George Stokes found (in 1845) the resistive force Fr on a tiny sphere sinking in a viscous
fluid as Fr = 6πηrv with (η, r) denoting (viscosity coefficient, sphere radius).
While falling through the viscous medium, the sphere encounters the frictional force Fr
of the surrounding fluid, the buoyant force B of that fluid and the weight w of the sphere
itself. The magnitude of the sphere's weight is w = ρgV equal to ρg(4/3)πr3.
By Archimedes' Principle, the magnitude of the buoyant force is the weight of the fluid
that the sphere displaces: B = ρfgV equal to ρfg(4/3)πr3 with ρf the fluid density.
When the fall begins, frictional resistance is zero since sphere
velocity is zero. The instantaneous rate of change of velocity with respect to time
(or acceleration) increases both sphere velocity and the resistive force Fr.
Upon reaching its maximum (or terminal) velocity vt, the resultant force
goes to zero with B and Fr balancing w.
Then write Fr + B = w as 6πηrvt + ρfg(4/3)πr3 = ρg(4/3)πr3.
Develop this last to obtain vt = g(4/3)πr3(ρ − ρf) ÷ 6πηr or 2gr2(ρ − ρf)/9η.
The density of the small ball is gained via 0.00315 kg ÷ [(4/3)π(0.0087m)3]
or 1141.994958 kg/m3.
Now determine 2gr2(ρ − ρf)/9η as 2(9.80665 m/s2)(0.0087m)2(1141.994958 − 869) kg/m3
divided by 9(0.075 N•s/m2) which crushes into 0.600399096 meter per second
(roughly 60 centimeters per second).