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磁流体中自激波过程的实验与理论研究

Experimental and Theoretical Study of an Autowave Process in a Magnetic Fluid.

机构信息

Department of Digital Development, North-Caucasus Federal University, 1 Pushkin Street, 355017 Stavropol, Russia.

Department of Information Technologies, MIREA-Russian Technological University, 8 Kulakova Avenue, 355000 Stavropol, Russia.

出版信息

Int J Mol Sci. 2022 Jan 31;23(3):1642. doi: 10.3390/ijms23031642.

Abstract

Magnetic fluid (MF) is a colloidal system consisting of ferromagnetic particles (magnetite) with a diameter of ~10 nm suspended in a dispersion medium of a carrier fluid (for example, kerosene). A distinctive feature of magnetic fluid is the fact that when an electric field is applied to it using two electrodes, thin layers consisting of close-packed particles of the dispersed phase are formed in the regions near the surface of both electrodes. These layers significantly affect the macroscopic properties of the colloidal system. In this work, the interpretation of the near-electrode layer is for the first time given as a new type of liquid membrane, in which the particles of the dispersed phase become charged with the opposite sign. On the basis of experimental studies, we propose a physicochemical mechanism of the autowave process in a cell with a magnetic fluid. It is based on the idea of oppositely recharging colloidal particles of magnetite in a liquid membrane. A mathematical model of an autowave process, which is described by a system of coupled partial differential equations of Nernst-Planck-Poisson and Navier-Stokes with appropriate boundary conditions, is proposed for the first time. One-dimensional, two-dimensional, and three-dimensional versions of the model are considered. The dependence of the frequency of concentration fluctuations on the stationary voltage between the electrodes was obtained, and the time of formation of a liquid membrane was estimated. Qualitative agreement between theoretical and experimental results has been established.

摘要

磁流体(MF)是一种胶体系统,由直径约为 10nm 的铁磁颗粒(磁铁矿)悬浮在载体流体(例如煤油)中组成。磁流体的一个显著特点是,当在两个电极上施加电场时,在靠近两个电极表面的区域中形成由分散相的紧密堆积颗粒组成的薄层层。这些层显著影响胶体系统的宏观性质。在这项工作中,首次将近电极层解释为一种新型的液体膜,其中分散相的颗粒带相反符号的电荷。基于实验研究,我们提出了一个具有磁流体的电池中自波过程的物理化学机制。它基于在液体膜中对胶体磁铁矿颗粒进行相反充电的想法。首次提出了由纳恩斯特-普朗克-泊松和纳维-斯托克斯耦合偏微分方程系统以及适当的边界条件描述的自波过程的数学模型。考虑了一维、二维和三维模型。获得了浓度波动频率与电极间稳态电压的关系,并估计了液体膜形成的时间。已经建立了理论和实验结果之间的定性一致性。

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