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Equation of State for Macromolecules of Variable Flexibility in Good Solvents: A Comparison of Techniques for Monte Carlo Simulations of Lattice Models

机译:良好的可变灵活性大分子的状态方程   溶剂:格子蒙特卡罗模拟技术的比较   楷模

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摘要

The osmotic equation of state for the athermal bond fluctuation model on thesimple cubic lattice is obtained from extensive Monte Carlo simulations. Forshort macromolecules (chain length N=20) we study the influence of variouschoices for the chain stiffness on the equation of state. Three techniques areapplied and compared in order to critically assess their efficiency andaccuracy: the repulsive wall method, the thermodynamic integration method(which rests on the feasibility of simulations in the grand canonicalensemble), and the recently advocated sedimentation equilibrium method, whichrecords the density profile in an external (e.g. gravitation-like) field andinfers, via a local density approximation, the equation of state from thehydrostatic equilibrium condition. We confirm the conclusion that the lattertechnique is far more efficient than the repulsive wall method, but we findthat the thermodynamic integration method is similarly efficient as thesedimentation equilibrium method. For very stiff chains the onset of nematicorder enforces the formation of isotropic-nematic interface in thesedimentation equilibrium method leading to strong rounding effects anddeviations from the true equation of state in the transition regime.
机译:通过广泛的蒙特卡洛模拟,获得了简单立方晶格上非热键涨落模型的渗透状态方程。对于短大分子(链长N = 20),我们研究了链选择的各种选择对状态方程的影响。为了严格评估它们的效率和准确性,应用了三种技术并进行了比较:斥力壁法,热力学积分法(取决于在大炮台状群中模拟的可行性)和最近提倡的沉降平衡法,该方法记录了岩心中的密度分布。外部(如重力)场,并通过局部密度近似推导静水力平衡条件下的状态方程。我们确认了这样的结论:后一种技术比排斥壁方法要有效得多,但是我们发现热力学积分方法与这些沉降平衡方法同样有效。对于非常刚性的链,向列相的出现迫使这些沉降平衡方法形成各向同性向列界面,从而导致强烈的舍入效应和与过渡状态下真实状态方程的偏离。

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