Conservation of Angular Momentum

Angular momentum is a fundamental quantity in rotational motion that describes how much rotational motion an object or system possesses. Just as linear momentum (p=mvp = mv) measures the 'quantity of motion' for objects moving in straight lines, angular momentum (L=IωL = I\omega) captures the rotational equivalent. The conservation of angular momentum is one of the most powerful principles in all of physics, stating that the total angular momentum of a system remains constant when no net external torque acts upon it. This conservation law arises directly from Newton's laws applied to rotational systems and is deeply connected to the symmetry of physical laws under rotation — a profound result first formalized by mathematician Emmy Noether. In everyday life, conservation of angular momentum explains why a spinning figure skater speeds up when pulling in their arms, why a gyroscope resists changes in orientation, and how planets maintain their orbital motion around the Sun. Understanding angular momentum conservation requires mastering a few key ideas: the definition of angular momentum for point masses and rigid bodies, the concept of moment of inertia as rotational inertia, and the role of external torque. Once these foundations are in place, the conservation principle becomes an extraordinarily useful tool for solving complex rotational problems without needing to know the details of internal forces acting within the system.

Key takeaways
  • Defining Angular Momentum
  • Connecting Torque to Angular Momentum
  • The Conservation Condition
  • Moment of Inertia Can Change
  • Rotational Kinetic Energy and Angular Momentum

Defining Angular Momentum

For a point mass mm moving with velocity v⃗\vec{v} at position r⃗\vec{r} from a reference point, angular momentum is defined as L⃗=r⃗×p⃗=r⃗×mv⃗\vec{L} = \vec{r} \times \vec{p} = \vec{r} \times m\vec{v}. The magnitude is L=rmvsin⁡θL = rmv\sin\theta, where θ\theta is the angle between r⃗\vec{r} and v⃗\vec{v}. For a rigid body rotating about a fixed axis, this simplifies to L=IωL = I\omega, where II is the moment of inertia and ω\omega is the angular velocity. The SI unit of angular momentum is kg·m²/s.

Connecting Torque to Angular Momentum

Newton's second law for rotation states that the net external torque equals the rate of change of angular momentum: τ⃗net=dL⃗dt\vec{\tau}_{net} = \frac{d\vec{L}}{dt}. This is the rotational analogue of F⃗net=dp⃗dt\vec{F}_{net} = \frac{d\vec{p}}{dt}. Notice that internal torques — forces that system parts exert on each other — always come in equal and opposite pairs (Newton's third law), so they cancel out when summing over the whole system. Only external torques can change the total angular momentum of a system.

The Conservation Condition

If the net external torque on a system is zero (τ⃗net=0\vec{\tau}_{net} = 0), then dL⃗dt=0\frac{d\vec{L}}{dt} = 0, which means L⃗=\vec{L} = constant. Written explicitly: L⃗i=L⃗f\vec{L}_i = \vec{L}_f, or Iiωi=IfωfI_i\omega_i = I_f\omega_f. This is the conservation of angular momentum. Note that τ⃗net=0\vec{\tau}_{net} = 0 can occur either because there are no external torques at all, or because all external torques cancel each other. The conservation applies to each component of L⃗\vec{L} independently along any axis where torque is absent.

Moment of Inertia Can Change

Unlike mass in linear momentum, the moment of inertia I=∑miri2I = \sum m_i r_i^2 of a system can change if the distribution of mass relative to the rotation axis changes. When a skater pulls their arms inward, II decreases (mass moves closer to the axis), so ω\omega must increase to keep L=IωL = I\omega constant. Quantitatively, if II halves, ω\omega doubles. This redistribution of rotational inertia is the mechanism behind many spectacular demonstrations of angular momentum conservation in sports, dance, and astronomy.

Rotational Kinetic Energy and Angular Momentum

An important subtlety: while angular momentum is conserved when τnet=0\tau_{net}=0, rotational kinetic energy Krot=L22IK_{rot} = \frac{L^2}{2I} is generally not conserved during a change in II. When a skater pulls in their arms, they do positive work against the centrifugal tendency of their arms, increasing KrotK_{rot}. Specifically, Krot=(Iω)22I=L22IK_{rot} = \frac{(I\omega)^2}{2I} = \frac{L^2}{2I}, so as II decreases with LL fixed, KrotK_{rot} increases. Energy is conserved overall — the extra kinetic energy comes from the internal work done by the skater's muscles.

The Key Equation

$$I_i \omega_i = I_f \omega_f
- **$I_i$** — Initial moment of inertia (kg\cdot m²): The rotational inertia of the system before the configuration change; depends on both mass distribution and rotation axis. - **$\omega_i$** — Initial angular velocity (rad/s): The rate of rotation of the system at the initial moment, measured in radians per second. - **$I_f$** — Final moment of inertia (kg\cdot m²): The rotational inertia of the system after the mass distribution has changed. - **$\omega_f$** — Final angular velocity (rad/s): The rate of rotation after the change in configuration; increases if $I$ decreases, decreases if $I$ increases. ## Worked Example **Problem.** A figure skater spins with her arms extended, giving her a moment of inertia of $I_i = 4.0$ kg\cdot m² and an angular velocity of $\omega_i = 2.0$ rad/s. She then pulls her arms tightly against her body, reducing her moment of inertia to $I_f = 1.0$ kg\cdot m². (a) What is her new angular velocity? (b) By what factor does her rotational kinetic energy change?
ωf=8.0 rad/s,KfKi=4.0\omega_f = 8.0 \text{ rad/s}, \quad \frac{K_f}{K_i} = 4.0
∗∗Answer.∗∗Hernewangularvelocityis8.0rad/s,andherrotationalkineticenergyincreasesbyafactorof4.**Answer.** Her new angular velocity is 8.0 rad/s, and her rotational kinetic energy increases by a factor of 4.
Figure
Diagram
Conservation of Angular Momentum: Figure SkaterArms ExtendedIᵈ= 4.0 kg·m²ωᵈ= 2.0 rad/sL = 8.0 kg·m²/sArms Pulled InIḟ= 1.0 kg·m²ωḟ= 8.0 rad/sL = 8.0 kg·m²/s→τ_net = 0slow spinfast spinL conserved
Origins · 1 minEmmy Noether and how this was discovered
EN
Emmy Noether
1882–1935 · German

Emmy Noether proved the landmark theorem (1915, published 1918) that bears her name: every differentiable symmetry of the action of a physical system corresponds to a conservation law. Rotational symmetry — the fact that the laws of physics are the same in all directions — directly implies conservation of angular momentum through Noether's theorem. This provided the deepest mathematical foundation for why angular momentum is conserved, unifying it with other conservation laws under a single elegant framework. Albert Einstein called Noether 'the most significant creative mathematical genius thus far produced,' yet she was denied an academic position for years solely because she was a woman. She eventually lectured at the University of Göttingen under a male colleague's name before finally receiving official recognition.

  • Moment of Inertia — Moment of inertia I=∑miri2I = \sum m_i r_i^2 is the rotational analogue of mass and appears directly in L=IωL = I\omega. Understanding how II depends on mass distribution is essential for applying angular momentum conservation.
  • Torque — Torque is the rotational analogue of force and is defined by τ⃗=r⃗×F⃗\vec{\tau} = \vec{r} \times \vec{F}. The condition for angular momentum conservation is precisely that the net external torque equals zero, making torque conceptually central to this topic.
  • Conservation of Linear Momentum — Linear momentum conservation (F⃗net=0⇒p⃗=\vec{F}_{net}=0 \Rightarrow \vec{p}= const) is the direct linear analogue. Comparing the two conservation laws deepens understanding of both and highlights the parallel structure of translational and rotational dynamics.
  • Rotational Kinetic Energy — Rotational KE (K=12Iω2=L22IK = \frac{1}{2}I\omega^2 = \frac{L^2}{2I}) is related to angular momentum but is not generally conserved when II changes. Distinguishing between conservation of LL and conservation of KrotK_{rot} is a key conceptual challenge in this topic.
  • Orbital Mechanics and Kepler's Laws — Kepler's second law — equal areas swept in equal times — is a direct consequence of angular momentum conservation for planets orbiting the Sun under a central (radial) gravitational force that exerts zero torque about the Sun.