Camp Philip J, Elfimova Ekaterina A, Ivanov Alexey O
School of Chemistry, University of Edinburgh, David Brewster Road, Edinburgh, EH9 3FJ, UK.
J Phys Condens Matter. 2014 Nov 12;26(45):456002. doi: 10.1088/0953-8984/26/45/456002. Epub 2014 Oct 20.
The effects of particle-size polydispersity on the initial susceptibilities of concentrated ferrofluids are analyzed using a combination of theory and computer simulation. The study is focused on a model ferrofluid with a prescribed magnetic-core diameter distribution, a fixed non-magnetic surface layer (corresponding to a demagnetized layer and adsorbed surfactant) and a combination of dipolar and hard-core interactions. The non-trivial effects of polydispersity are identified by comparing the initial susceptibilities of monodisperse and polydisperse ferrofluids with the same Langevin susceptibility. The theory is based on a correction to the second-order modified mean-field theory arising from a formal Mayer-type cluster expansion; this correction is dependent on a parameter similar to the normal dipolar coupling constant, except that it contains a complicated double average over the particle-size distribution, which means that the initial susceptibility should depend significantly on polydispersity. Specifically, the theory predicts that the initial susceptibility is enhanced significantly by polydispersity. This prediction is tested rigorously against results from Monte Carlo simulations and is found to be robust. The qualitative agreement between theory and simulation is already satisfactory, but the quantitative agreement could be improved by a systematic extension of the cluster expansion. The overall conclusion is that polydispersity should be accounted for carefully in magnetogranulometric analyses of real ferrofluids.
采用理论与计算机模拟相结合的方法,分析了粒径多分散性对浓铁磁流体初始磁化率的影响。该研究聚焦于一种模型铁磁流体,其具有规定的磁芯直径分布、固定的非磁性表面层(对应于退磁层和吸附的表面活性剂)以及偶极相互作用和硬核相互作用的组合。通过比较具有相同朗之万磁化率的单分散和多分散铁磁流体的初始磁化率,确定了多分散性的重要影响。该理论基于对二阶修正平均场理论的修正,该修正源于形式上的迈耶型簇展开;这种修正依赖于一个类似于正常偶极耦合常数的参数,不同之处在于它包含了对粒径分布的复杂双重平均,这意味着初始磁化率应显著依赖于多分散性。具体而言,该理论预测多分散性会显著提高初始磁化率。这一预测通过与蒙特卡罗模拟结果进行严格检验,发现是可靠的。理论与模拟之间的定性一致性已经令人满意,但通过系统扩展簇展开可以改善定量一致性。总体结论是,在对实际铁磁流体进行磁粒度分析时,应仔细考虑多分散性。