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多分散铁磁流体的磁化和磁化率的理论与模拟比较。

Comparison between theory and simulations for the magnetization and the susceptibility of polydisperse ferrofluids.

机构信息

Institute of Physics and Mechatronics, University of Pannonia, H-8201 Veszprém, PO Box 158, Hungary.

出版信息

J Phys Condens Matter. 2013 Nov 20;25(46):465108. doi: 10.1088/0953-8984/25/46/465108. Epub 2013 Oct 23.

Abstract

The influence of polydispersity on the magnetization of ferrofluids is studied based on a previously published magnetization equation of state (Szalai and Dietrich, 2011 J. Phys.: Condens. Matter 23 326004) and computer simulations. The polydispersity of the particle diameter is described by the gamma distribution function. Canonical ensemble Monte Carlo simulations have been performed in order to test these theoretical results for the initial susceptibility and the magnetization. The results for the magnetic properties of the polydisperse systems turn out to be in quantitative agreement with our present simulation data. In addition, we find good agreement between our theory and experimental data for magnetite-based ferrofluids.

摘要

基于先前发表的磁化状态方程(Szalai 和 Dietrich,2011 J. Phys.:Condens. Matter 23 326004)和计算机模拟,研究了多分散性对铁磁流体磁化的影响。颗粒直径的多分散性用伽马分布函数来描述。为了检验这些关于初始磁化率和磁化强度的理论结果,进行了正则系综蒙特卡罗模拟。多分散体系磁性质的结果与我们目前的模拟数据在定量上是一致的。此外,我们还发现我们的理论与基于磁铁矿的铁磁流体的实验数据之间有很好的一致性。

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