经典力学
相空间
统计力学
物理
连续介质力学
非线性系统
统计物理学
偏微分方程
粒子(生态学)
相场模型
流体力学
常微分方程
机械
微分方程
相(物质)
热力学
量子力学
地质学
海洋学
作者
Wm. G. Hoover,Christian G. Hoover
出处
期刊:Molecular Physics
[Taylor & Francis]
日期:2003-06-10
卷期号:101 (11): 1559-1573
被引量:34
标识
DOI:10.1080/0026897021000026647
摘要
The microscopic and macroscopic versions of fluid mechanics differ qualitatively. Microscopic particles obey time-reversible ordinary differential equations. The resulting particle trajectories {q(t)} may be time-averaged or ensemble-averaged so as to generate field quantities corresponding to macroscopic variables. On the other hand, the macroscopic continuum fields described by fluid mechanics follow irreversible partial differential equations. Smooth particle methods bridge the gap separating these two views of fluids by solving the macroscopic field equations with particle dynamics that resemble molecular dynamics. Recently, nonlinear dynamics have provided some useful tools for understanding the relationship between the microscopic and macroscopic points of view. Chaos and fractals play key roles in this new understanding. Non-equilibrium phase-space averages look very different from their equilibrium counterparts. Away from equilibrium the smooth phase-space distributions are replaced by fractional-dimensional singular distributions that exhibit time irreversibility.
科研通智能强力驱动
Strongly Powered by AbleSci AI