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复杂系统的熵的三个方面:信息、热力学和最大熵原理。

Three faces of entropy for complex systems: Information, thermodynamics, and the maximum entropy principle.

机构信息

Section for the Science of Complex Systems, CeMSIIS, Medical University of Vienna, Spitalgasse 23, A-1090 Vienna, Austria.

Santa Fe Institute, 1399 Hyde Park Road, Santa Fe, New Mexico 87501, USA.

出版信息

Phys Rev E. 2017 Sep;96(3-1):032124. doi: 10.1103/PhysRevE.96.032124. Epub 2017 Sep 15.

DOI:10.1103/PhysRevE.96.032124
PMID:29346985
Abstract

There are at least three distinct ways to conceptualize entropy: entropy as an extensive thermodynamic quantity of physical systems (Clausius, Boltzmann, Gibbs), entropy as a measure for information production of ergodic sources (Shannon), and entropy as a means for statistical inference on multinomial processes (Jaynes maximum entropy principle). Even though these notions represent fundamentally different concepts, the functional form of the entropy for thermodynamic systems in equilibrium, for ergodic sources in information theory, and for independent sampling processes in statistical systems, is degenerate, H(p)=-∑{i}p{i}logp_{i}. For many complex systems, which are typically history-dependent, nonergodic, and nonmultinomial, this is no longer the case. Here we show that for such processes, the three entropy concepts lead to different functional forms of entropy, which we will refer to as S_{EXT} for extensive entropy, S_{IT} for the source information rate in information theory, and S_{MEP} for the entropy functional that appears in the so-called maximum entropy principle, which characterizes the most likely observable distribution functions of a system. We explicitly compute these three entropy functionals for three concrete examples: for Pólya urn processes, which are simple self-reinforcing processes, for sample-space-reducing (SSR) processes, which are simple history dependent processes that are associated with power-law statistics, and finally for multinomial mixture processes.

摘要

有至少三种不同的方法来概念化熵

作为物理系统的广延热力学量的熵(克劳修斯、玻尔兹曼、吉布斯)、作为遍历源信息产生的度量的熵(香农)以及作为多项式过程统计推断的手段的熵(杰恩斯最大熵原理)。尽管这些概念代表了根本不同的概念,但平衡热力学系统、信息论中的遍历源以及统计系统中独立采样过程的熵的函数形式是退化的,H(p)=-∑{i}p{i}logp_{i}。对于许多复杂系统,它们通常是依赖历史的、非遍历的和非多项式的,情况就不再如此。在这里,我们表明对于这些过程,三个熵概念导致了不同的熵函数形式,我们将其称为 EXT 熵、IT 源信息率和 MEP 熵函数,它们出现在所谓的最大熵原理中,该原理表征了系统最可能的可观察分布函数。我们明确地为三个具体例子计算了这三个熵函数:对于玻尔兹曼抽样过程,这是简单的自我强化过程,对于样本空间缩减(SSR)过程,这是与幂律统计相关的简单依赖历史的过程,最后是对于多项式混合过程。

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