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首页> 外文期刊>Journal of Physics. Condensed Matter >Transverse gradient diffusion in a polydisperse dilute suspension of magnetic spheres during sedimentation
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Transverse gradient diffusion in a polydisperse dilute suspension of magnetic spheres during sedimentation

机译:沉积过程中磁球多分散稀悬液中的横向梯度扩散

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In this work we investigate the pair interaction of magnetic particles in a dilute polydisperse sedimenting suspension. The suspension is composed of magnetic spherical forms of different radii and densities immersed in a Newtonian fluid, settling due to the gravity. When in close contact, the particles may exert on each other a magnetic force due to a permanent magnetization. We restrict our attention to dispersions of micromagnetic composite with negligible Brownian motion. The calculations of the relative particle trajectories are based on direct computations of the hydrodynamic interactions among rigid spheres in the regime of low particle Reynolds number. Depending on the relative importance of the interparticle forces and gravity, the collisions may result in aggregation or simply in a breaking of the particle relative trajectory time reversibility. After summing over all possible encounters, the transverse self-diffusion and down-gradient diffusion coefficients that describe the cross-flow migration of the particles are calculated. Our calculation shows first evidence and the significance of the diffusion process arising from magnetic interactions in dilute non-Brownian suspensions.
机译:在这项工作中,我们研究了稀释的多分散沉降悬浮液中磁性颗粒的配对相互作用。悬浮液由不同半径和密度的磁性球形形式浸入牛顿流体中,并由于重力而沉降。当紧密接触时,由于永久磁化,颗粒可能彼此施加磁力。我们将注意力集中在布朗运动可忽略的微磁复合材料的色散上。相对粒子轨迹的计算是基于在低粒子雷诺数状态下对刚性球体之间的水动力相互作用的直接计算。取决于粒子间力和重力的相对重要性,碰撞可能会导致聚集或仅导致粒子相对轨迹时间可逆性的破坏。在对所有可能的相遇进行求和之后,将计算出描述颗粒的错流迁移的横向自扩散系数和向下梯度扩散系数。我们的计算显示了稀有非布朗悬浮液中磁相互作用引起的扩散过程的初步证据和重要性。

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