The Hagen-Poiseuille equation, or simply the Poiseuille equation,
describes the flow of a fluid with nonzero viscosity
through a cylindrical pipe: the fluid clings to the sides,
limiting the amount that can pass through per unit time.
Consider the Navier-Stokes equations
of an incompressible fluid with spatially uniform density ρ.
Assuming that the flow is steady ∂v/∂t=0,
and that gravity is negligible g=0, we get:
(v⋅∇)v=−ρ∇p+ν∇2v∇⋅v=0
Let the pipe have radius R, and be infinitely long and parallel to the z-axis.
We insert the ansatz v=e^zvz(r),
where e^z is the z-axis’ unit vector,
and we are assuming that the flow depends only on r, not on ϕ or z.
With this, ∇⋅v trivially vanishes,
and in the main equation multiplying out ρ yields this,
where η=ρν is the dynamic viscosity:
∇p=e^zη∇2vz
Because only e^z appears on the right-hand side,
only the z-component of ∇p can be nonzero.
However, vz(r) is a function of r, not z!
The left thus only depends on z, and the right only on r,
meaning that both sides must equal a constant,
which we call −G:
dzdp=−Gηr1drd(rdrdvz)=−G
The former equation for p(z) is easy to solve.
We get an integration constant p(0):
p(z)=p(0)−Gz
This gives meaning to G: it is the pressure gradient,
which for a pipe of length L
describes the pressure difference Δp=p(0)−p(L)
that is driving the fluid, i.e. G=Δp/L.
As for the latter equation for vz(r),
we start by integrating it once, introducing a constant A:
drd(rdrdvz)=−ηGr⟹drdvz=−2ηGr+rA
Integrating this one more time,
thereby introducing another constant B,
we arrive at:
vz=−4ηGr2+Alnr+B
The velocity must be finite at r=0, so we set A=0.
Furthermore, the Navier-Stokes equation’s no-slip condition
demands that vz=0 at the boundary r=R,
so B=GR2/(4η).
This brings us to the Poiseuille solution for vz(r):
vz(r)=4ηG(R2−r2)
How much fluid can pass through the pipe per unit time?
This is denoted by the volumetric flow rateQ,
which is the integral of vz over the circular cross-section:
We thus arrive at the main Hagen-Poiseuille equation,
which predicts Q for a given setup:
Q=8ηπGR4
Consequently, the average flow velocity ⟨vz⟩
is simply Q divided by the cross-sectional area:
⟨vz⟩=πR2Q=8ηGR2
The fluid’s viscous stickiness means it exerts a drag force D
on the pipe as it flows. For a pipe of length L and radius R,
we calculate D by multiplying the internal area 2πRL
by the shear stress−σzr on the wall
(i.e. the wall applies σzr, the fluid responds with −σzr):
G is an inconvenient quantity here, so we remove it
by substituting R2G=8η⟨vz⟩:
D=8πηL⟨vz⟩
Due to this drag, the pressure difference Δp=p(0)−p(L)
does work on the fluid at a rate P.
Since power equals force (i.e. pressure times area) times velocity:
P=2π∫0RΔpvz(r)rdr
Because Δp is independent of r,
we get the same integral we used to calculate Q.
Then, thanks to the fact that Δp=GL
and Q=πR2⟨vz⟩, it follows that:
P=ΔpQ=GLπR2⟨vz⟩=D⟨vz⟩
In conclusion, the power P needed to drive a fluid
through the pipe at a rate Q is given by:
P=8πηL⟨vz⟩2=πR48ηLQ2
References
B. Lautrup,
Physics of continuous matter: exotic and everyday phenomena in the macroscopic world, 2nd edition,
CRC Press.