What is Stoke’s Law?
Stoke’s Law is a mathematical equation that expresses the settling velocities of the small spherical particles in a fluid medium. The law is derived considering the forces acting on a particular particle as it sinks through the liquid column under the influence of gravity. The force that retards a sphere moving through a viscous fluid is directly proportional to the velocity and the radius of the sphere, and the fluid’s viscosity.
Stoke’s Law Equation
Sir George G. Stokes, an English scientist, clearly expressed the viscous drag force F as:
| F=6πηrv |
Where r is the sphere radius, η is the fluid viscosity, and v is the sphere’s velocity.
Stoke’s Law Derivation
From Stoke’s Law viscosity equation, we know that viscous force acting on a sphere is directly proportional to the following parameters:
- the radius of the sphere
- coefficient of viscosity
- the velocity of the object
Mathematically, this is represented as
F ∝ η a r b v c
Now let us evaluate the values of a, b and c.
Substituting the proportionality sign with an equality sign, we get(1)
F = k η a r b v c
Here, k is the constant of proportionality which is a numerical value and has no dimensions.
Writing the dimensions of parameters on either side of equation (1), we get[MLT–2] = [ML–1T–1]a [L]b [LT-1]c
Simplifying the above equation, we get[MLT–2] = Ma ⋅ L–a+b+c ⋅ T–a–c (2)
According to classical mechanics, mass, length and time are independent entities.
Equating the superscripts of mass, length and time respectively from equation (2), we get
a = 1 (3)
–a + b + c = 1 (4)
–a –c = 2 or a + c = 2 (5)
Substituting (3) in (5), we get
1 + c = 2
c = 1 (6)
Substituting the value of (3) & (6) in (4), we get
–1 + b + 1 = 1
b = 1 (7)
Substituting the value of (3), (6) and (7) in (1), we get
F = k η r v
The value of k for a spherical body was experimentally obtained as
6 π
Therefore, the viscous force on a spherical body falling through a liquid is given by the equation.
F = 6 π η r v
Terminal Velocity Formula
In the case of raindrops, initially, it is due to the gravity that it accelerates. As the velocity increases, the retarding force also increases. Finally, when viscous force and the buoyant force is equal to the force due to gravity, the net force becomes zero, and so does the acceleration. The raindrop then falls with a constant velocity. Thus, in equilibrium, the terminal velocity vt is given by the equation
v t = 2 a 2 ( ρ − σ ) g /9 η
and
σ
are sphere and fluid mass densities, respectively.
From the equation above, we can infer that the terminal velocity depends on the square of the radius of the sphere and is inversely proportional to the viscosity of the medium.
Stoke’s Law Applications
Stokes’s law finds application in several areas such as:
- Settling of sediment in freshwater
- Measurement of the viscosity of fluids