Abstract
The trajectories of small heavy particles in a gravitational field, having fall speed in still
fluid V˜T and moving with velocity V˜ near fixed
line vortices with radius R˜v and circulation Γ˜,
are determined by a balance between the settling process and the centrifugal
effects of the particles' inertia. We show that the main characteristics are determined
by two parameters: the dimensionless ratio VT
= V˜TR˜v/Γ˜
and a new parameter (Fp) given by the ratio between the relaxation time of the particle
(t˜p) and the time
(Γ˜/V˜2T)
for the particle to move around a vortex when VT is of order unity or small.The average time ΔT˜ for particles to settle between two levels a distance
Y˜0 above and below the vortex (where
Y˜0 [Gt ] Γ˜/VT) and the average
vertical velocity of particles 〈Vy〉L along their
trajectories depends on the dimensionless parameters VT and
Fp. The bulk settling velocity
〈Vy〉B
= 2Y˜0/〈ΔT˜〉, where the average value of
〈ΔT˜〉 is taken over all initial particle positions of the upper level, is only equal to
〈V˜y〉L for small values of the effective volume
fraction within which the trajectories of the particles are distorted,
α = (Γ˜/V˜T)2/
Y˜20. It is shown here how
〈Vy〉B is related to
Δ&η;(X˜0), the difference between the vertical settling distances with and
without the vortex for particles starting on
(X˜0, Y˜0) and falling for a fixed period
Δt˜T [Gt ]
&Γtilde;/V˜2T;
〈V˜y〉B
= V˜T[1 − αD], where D
= ∫∞−∞(Δ&η;dX˜0/
(&Γtilde;/V˜T)2)
is the drift integral. The maximum value of 〈V˜〉B for any
constant value of VT occurs when
Fp = FpM ∼ 1
and the minimum when Fp = Fpm
> FpM, where typically
3 < Fpm < 5.Individual trajectories and the bulk quantities D and
〈Vy〉B have been calculated
analytically in two limits, first Fp → 0, finite VT,
and secondly VT [Gt ] 1. They have also been computed for the range
0 < Fp < 102, 0 < VT < 5
in the case of a Rankine vortex. The results of this study are consistent with experimental observations of the
pattern of particle motion and on how the fall speed of inertial particles in turbulent
flows (where the vorticity is concentrated in small regions) is typically up to 80%
greater than in still fluid for inertial particles (Fp ∼ 1) whose terminal velocity is
less than the root mean square of the fluid velocity, ũ′, and typically up to 20% less
for particles with a terminal velocity larger than ũ′.
If V˜T/ũ′ > 4 the differences are negligible.
Publisher
Cambridge University Press (CUP)
Subject
Mechanical Engineering,Mechanics of Materials,Condensed Matter Physics
Cited by
96 articles.
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