Hostname: page-component-74656f9884-npj9w Total loading time: 0 Render date: 2026-11-10T21:22:33.702Z Has data issue: false hasContentIssue false

Hydrodynamic interactions between aerosol particles in the transition regime

Published online by Cambridge University Press:  19 September 2018

James Corson
Affiliation:
Department of Chemical and Biomolecular Engineering, University of Maryland, College Park, MD 20742, USA
G. W. Mulholland
Affiliation:
Department of Chemical and Biomolecular Engineering, University of Maryland, College Park, MD 20742, USA
M. R. Zachariah*
Affiliation:
Department of Chemical and Biomolecular Engineering, University of Maryland, College Park, MD 20742, USA Department of Chemistry and Biochemistry, University of Maryland, College Park, MD 20742, USA
*
†Email address for correspondence: mrz@umd.edu

Abstract

We present a method for calculating the hydrodynamic interactions between particles in the kinetic (or transition regime), characterized by non-negligible particle Knudsen numbers. Such particles are often present in aerosol systems. The method is based on our extended Kirkwood–Riseman theory (Corson et al., Phys. Rev. E, vol. 95 (1), 2017c, 013103), which accounts for interactions between spheres using the velocity field around a translating sphere as a function of Knudsen number. Results for the two-sphere problem at small Knudsen numbers are in good agreement with those obtained using Felderhof’s interaction actions for mixed slip-stick boundary conditions, which are accurate to order $r^{-7}$ (Felderhof, Physica A, vol. 89 (2), 1977, pp. 373–384). The strength of the interactions decreases with increasing Knudsen number. Results for two fractal aggregates demonstrate that one can apply a point force approach for interactions between particles in the transition regime; the interaction tensor is similar to the Oseen tensor for continuum flow. Using this point force approach, we present an analysis for the settling of an unbounded cloud of particles. Our analysis shows that for sufficiently high volume fractions and cloud radii, the cloud behaves as a gas droplet in continuum flow even when the individual particles are small relative to the mean free path of the gas. The method presented here can be applied in a Brownian dynamics simulation analogous to Stokesian dynamics to study the behaviour of a dense aerosol system.

Information

Type
JFM Papers
Copyright
© 2018 Cambridge University Press 
Figure 0

Figure 1. Two spheres in the parallel, anti-parallel and perpendicular flow configurations, and two ten-sphere aggregates with random orientations in parallel flow. The descriptor refers to the direction of movement relative to the line connecting the centre of mass of each particle.

Figure 1

Table 1. Speed of two spheres moving parallel to their line of centres, relative to the speed of isolated spheres subjected to the same external force. The EKR or Stokes tensor solution refers to $\unicode[STIX]{x1D648}_{ii}=\unicode[STIX]{x1D701}_{i,0}^{-1}$ and $\unicode[STIX]{x1D648}_{ij}=\unicode[STIX]{x1D701}_{i,0}^{-1}\unicode[STIX]{x1D651}(\boldsymbol{r})$, where $\unicode[STIX]{x1D651}(\boldsymbol{r})$ is defined in (2.6). The Felderhof tensors (Felderhof 1977) are accurate to order $r^{-7}$. The exact solution is given by Stimson & Jeffery (1926).

Figure 2

Table 2. Speed of two spheres moving anti-parallel to their line of centres, relative to the speed of isolated spheres subjected to the same external force. The exact solution is given by Brenner (1961).

Figure 3

Table 3. Speed of two spheres moving perpendicular to their line of centres, relative to the speed of isolated spheres subjected to the same external force. The exact solution is given by Goldman et al. (1966).

Figure 4

Figure 2. Speed of two spheres moving (a) parallel, (b) anti-parallel and (c) perpendicular to their line of centres, relative to the speed of isolated spheres subjected to the same external force. Results using the mobility tensors of Felderhof (1977) for mixed slip-stick boundary conditions are shown for comparison to the $Kn=0.1$ results. Note that for the Felderhof calculations we use a slip length of 0.9875 times the gas mean free path based on the best-estimate results of Loyalka (1990). Results in the free molecular limit are shown for comparison to the $Kn=10$ results for the parallel and perpendicular configurations. Solid lines represent our EKR results (2.9), while dashed lines represent point force results (2.13) for each Knudsen number.

Figure 5

Figure 3. Hydrodynamic force on an aggregate as a function of the distance between its centre of mass and the centre of mass of an identical aggregate. (a) Shows results for $N=10$, while (b) shows results for $N=1000$. The solid lines represent the full EKR results (2.9), while the dotted lines represent the point force results (2.13). The drag force is normalized by the drag on one of the aggregates in an infinite fluid, while the separation distance is presented as the number of effective sphere radii (i.e. the radius of a sphere experiencing drag force $F_{0}$) between the centres of mass of the particles.

Figure 6

Figure 4. Effects of orientation on the hydrodynamic force on one of two 500-sphere aggregates with primary sphere $Kn=2.7$ (sphere radius of 25 nm at room temperature), calculated using the EKR method. Results are presented as the ratio of the force on an aggregate for the specified separation distance to the force on the aggregate alone in an infinite fluid at a particular orientation. Each line represents a randomly chosen orientation for each aggregate in the two-aggregate system. (a) An aggregate with anisotropy $A_{31}=2.0$, and (b) an aggregate with $A_{31}=6.5$.

Figure 7

Figure 5. Average velocity for a cloud of spheres, normalized by the settling velocity of a single particle, $v_{s1}$. The velocity of a gas bubble having the same volume fraction and cloud radius is also shown. For $v_{s2}/v_{s1}\gg 1$, the average velocity approaches the gas bubble velocity, and the two curves coincide. For $v_{s2}/v_{s1}\ll 1$, the particles behave as if they are isolated.