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Physics · Ch 9 — Mechanical Properties of Fluids

Stokes' Law and Terminal Velocity

9.4

Stokes' Law and Terminal Velocity

Stokes' law. When a small solid sphere moves at a constant, sufficiently slow speed through a viscous fluid that is otherwise at rest (or, equivalently, when a viscous fluid flows steadily past a stationary small sphere), the fluid exerts a retarding (drag) force on the sphere, opposing its motion. Sir George Gabriel Stokes showed, from a detailed analysis of viscous flow around a sphere, that for such slow motion this viscous drag force is given by:

F=6πηrvF = 6\pi\eta r v

where η\eta is the coefficient of viscosity of the fluid, rr is the radius of the sphere, and vv is the speed of the sphere relative to the fluid. This result, known as Stokes' law, shows that the viscous drag on a small sphere is directly proportional to its radius and to its speed -- doubling either the size of the sphere or its speed through the fluid exactly doubles the drag force resisting its motion.

Terminal velocity. Consider a small sphere of radius rr and density ρ\rho released from rest inside a large body of viscous fluid of density σ\sigma (with ρ>σ\rho > \sigma, so the sphere sinks). Three forces act on the sphere as it falls: its weight mg=43πr3ρgmg = \tfrac{4}{3}\pi r^3 \rho g, acting vertically downward; the buoyant force (Archimedes' upthrust) FB=43πr3σgF_B = \tfrac{4}{3}\pi r^3 \sigma g, acting vertically upward, equal to the weight of fluid displaced by the sphere; and the viscous drag F=6πηrvF = 6\pi\eta r v, given by Stokes' law, also acting vertically upward (opposing the sphere's downward motion) and growing larger as the sphere's speed vv increases.

At the very instant of release, v=0v = 0, so the viscous drag is zero and the sphere accelerates downward under the net force mg−FBmg - F_B. As the sphere speeds up, the (upward) viscous drag grows, so the net downward force -- and hence the sphere's acceleration -- steadily decreases. Eventually, the viscous drag grows large enough that the two upward forces, buoyancy and viscous drag, together exactly balance the sphere's weight. From this point on the net force on the sphere is zero, so it stops accelerating and falls, from then on, at a constant speed, called its terminal velocity, vtv_t.

Setting the net force to zero at terminal velocity:

mg=FB+F⟹43πr3ρg=43πr3σg+6πηrvtmg = F_B + F \qquad\Longrightarrow\qquad \frac{4}{3}\pi r^3 \rho g = \frac{4}{3}\pi r^3 \sigma g + 6\pi\eta r v_t

43πr3g(ρ−σ)=6πηrvt\frac{4}{3}\pi r^3 g(\rho - \sigma) = 6\pi\eta r v_t

Dividing both sides by 6πηr6\pi\eta r:

vt=4πr3g(ρ−σ)3×6πηr=2r2(ρ−σ)g9ηv_t = \frac{4\pi r^3 g (\rho-\sigma)}{3 \times 6\pi\eta r} = \frac{2r^2(\rho-\sigma)g}{9\eta} …

Figure 1Force balance on a sphere falling through a viscous fluid, reaching terminal velocity

What this figure shows. A single sphere of radius rr shown falling vertically downward through a tall column of viscous fluid, with three labelled force arrows drawn on it. A downward arrow, drawn from the sphere's centre, is labelled "Weight, mgmg". Two upward arrows are drawn alongside it: one labelled "Buoyant force (upthrust), FBF_B" and a second, growing arrow labelled "Viscous drag (Stokes' force), F=6πηrvF = 6\pi\eta r v". A small inset velocity-time graph beside the sphere shows the speed rising quickly at first and then levelling off into a horizontal straight line at the terminal velocity vtv_t, the point at which the two upward forces together exactly balance the downward weight, so the net force -- and hen …