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Entropy production and transports in a conservative multibaker map with energy

机译:具有能量的保守多贝克图中的熵产生和输运

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For a previously introduced conservative multibaker map with energy, the Gaspard-Gilbert-Dorfman entropy production of the stationary slate induced by the flux boundary condition is calculated and the entropy production is shown (i) to be nonnegative, (ii) to vanish in the fine-grained limit for finite chains, (iii) to take the phenomenologically expected value in the middle of the chain and to deviate From it near the boundaries, and (iv) to reduce to the phenomenological expression in the scaling limit where the lattice site n is an element of Z and time t is an element of Z are scaled respectively as n = LxiX and t = LtauT and the limits of L-xi --> +infinity and L-tau --> +infinity are taken while keeping the diffusion coefficient D = lL(tau)/L-xi(2) constant, I being the transition rate of the model. The mass and heat transports are also studied in the scaling limit under an additional assumption that the edges of the chain are in equilibrium with different temperatures. In the linear heat transport regime, Fourier's Law of heat conduction and t:he thermodynamic expression of the associated entropy production are obtained. [References: 48]
机译:对于先前引入的带有能量的保守多贝克图,计算了由通量边界条件引起的固定板岩的Gaspard-Gilbert-Dorfman熵产生,并且该熵产生显示为(i)为非负值,(ii)在熵值中消失。有限链的细粒度限制,(iii)取链中间的现象学预期值,并在边界附近偏离它,以及(iv)在晶格位置处的缩放极限中还原为现象学表达n是Z的元素,时间t是Z的元素,分别缩放为n = LxiX和t = LtauT,在保持不变的情况下取L-xi-> +无穷大和L-tau-> +无穷大的极限扩散系数D = lL(tau)/ L-xi(2)常数,I是模型的转化率。在链条的边缘在不同温度下处于平衡状态的附加假设下,还在缩放比例下研究了质量和热传递。在线性传热条件下,获得了热传导的傅立叶定律和相关熵产生的热力学表达式。 [参考:48]

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