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On the Fundamental Equation of Nonequilibrium Statistical Physics -- Nonequilibrium Entropy Evolution Equation and the Formula for Entropy Production Rate

机译:关于非平衡统计物理学的基本方程 -   非平衡熵演化方程和熵的公式   生产率

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摘要

In this paper we presented an overview on our works. More than ten years ago,we proposed a new fundamental equation of nonequilibrium statistical physics inplace of the present Liouville equation. That is the stochastic velocity type'sLangevin equation in 6N dimensional phase space or its equivalent Liouvillediffusion equation. This equation is time-reversed asymmetrical. It shows thatthe form of motion of particles in statistical thermodynamic systems has thedrift-diffusion duality, and the law of motion of statistical thermodynamics isexpressed by a superposition of both the law of dynamics and stochasticvelocity and possesses both determinism and probability. Hence it is differentwith the law of motion of particles in dynamical systems. Starting from thisfundamental equation the BBGKY diffusion equation hierarchy, the Boltzmanncollision diffusion equation, the hydrodynamic equations such as the massdrift-diffusion equation, the Navier-Stokes equation and the thermalconductivity equation have been derived and presented here. What is moreimportant, we first constructed a nonlinear evolution equation ofnonequilibrium entropy density in 6N, 6 and 3 dimensional phase space,predicted the existence of entropy diffusion. This evolution equation revealsthat the time rate of change of nonequilibrium entropy density originatestogether from its drift, diffusion and production in space. Furthermore, wepresented a formula for entropy production rate (i.e. the law of entropyincrease), proved that internal attractive force in nonequilibrium system canresult in entropy decrease while internal repulsive force leads to anotherentropy increase, obtained an unified theoretical expression for thermodynamicdegradation and self-organizing evolution, and revealed that the entropydiffusion mechanism caused the system to approach to equilibrium.
机译:在本文中,我们概述了我们的工作。十多年前,我们提出了一个新的非平衡统计物理基本方程,代替了现在的Liouville方程。这就是在6N维相空间中的随机速度类型的Langevin方程或其等效的Liouvillediffusion方程。该方程是时间逆的不对称的。结果表明,统计热力学系统中粒子的运动形式具有漂移-扩散对偶性,统计热力学的运动规律由动力学定律和随机速度的叠加表示,具有确定性和概率性。因此,它与动力学系统中粒子的运动定律不同。从这个基本方程开始,BBGKY扩散方程层次,玻尔兹曼碰撞扩散方程,流体动力学方程(例如质量漂移-扩散方程),Navier-Stokes方程和导热系数方程在此得到了介绍。更重要的是,我们首先构造了一个在6N,6和3维相空间中的非平衡熵密度的非线性演化方程,预测了熵扩散的存在。这个演化方程表明,非平衡熵密度的时间变化率完全源于其在空间中的漂移,扩散和产生。此外,我们提出了一个熵产生率的公式(即熵增加定律),证明了非平衡系统内部的吸引力会导致熵的减少,而内部排斥力会导致另一个熵的增加,从而获得了热力学降解和自组织演化的统一理论表达式。 ,并揭示了熵扩散机制使系统趋于平衡。

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    Xing, Xiu-San;

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  • 年度 2011
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