Navier-Stokes Drain Vortex

Re:5.57e+4
Fr:9.51
Core Ø:32.0mm
Funnel Dip:40.0cm
3D Free-Surface Funnel & DrainageWebGL Orbit
Camera:
Left Drag: Orbit Camera | Scroll: Zoom | Center: Drain Aperture (z = -0.150m)
2D Velocity Vector Field & Core StreamlinesClick to Probe
Active Analytical Probe
Radius r: 6.0 cm
Total |u|: 14.90 m/s
Swirl u_θ: 9.28 m/s
Sink u_r: -10.59 m/s
Vorticity ω_z: 0.0 1/s
Surface Dip: 40.0 cm
Velocity Field |u| (m/s)
0.0Core Peak
Click/drag canvas to move analytical probe | Amber ring = Viscous Core boundary (Rc = 1.6cm)
Discharge Flow Rate (Q):1.20 L/s
Circulation Strength (Γ):3.50 m²/s
Kinematic Viscosity (ν):1.0e-5 m²/s
Vortex Model:Exact Solution

Navier-Stokes Dynamic Balance in Cylindrical Coordinates

Real-time evaluation at probe radius r = 6.0 cm

Core Radius Rc = 1.60 cm
Incompressible Navier-Stokes Equation:
ρ · [ ∂u/∂t + (u · )u ] = -p + μ ²u + ρ g
1. Radial Momentum Balance (r-direction):Click any term below to inspect
Inertial Convective Term:Centrifugal Acceleration (u_θ² / r)
1.44MN/m³

As fluid elements orbit the drain with tangential velocity u_θ, their inertia creates an apparent outward centrifugal acceleration. For a steady vortex, this outward push must be precisely countered by the inward pressure gradient directed toward the low-pressure drain eye.

Higher swirl circulation (Γ) exponentially amplifies this centrifugal force as 1/r³, creating the massive hollow air core seen in bath drains and ocean whirlpools.

Radial Velocity & Surface Funnel Distribution Profiles

Cross-section across radius r from drain center (0 to 45cm)

Swirl u_θ(r)
Sink |u_r(r)|
Funnel Dip z(r)
Core Rc
Rc = 1.6cmProbe r = 6.0cm0cm10cm20cm30cm40cm22.2m/s0
Click anywhere on chart to position the analytical inspection probePeak Swirl: 22.22 m/s at r ≈ Rc

Hydrodynamics of Bathtub & Drain Vortices

1. Conservation of Angular Momentum

As fluid parcels are sucked toward the center drain aperture, their radial distance r diminishes. Because angular momentum L = m · r · u_θ is conserved in inviscid flow, the swirl velocity u_θ increases sharply as 1/r.

2. Burgers-Rott Steady Navier-Stokes Solution

Real fluids have viscosity (μ > 0). Viscous shear diffuses momentum outward while radial sink flow advects it inward. The exact steady balance yields the Burgers-Rott vortex: a solid-body core (u_θ ∝ r) surrounded by potential decay (u_θ ∝ 1/r).

3. The Coriolis Myth vs Reality

In ordinary household sinks, Earth's Coriolis acceleration (2Ω sinφ ≈ 10⁻⁴ s⁻¹) is eclipsed by residual filling currents and basin geometry. Only in giant, meticulously settled tanks does a purely planetary Coriolis vortex emerge.