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首页> 外文期刊>Journal of Physics, A. Mathematical and General: A Europhysics Journal >CAPILLARY CONDENSATION IN THE TWO-DIMENSIONAL LATTICE GAS - A MONTE CARLO TEST OF FLUCTUATION CORRECTIONS TO THE KELVIN EQUATION
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CAPILLARY CONDENSATION IN THE TWO-DIMENSIONAL LATTICE GAS - A MONTE CARLO TEST OF FLUCTUATION CORRECTIONS TO THE KELVIN EQUATION

机译:二维晶格气体中的毛细管凝结-开尔文方程波动修正的蒙特卡罗测试

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A two-dimensional lattice gas model with nearest-neighbour attractive interaction confined in a strip of width L between two parallel boundaries at which an attractive short-range force acts is studied by Monte Carlo simulations, for cases where the system is in the wet phase near the critical wetting transition line for L --> infinity. We study the shift of the chemical potential mu of the transition in the strip as a function of L by thermodynamic integration methods, Delta mu = mu(c)(L) - mu(c)(infinity), and also obtain the thickness l(c) of the wetting film at the chemical potential mu(c)(L) at which capillary condensation occurs. In the range 32 less than or equal to L less than or equal to 120 the data are consistent with a variation according to the Kelvin equation, Delta mu proportional to L-1, as well as with a shifted Kelvin equation, Delta mu proportional to (L - L-0)(-1), with a constant L-0. Thus, we find no evidence for the fluctuation correction {Delta mu proportional to (L - 3l(c))(-1)} predicted by Parry and Evans. This failure is traced back to the fact that in this range of linear dimensions there are not yet any well developed wetting layers at coexistence, and the prediction l(c) proportional to L-1/3 from the theory of complete wetting does not hold in this range either. Instead we empirically find a relation l(c) proportional to ln L + constant over the whole range of system sizes we studied. [References: 32]
机译:对于系统处于湿相的情况,通过蒙特卡罗模拟研究了具有最近邻吸引相互作用的二维晶格气体模型,该模型被限制在两个平行边界之间的宽度为L的条带上,在该条带上有短距离吸引力作用接近L的临界润湿过渡线->无穷大。我们通过热力学积分方法研究了带钢中跃迁的化学势mu随L的变化,Δmu = mu(c)(L)-mu(c)(infinity),并获得了厚度l (c)在发生毛细管冷凝的化学势为mu(c)(L)的湿膜上。在32小于或等于L小于或等于120的范围内,数据与根据开尔文方程式的变化Δmu与L-1成比例,以及与移位的开尔文方程式的变化Δmu与以下条件相一致: (L-L-0)(-1),且常数为L-0。因此,我们没有发现任何证据可以证明由Parry和Evans预测的波动校正{Δmu与(L-3l(c))(-1)成比例”。失败的原因可追溯到以下事实:在此线性尺寸范围内,尚没有任何发达的润湿层共存,并且完全润湿理论中与L-1 / 3成比例的预测l(c)不成立。在这个范围内。取而代之的是,我们凭经验找到了在我们研究的整个系统尺寸范围内与ln L +常数成比例的关系l(c)。 [参考:32]

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