University Press
Print publication year: 1997

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