Vorticity, circulation and rotational flow

Vorticity as twice the local angular velocity, rotational versus irrotational flow, circulation and Stokes' theorem, forced, free and Rankine vortices, Kelvin and Helmholtz theorems and Kutta–Joukowski lift.

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Why it matters

Lift on a wing exists because of circulation around it, wing-tip vortices and wake turbulence come from shed vorticity, and the decision to use potential flow (and Bernoulli across streamlines) depends on whether the flow is irrotational. Vorticity and circulation are therefore the link between basic kinematics and aerodynamics.

Key ideas

Motion of a fluid element. A small fluid element can translate, rotate, stretch (linear strain) and shear (angular strain). Rotation is measured by the average angular velocity of two perpendicular line segments in the element.

Vorticity is the curl of velocity, ω = ∇ × V. It equals twice the local angular velocity of the fluid element. In 2-D flow in the x–y plane only the z-component exists: ω_z = ∂v/∂x − ∂u/∂y, positive for anticlockwise rotation.

Rotational and irrotational flow. A flow with ω = 0 everywhere is irrotational. Then a velocity potential φ exists with V = ∇φ, and Bernoulli's constant is the same on all streamlines (for steady, inviscid, incompressible flow). Irrotational does not mean particles move in straight lines: in a free vortex particles move in circles yet do not spin about their own axes. Conversely, a simple shear flow u = ky has straight streamlines but is rotational.

Where vorticity comes from. Viscous no-slip at walls generates vorticity, so boundary layers and wakes are rotational, while flow outside them that started from a uniform stream remains irrotational. Curved shocks and baroclinic effects (density and pressure gradients not aligned) also generate vorticity.

Circulation is the line integral of the tangential velocity around a closed curve, Γ = ∮V·dl, taken anticlockwise as positive. By Stokes' theorem it equals the flux of vorticity through any surface bounded by the curve, Γ = ∬ω·n dA. So circulation is the "total vorticity" enclosed.

Model vortices.

  • Forced vortex (solid-body rotation, V_θ = Ωr): uniform vorticity 2Ω, rotational.
  • Free vortex (V_θ = Γ/(2πr)): irrotational everywhere except the singular centre, where all the circulation is concentrated. Any loop enclosing the centre has circulation Γ; any loop not enclosing it has zero circulation.
  • Rankine vortex: forced core plus free-vortex outer region, a realistic model of tip vortices and tornadoes.

Kelvin's circulation theorem. For an inviscid, barotropic fluid (ρ a function of p only) with conservative body forces, the circulation around a closed curve moving with the fluid stays constant. Consequence: when a wing starts from rest and develops circulation Γ around itself, an equal and opposite starting vortex is shed into the wake, so the total stays zero.

Helmholtz vortex theorems (same assumptions): vortex-line strength is constant along its length, and a vortex line cannot end in the fluid; it must close on itself or end on a boundary. This is why a wing's bound vortex turns into trailing tip vortices (horseshoe vortex model).

Kutta–Joukowski theorem. For a 2-D body in a uniform inviscid stream, the lift per unit span is L′ = ρU∞Γ, perpendicular to the free stream. The Kutta condition at a sharp trailing edge fixes Γ.

Formulas

ω = ∇ × V and in 2-D ω_z = ∂v/∂x − ∂u/∂y

  • ω: vorticity (s⁻¹); u, v: velocity components (m/s). Angular velocity of element = ω/2 (rad/s).

Γ = ∮ V·dl = ∬ ω·n dA

  • Γ: circulation (m²/s); dl: line element (m); dA: area element (m²).

V_θ = Ω·r (forced vortex, ω = 2Ω) and V_θ = Γ / (2π·r) (free vortex)

  • Ω: angular speed (rad/s); r: radius (m).

L′ = ρ·U∞·Γ

  • L′: lift per unit span (N/m); ρ: density (kg/m³); U∞: free-stream speed (m/s).

V = ∇φ exists only when ω = 0 (φ: velocity potential, m²/s).

Worked examples

Example 1 (standard): simple shear flow. Given: u = 4y, v = 0 (m/s, y in m). Find the vorticity and the circulation around the unit square 0 ≤ x ≤ 1, 0 ≤ y ≤ 1.

  1. ω_z = ∂v/∂x − ∂u/∂y = 0 − 4 = −4 s⁻¹ (clockwise rotation at 2 rad/s).
  2. Line integral anticlockwise: bottom (y = 0) u = 0, contributes 0; right side v = 0; top (y = 1), moving in −x: −∫u dx = −4 × 1 = −4; left side 0. Γ = −4 m²/s.
  3. Stokes check: ω_z × area = −4 × 1 = −4 m²/s. Answer: ω_z = −4 s⁻¹, Γ = −4 m²/s. The streamlines are straight yet the flow is rotational.

Example 2 (standard): forced and free vortex. (a) A tank rotates as a solid body at Ω = 10 rad/s. Circulation around a circle of r = 0.2 m: Γ = 2πr·V_θ = 2π × 0.2 × (10 × 0.2) = 2.513 m²/s. Check by Stokes: ω × πr² = 20 × π × 0.04 = 2.513 m²/s. (b) A free vortex has Γ = 2π m²/s. At r = 0.5 m, V_θ = Γ/(2πr) = 2π/(2π × 0.5) = 2 m/s. The circulation around any loop that encloses the centre is 2π m²/s; around a loop that excludes it, zero. Answers: (a) 2.51 m²/s (b) 2 m/s.

Example 3 (GATE level): lift from circulation. Given: a rectangular wing of span 10 m in a stream of 60 m/s, ρ = 1.225 kg/m³, with uniform bound circulation Γ = 20 m²/s (2-D estimate).

  1. L′ = ρ·U∞·Γ = 1.225 × 60 × 20 = 1470 N/m.
  2. L = L′ × b = 1470 × 10 = 14 700 N. Answer: L ≈ 14.7 kN (an upper estimate; tip vortices reduce real 3-D lift).

Common mistakes

  • Equating vorticity with angular velocity. Vorticity is twice the angular velocity.
  • Sign errors in ω_z = ∂v/∂x − ∂u/∂y (the order matters).
  • Assuming curved streamlines mean rotational flow (the free vortex is irrotational) or straight streamlines mean irrotational flow (shear flow is rotational).
  • Saying circulation is always zero in irrotational flow. It is zero around loops in a simply connected irrotational region, but a loop around a free vortex or a lifting aerofoil has non-zero circulation.
  • Applying Kelvin's theorem inside viscous boundary layers, where it does not hold.

For GATE AE

Expect: compute vorticity or angular velocity of a given 2-D field and decide whether it is irrotational; circulation around a rectangle or circle (directly or with Stokes' theorem); free-vortex and forced-vortex velocity and circulation; lift per unit span from L′ = ρU∞Γ; and conceptual questions on Kelvin's and Helmholtz's theorems, the starting vortex and the horseshoe vortex. Practise both the direct line integral and the Stokes shortcut.

Quick check

  1. For u = 2y, v = −2x, what is ω_z?
  2. What is the angular velocity of a fluid element if ω_z = 6 s⁻¹?
  3. Is the free vortex V_θ = C/r rotational or irrotational away from its centre?
  4. Find L′ for ρ = 1.225 kg/m³, U∞ = 50 m/s, Γ = 15 m²/s.

Answers: 1. −4 s⁻¹ 2. 3 rad/s 3. Irrotational 4. 918.75 N/m

Try answering each one aloud before you open it.

  1. 1.What is vorticity in fluid mechanics?Concept

    Vorticity is a measure of the local rotation in a fluid flow. It is a vector quantity that represents the tendency of fluid elements to spin. Mathematically, it is defined as the curl of the velocity field, often denoted by the symbol ω, where ω = ∇ × v, with v being the velocity vector.

  2. 2.Explain the concept of circulation in fluid mechanics.Concept

    Circulation is a scalar quantity that represents the total 'amount' of rotation or swirling strength of a fluid around a closed curve. It is defined as the line integral of the velocity field around a closed loop, given by Γ = ∮ v · dl, where v is the velocity vector and dl is an infinitesimal element of the loop.

  3. 3.What is the difference between rotational and irrotational flow?Concept

    In rotational flow, fluid particles have a non-zero vorticity, meaning they exhibit local rotation. In contrast, irrotational flow is characterized by zero vorticity, where fluid particles do not rotate about their own axes. Irrotational flow is often idealized and simplifies the analysis of fluid motion.

  4. 4.Why is vorticity important in understanding fluid dynamics?Application

    Vorticity is crucial for understanding the rotational behavior of fluid flows, which affects mixing, turbulence, and the stability of the flow. It helps in analyzing complex flow patterns and is essential in the study of phenomena like vortex formation and the dynamics of turbulent flows.

  5. 5.How does circulation relate to lift in aerodynamics?Application

    According to the Kutta-Joukowski theorem, the lift per unit span on an airfoil is directly proportional to the circulation around it. The theorem states that L' = ρVΓ, where L' is the lift per unit span, ρ is the fluid density, V is the free-stream velocity, and Γ is the circulation. This relationship is fundamental in understanding how wings generate lift.

  6. 6.What happens to vorticity in a viscous fluid over time?Application

    In a viscous fluid, vorticity tends to diffuse over time due to the effects of viscosity. This diffusion leads to the spreading and eventual dissipation of vortices. Viscosity acts as a damping mechanism, reducing the intensity of rotational motion and smoothing out velocity gradients.

  7. 7.Explain how the conservation of circulation is applied in fluid mechanics.Application

    The conservation of circulation, often referred to as Kelvin's circulation theorem, states that in an inviscid, barotropic fluid with conservative body forces, the circulation around a closed loop moving with the fluid remains constant over time. This principle is used to analyze the behavior of vortices and predict the evolution of flow patterns.

  8. 8.Calculate the vorticity of a two-dimensional velocity field given by v = (y, -x).Numerical

    To calculate the vorticity, we take the curl of the velocity field. For a 2D flow, vorticity ω = ∂v/∂x - ∂u/∂y. Here, u = y and v = -x. Thus, ω = ∂(-x)/∂x - ∂(y)/∂y = -1 - 1 = -2. The vorticity is -2 in the z-direction.

  9. 9.A circular loop of radius 0.5 m is placed in a fluid flow with a velocity field v = (2x, 3y). Calculate the circulation around the loop.Numerical

    The circulation Γ is given by the line integral Γ = ∮ v · dl. For a circular loop, we parameterize the loop as x = 0.5 cos(θ), y = 0.5 sin(θ). The velocity field becomes v = (2(0.5 cos(θ)), 3(0.5 sin(θ))). The differential length element dl = (-0.5 sin(θ), 0.5 cos(θ)) dθ. The dot product v · dl = (2(0.5 cos(θ)))(-0.5 sin(θ)) + (3(0.5 sin(θ)))(0.5 cos(θ)) = -0.5 sin(θ) cos(θ) + 0.75 sin(θ) cos(θ) = 0.25 sin(θ) cos(θ). Integrating from 0 to 2π, Γ = ∫ (0 to 2π) 0.25 sin(θ) cos(θ) dθ = 0, since the integral of sin(θ) cos(θ) over a full period is zero.

  10. 10.What role does vorticity play in the formation of tornadoes?Application

    Vorticity is a key factor in the formation and dynamics of tornadoes. It represents the rotation within the storm system, and the concentration of vorticity can lead to the development of a tornado. The stretching and tilting of vorticity lines in a thunderstorm can intensify the rotation, leading to the characteristic funnel shape of a tornado.

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