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Magnetorheology in rotating magnetic fields.

机译:旋转磁场中的磁流变学。

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We studied the flow of ferrofluid induced by rotating magnetic fileds. This flow was observed for first time in 1967 by Moskowitz and Rosensweig [Appl. Phys. Lett., 10, pag. 301 (1967)] and since then researchers has attempted to explain the phenomenon through theories such as spin diffusion, magnetic tangential surface stresses, and others that claim the impossibility in to obtain ferrofluid flow through a uniform rotating magnetic field. These theories have been tested using experimental observations of tracer particles on the free surface of the container because of the difficulty in obtaining bulk velocity profiles by traditional methods. Nevertheless, as is demonstrated herein such surface velocity profiles are inadequate for the assessment of bulk flow theories as they misrepresent the bulk flow of the fluid and as such can be the cause of confusion.; The principal contribution of the thesis is to provide experimental evidence that allows clarification of the mechanism responsible for the observed flow. To this end we focused on the flow of ferrofluid induced by a rotating magnetic field in a cylindrical container and between two coaxial cylinders. In order to obtain bulk flow measurements we used the ultrasound velocity profile method. Bulk flow measurements taken in the cylindrical container show the fluid co-rotating with the field in a rigid-body-like fashion throughout most of the bulk region of the container, except near the air-fluid interface, where it was observed to counter-rotate. Our experimental measurements show qualitative agreement with an extension of the spin diffusion theory of Zaitsev and Shliomis [ J. Appl. Mech. Tech. Phys. 10, pag. 696 (1969)], obtained using the regular perturbation method. An estimate of the spin viscosity is obtained from comparison of flow measurements and theoretical results of the extrapolated wall velocity from the regular perturbation method. The estimated value eta' = 5.8 x 10-10 kg ms-1 is several orders of magnitude higher than that obtained from dimensional analysis.; We present the first measurements of bulk flow for ferrofluid in the annular gap between two stationary coaxial cylinders. These results contrast with current theories which only predict flow when one of the cylinders is free to rotate. Qualitative comparison of the experimental results with the predictions of the spin diffusion theory for the annular flow of ferrofluid in the limit of low fields were found in good agreement with velocity profiles obtained for the kerosene based ferrofluid.
机译:我们研究了旋转磁场引起的铁磁流体的流动。 Moskowitz和Rosensweig在1967年首次观察到了这种流动。物理Lett。,10,pag。 301(1967)]之后,研究人员便尝试通过自旋扩散,磁切向表面应力等理论来解释这种现象,这些理论声称不可能通过均匀的旋转磁场获得铁磁流体。由于难以通过传统方法获得体积速度分布图,因此使用容器自由表面上的示踪剂颗粒的实验观察结果对这些理论进行了测试。然而,如本文所证明的,这样的表面速度分布图不足以用于评估整体流动理论,因为它们错误地代表了流体的整体流动,因此可能造成混乱。论文的主要贡献是提供实验证据,以澄清负责观察到的流动的机制。为此,我们集中研究了圆柱形容器中以及两个同轴圆柱体之间由旋转磁场引起的铁磁流体的流动。为了获得大流量测量,我们使用了超声速度剖面法。在圆柱形容器中进行的散装流量测量显示,在整个容器的大部分散装区域中,流体均以类似于刚体的方式与磁场共同旋转,除了在空气-流体界面附近,观察到与旋转。我们的实验测量结果显示,Zaitsev和Shliomis自旋扩散理论的扩展与定性一致[J. Appl。机甲科技物理10,pag。 [696(1969)],使用常规摄动法获得。通过比较流量测量值和常规微扰法得出的外推壁速度的理论结果,可以得出自旋粘度的估计值。估计值eta'= 5.8 x 10-10 kg ms-1,比从尺寸分析获得的估计值高几个数量级。我们介绍了在两个固定同轴圆柱体之间的环形间隙中铁磁流体总体流量的首次测量。这些结果与当前的理论形成了鲜明的对比,后者仅在汽缸之一自由旋转时预测流量。实验结果与自旋扩散理论对铁磁流体在低场范围内的环形流动的预测进行了定性比较,这与基于煤油的铁磁流体的速度分布图非常吻合。

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