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Deposition of Colloidal Particles onHomogeneous Surfaces: Integral-EquationTheory and Monte Carlo Simulation

机译:胶体颗粒的沉积不均匀表面:积分式odationtheory和Monte Carlo仿真

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Deposition of large particles such as colloidal or bio-particles on a solid surface isusually modeled by the random sequential adsorption (RSA). The model was previouslydescribed by the integral-equation theory whose validity was proved by Monte Carlo simulation.This work generalized the model to include the concentration effect of added particles on thesurface. The fraction of particles inserted was varied by the reduced number density of 0.05, 0.1,and 0.2. It was found that the modified integral-equation theory yielded the results in goodaccordance with the simulation. Regarding colloidal particles as hard spheres, when the fractionof particles added was increased, the radial distribution function has higher peak, due to thecooperative and entropic effects. This work could bridge the gap between equilibrium adsorption,where all particles may be considered moving and RSA, where there is no moving particle onthe surface. In addition, the effect of attractive interaction was also incorporated and it wasfound that increasing number of added particles at one time yields less values of the radialdistribution function.
机译:在通过随机顺序吸附(RSA)的固体表面上沉积如胶体或生物颗粒的大颗粒。通过蒙特卡罗模拟证明了一体式方程理论以先前输入的模型,其有效性仿真。该工作概括了模型,包括添加颗粒对句子上添加的颗粒的浓度效应。插入的颗粒的颗粒的级分通过减小的数量密度为0.05,0.1和0.2。结果发现,改进的积分方程理论产生了仿真效果的结果。关于胶体颗粒作为硬球体,当增加颗粒的颗粒时,由于备注和熵效应,径向分布函数具有更高的峰。这项工作可以弥合平衡吸附之间的间隙,其中所有颗粒可以被认为是移动和RSA,在此外表面没有移动粒子。此外,还掺入了含有吸引性相互作用的效果,并且逐渐发现,一次增加添加的颗粒数量,产生较少的放射性分布功能的值。

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