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Correlation of rheological properties of ferrofluid-based magnetorheological fluids using the concentration-magnetization superposition

机译:利用浓缩 - 磁化叠加的铁磁石基磁流变流变流变性能的相关性

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摘要

In this work, the yield stress previously measured for some ferrofluid-based magnetorheological fluids (FF-MRFs) with various volume fractions of nanosize magnetite (phi) and micrometer size iron particle (Phi(Fe)), for a wide range of magnetic fields (B), is further investigated from a new point of view. The mean magnetization (MM) approximation developed for conventional magnetorheological (MR) suspensions is extended to FF-MRFs and a characteristic magnetic stress is defined and determined by using the average iron particles magnetization in FF-MRF suspensions. We thus generate a rheological master curve of static yield stress vs characteristic magnetic stress, for different values of phi, Phi(Fe), and B by using a single variable, the characteristic magnetic stress, which contains only data that can be determined experimentally. This indicates, for the first time in literature, a concentration-magnetization superposition in the case of FF-MRFs. This master curve is useful to determine an optimal composition that allows one to obtain FF-MRFs with the best possible MR properties for a particular application. We also find that, regardless of the magnetite nanoparticles' volume fraction in the carrier ferrofluid, when the iron volume fraction is close to Phi(Fe)* = 30% a change in magnetorheological behavior appears; this is most probably due to the structural transition from chainlike structures of iron particles to more complex ones. In addition, in order to show that the MM approximation may be used even for the FF-MRFs, we employ the finite element method (FEM) to compute a characteristic force and a characteristic magnetic stress by considering a very simple model of a FF-MRF. We find that the FEM model developed for FF-MRFs on the basis of the MM approximation gives reasonably good results especially for low and saturation magnetic field regimes. (C) 2018 The Society of Rheology.
机译:在这项工作中,预先用各种体积分数的纳米磁铁矿(PHI)和千分尺尺寸铁颗粒(PHI(FE))的各种体积分数测量的屈服应力(FF-MRF),用于各种磁场(b),从新的角度进一步调查。为常规磁流变学(MR)悬浮液开发的平均磁化(MM)近似延伸到FF-MRFS,并且通过使用FF-MRF悬浮液中的平均铁颗粒磁化来限定和确定特征磁应力。因此,我们通过使用单个变量,特征磁力应力与特征磁应力与特征磁应力的流变源曲线产生了静态屈服应力与特征磁力应力。这表明在文献中首次,在FF-MRF的情况下,浓缩磁化叠加。该主曲线可用于确定允许人获得FF-MRF的最佳组合物有用的是有用的。我们还发现,无论载体铁物流体中的磁铁矿纳米颗粒的体积分数如何,当铁体积分数接近phi(Fe)* = 30%出现磁流变行为的变化;这可能是由于从铁颗粒的链状结构到更复杂的结构过渡。另外,为了表明即使对于FF-MRF也可以使用MM近似,我们采用有限元方法(FEM)来计算特征力和特征磁力应力,通过考虑一个非常简单的FF模型 - MRF。我们发现基于MM近似为FF-MRFS开发的有限元模型提供了合理的良好结果,特别是对于低和饱和磁场制度。 (c)2018年流变学会。

著录项

  • 来源
    《Journal of Rheology》 |2018年第3期|共14页
  • 作者单位

    Romanian Acad Timisoara Branch Ctr Fundamental &

    Adv Tech Res Lab Magnet Fluids Timisoara 300223 Romania;

    West Univ Timisoara Fac Phys Timisoara 300223 Romania;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 流变学;
  • 关键词

  • 入库时间 2022-08-20 10:10:16

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