首页> 外文期刊>Journal of magnetism and magnetic materials >Regime of aggregate structures and magneto-rheological characteristics of a magnetic rod-like particle suspension: Monte Carlo and Brownian dynamics simulations
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Regime of aggregate structures and magneto-rheological characteristics of a magnetic rod-like particle suspension: Monte Carlo and Brownian dynamics simulations

机译:棒状颗粒悬浮液的聚集体结构和磁流变特性:蒙特卡洛和布朗动力学模拟

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In the present study, we address a suspension composed ferromagnetic rod-like particles to elucidate a regime change in the aggregate structures and the magneto-rheological characteristics. Monte Carlo simulations have been employed for investigating the aggregate structures in thermodynamic equilibrium, and Brownian dynamics simulations for magneto-rheological features in a simple shear flow. The main results obtained here are summarized as follows. For the case of thermodynamic equilibrium, the rod-like particles aggregate to form thick chain-like clusters and the neighboring clusters incline in opposite directions. If the external magnetic field is increased, the thick chain-like clusters in the magnetic field direction grow thicker by adsorbing the neighboring clusters that incline in the opposite direction. Hence, a significant phase change in the particle aggregates is not induced by an increase in the magnetic field strength. For the case of a simple shear flow, even a weak shear flow induces a significant regime change from the thick chain-like clusters of thermodynamic equilibrium into wall-like aggregates composed of short raft-like clusters. A strong external magnetic field drastically changes these aggregates into wall-like aggregates composed of thick chain-like clusters rather than the short raft-like clusters. The internal structure of these aggregates is not strongly influenced by a shear flow, and the formation of the short raft-like clusters is maintained inside the aggregates. The main contribution to the net viscosity is the viscosity component due to magnetic particle-particle interaction forces in relation to the present volumetric fraction. Hence, a larger magnetic interaction strength and also a stronger external magnetic field give rise to a larger magneto-rheological effect. However, the dependence of the viscosity on these factors is governed in a complex manner by whether or not the wall-like aggregates are composed mainly of short raft-like clusters. An increase in the shear rate functions to simply decrease the effect of the magnetic particle-particle and the particle-field interactions.
机译:在本研究中,我们研究了由铁磁棒状颗粒组成的悬浮液,以阐明聚集体结构和磁流变特性的变化。蒙特卡洛模拟已用于研究热力学平衡状态下的骨料结构,布朗动力学模拟用于简单剪切流中的磁流变特征。这里获得的主要结果总结如下。对于热力学平衡的情况,棒状颗粒聚集形成厚的链状簇,并且相邻的簇向相反的方向倾斜。如果增加外部磁场,则通过吸收沿相反方向倾斜的相邻簇,在磁场方向上的粗链状簇变得更厚。因此,磁场强度的增加不会引起颗粒聚集体的明显相变。对于简单的剪切流,即使是弱剪切流也会引起从热力学平衡的粗链状簇到短筏状簇的壁状聚集体的显着状态变化。强大的外部磁场将这些聚集体急剧地变成壁厚的聚集体,由壁厚的链状团簇组成,而不是短的筏状团簇。这些骨料的内部结构不受剪切流的强烈影响,并且在骨料内部保持了短筏状簇的形成。对净粘度的主要贡献是由于相对于当前体积分数的磁性颗粒-颗粒相互作用力引起的粘度成分。因此,更大的磁相互作用强度以及更强的外部磁场引起更大的磁流变效应。然而,粘度对这些因素的依赖性以复杂的方式由壁状聚集体是否主要由短木筏状团簇构成。剪切速率的增加起到简单地减小磁性粒子-粒子和粒子-场相互作用的作用的作用。

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