论文标题

相互作用的铁洛群的动力学有效现场模型:I。均质,不均匀和多分散病例的衍生物

Dynamical Effective Field Model for Interacting Ferrofluids: I. Derivations for homogeneous, inhomogeneous, and polydisperse cases

论文作者

Fang, Angbo

论文摘要

最近,我提出了一种非扰动动力学有效场模型(DEFM),以定量描述相互作用的铁氟烷的动力学。它的预测与模拟的结果相比非常好。在本文中,我通过将DEFM推导到动力学密度函数理论(DDFT)的框架内,将DEFM推向了牢固的理论基础,在该框架中,相关诱导的自由能的相关部分通过瞬时磁化的函数近似。由于存在远距离偶极 - 偶极 - 偶极相互作用,因此将DEFM推广到宏观和介质尺度分离的不均匀有限尺寸样品。自然而然地从微观考虑出来,并始终如一地考虑了撤电场。介质尺度上产生的粒子动力学仅涉及宏观局部数量,例如局部磁化和麦克斯韦场。然而,局部驱逐磁场本质上是在遥远的宏观位置上的磁化。因此,可以将涉及不同宏观位置之间信息传递的两尺度平行算法应用于不均匀样本中的粒子旋转动力学。我还得出了多分散铁体流体的DEFM,其中属于不同物种的粒子的动力学可以彼此强烈耦合。我讨论了获得热力学一致的多分散磁化弛豫方程的基本假设,该方程与单分散性铁氟烷的通用形式相同。本文提出的理论进步对于对铁流体动力学的定性理解和定量建模至关重要。

Quite recently I have proposed a nonperturbative dynamical effective field model (DEFM) to quantitatively describe the dynamics of interacting ferrofluids. Its predictions compare very well with the results from simulations. In this paper I put the DEFM on firm theoretical ground by deriving it within the framework of dynamical density functional theory (DDFT), in which the relevant part of correlation-induced free energy is approximated by a function of the instantaneous magnetization. The DEFM is generalized to inhomogeneous finite-size samples for which the macroscopic and mesoscopic scale separation is nontrivial due to the presence of long-range dipole-dipole interactions. The demagnetizing field naturally emerges from microscopic considerations and is consistently accounted for. The resulting particle dynamics on the mesoscopic scale only involves macroscopically local quantities such as local magnetization and Maxwell field. Nevertheless, the local demagnetizing field essentially couples to magnetization at distant macroscopic locations. Thus, a two-scale parallel algorithm, involving information transfer between different macroscopic locations, can be applied to fully resolve particle rotational dynamics in an inhomogeneous sample. I also derive the DEFM for polydisperse ferrofluids, in which the dynamics of particles belonging to different species can be strongly coupled to each other. I discuss the underlying assumptions in obtaining a thermodynamically consistent polydisperse magnetization relaxation equation, which is of the same generic form as that for monodisperse ferrofluids. The theoretical advances presented in this paper are important for both qualitative understanding and quantitative modeling of ferrofluid dynamics.

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