The effect of shear flow on the rotational diffusion of a single axisymmetric particle

被引:25
作者
Leahy, Brian D. [1 ]
Koch, Donald L. [2 ]
Cohen, Itai [1 ]
机构
[1] Cornell Univ, Dept Phys, Ithaca, NY 14853 USA
[2] Cornell Univ, Dept Chem Engn & Biomol Engn, Ithaca, NY 14853 USA
基金
美国国家科学基金会;
关键词
colloids; rheology; suspensions; WEAK BROWNIAN ROTATIONS; SEMIDILUTE FIBER SUSPENSIONS; RIGID DUMBBELL SUSPENSIONS; TAYLOR DISPERSION; HYDRODYNAMIC INTERACTIONS; RHEOLOGICAL PROPERTIES; ELLIPSOIDAL PARTICLES; ELASTIC FLUIDS; VISCOUS-FLUID; STRESS GROWTH;
D O I
10.1017/jfm.2015.186
中图分类号
O3 [力学];
学科分类号
08 ; 0801 ;
摘要
Understanding the orientation dynamics of anisotropic colloidal particles is important for suspension rheology and particle self-assembly. However, even for the simplest case of dilute suspensions in shear flow, the orientation dynamics of non-spherical Brownian particles are poorly understood. Here we analytically calculate the time-dependent orientation distributions for non-spherical axisymmetric particles confined to rotate in the flow-gradient plane, in the limit of small but non-zero Brownian diffusivity. For continuous shear, despite the complicated dynamics arising from the particle rotations, we find a coordinate change that maps the orientation dynamics to a diffusion equation with a remarkably simple ratio of the enhanced rotary diffusivity to the zero shear diffusion: D-eff(r)/D-0(r) = (3/8)(p - 1/p)(2) + 1, where p is the particle aspect ratio. For oscillatory shear, the enhanced diffusion becomes orientation dependent and drastically alters the long-time orientation distributions. We describe a general method for solving the time-dependent oscillatory shear distributions and finding the effective diffusion constant. As an illustration, we use this method to solve for the diffusion and distributions in the case of triangle-wave oscillatory shear and find that they depend strongly on the strain amplitude and particle aspect ratio. These results provide new insight into the time-dependent rheology of suspensions of anisotropic particles. For continuous shear, we find two distinct diffusive time scales in the rheology that scale separately with aspect ratio p, as 1/D(0)(r)p(4) and as 1/D(0)(r)p(2) for p >> 1. For oscillatory shear flows, the intrinsic viscosity oscillates with the strain amplitude. Finally, we show the relevance of our results to real suspensions in which particles can rotate freely. Collectively, the interplay between shear-induced rotations and diffusion has rich structure and strong effects: for a particle with aspect ratio 10, the oscillatory shear intrinsic viscosity varies by a factor of approximate to 2 and the rotational diffusion by a factor of approximate to 40.
引用
收藏
页码:42 / 79
页数:38
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