Stokes number

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The Stokes number (Stk), named after George Gabriel Stokes, is a dimensionless number corresponding to the behavior of particles suspended in a fluid flow. Stokes number is defined as the ratio of the characteristic time of a particle (or droplet) to a characteristic time of the flow or of an obstacle, or

\mathrm{Stk} = \frac{\tau\,U_o}{d_c}

where \tau is the relaxation time of the particle (the time constant in the exponential decay of the particle velocity due to drag), U_o is the fluid velocity of the flow well away from the obstacle and d_c is the characteristic dimension of the obstacle (typically its diameter). Particles with low Stokes number follow fluid streamlines (perfect advection) whereas for large Stokes number, the particle's inertia dominates so that the particle will continue along its initial trajectory.

In case of Stokes flow, which is when the particle (or droplet) Reynolds number is low enough that the particle drag coefficient is inversely proportional to the Reynolds number itself the characteristic time of the particle can be defined as

Drag coefficient Cd for a sphere as a function of Reynolds number Re, as obtained from laboratory experiments. The solid line is for a sphere with a smooth surface, while the dashed line is for the case of a rough surface. The numbers along the line indicate several flow regimes and associated changes in the drag coefficient:
•2: attached flow (Stokes flow) and steady separated flow,
•3: separated unsteady flow, having a laminar flow boundary layer upstream of the separation, and producing a vortex street,
•4: separated unsteady flow with a laminar boundary layer at the upstream side, before flow separation, with downstream of the sphere a chaotic turbulent wake,
•5: post-critical separated flow, with a turbulent boundary layer.
\tau = \frac{\rho_d d_d^2}{18 \mu_g}

where \rho_d is the particle density, d_d is the particle diameter and \mu_g is the gas dynamic viscosity.[1]

In experimental fluid dynamics, the Stokes number is a measure of flow tracer fidelity in particle image velocimetry (PIV) experiments where very small particles are entrained in turbulent flows and optically observed to determine the speed and direction of fluid movement (also known as the velocity field of the fluid). For acceptable tracing accuracy, the particle response time should be faster than the smallest time scale of the flow. Smaller Stokes numbers represent better tracing accuracy; for \mathrm{Stk} \gg 1, particles will detach from a flow especially where the flow decelerates abruptly. For \mathrm{Stk} \ll1, particles follow fluid streamlines closely. If \mathrm{Stk} \ll 0.1, tracing accuracy errors are below 1%.[2]

Application to anisokinetic sampling of particles[edit]

For example, the selective capture of particles by an aligned, thin-walled circular nozzle is given by Belyaev and Levin[3] as:

c / c_0 = 1 + (u_{0} / u -1) \left(\frac{1}{1 + \mathrm{Stk} (2 + 0.617 u / u_{0})} - 1\right)

where c is particle concentration, u is speed, and the subscript 0 indicates conditions far upstream of the nozzle. The characteristic distance is the diameter of the nozzle. Here the Stokes number is calculated,

\mathrm{Stk} = \frac{u_{0} V_{s}}{d g}

where V_{s} is the particle's settling velocity, d is the sampling tubes inner diameter, and g is the acceleration of gravity.

References[edit]

  1. ^ Brennen, Christopher E. (2005). Fundamentals of multiphase flow (Reprint. ed.). Cambridge [u.a.]: Cambridge Univ. Press. ISBN 9780521848046. 
  2. ^ Cameron Tropea, Alexander Yarin, John Foss (ed.). Springer Handbook of Experimental Fluid Mechanics. Springer. ISBN 978-3-540-25141-5. 
  3. ^ Belyaev, SP; Levin, LM (1974). "Techniques for collection of representative aerosol samples". Aerosol Science (Pergammon Press) 5: 325–338. doi:10.1016/0021-8502(74)90130-X. 

See also[edit]