Conservation of Angular Momentum

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angular-momentum conservation-laws torque

Core Idea

Angular momentum L = r × p (or L = Iω for rotation) is conserved in systems with zero net external torque. This explains why spinning ice skaters accelerate when pulling in their arms, and why rotating systems exhibit remarkable stability—it is the rotational analog of linear momentum conservation and equally fundamental.

Explainer

You already know from angular impulse-momentum that net torque causes angular momentum to change: ΣM = dL/dt. Conservation of angular momentum is simply the case where ΣM = 0, so dL/dt = 0, meaning L = constant. The logic mirrors linear momentum conservation exactly — just as a net force is required to change linear momentum, a net external torque is required to change angular momentum. If no torque acts, the rotational state of the system cannot change.

For a rigid body spinning about a fixed axis, this takes the compact form L = Iω = constant. The critical insight is that the moment of inertia I is not fixed — it depends on how mass is distributed relative to the spin axis. When an ice skater pulls their arms inward, they reduce their moment of inertia. Because Iω must stay constant, ω must increase proportionally. The total angular momentum (the product Iω) is conserved; the skater hasn't done any external work on angular momentum — they've merely redistributed mass to change I and ω simultaneously. This is why conservation calculations often proceed differently from torque-based ones: you don't need to know the internal forces, just the initial and final moments of inertia.

For particles and systems where the position vector matters, the vector form L = r × p becomes important. Angular momentum depends on both the speed of the particle *and* its perpendicular distance from the rotation axis (the moment arm). A planet in an elliptical orbit conserves angular momentum because gravity always points through the Sun (zero torque about the Sun), so it moves faster when close to the Sun (small r) and slower when far away (large r) — this is Kepler's second law as a direct consequence of angular momentum conservation.

Conservation of angular momentum also underlies gyroscopic stability: a spinning gyroscope resists changes to its orientation because any torque produces a change in the direction of L, not a change in its magnitude. A fast-spinning top doesn't fall because gravity's torque causes L to precess (rotate) rather than tip over. This counterintuitive behavior — where a torque produces motion perpendicular to itself — follows directly from the vector nature of L = r × p and the fact that torque is dL/dt. Recognizing when angular momentum is conserved (isolated system or zero net torque) and when it is not (net external torque present) is the fundamental skill this topic develops, and it is the rotational counterpart of the same judgment call you already make for linear momentum.

Practice Questions 5 questions

Prerequisite Chain

Counting to 10Counting to 20Understanding ZeroThe Number ZeroCounting to FiveOne-to-One CorrespondenceCombining Small Groups Within 5Addition Within 10Addition Within 20Two-Digit Addition Without RegroupingTwo-Digit Addition with RegroupingAddition Within 100Repeated Addition as MultiplicationMultiplication Facts Within 100Division as Equal SharingDivision as Grouping (Measurement Division)Division: Grouping (Repeated Subtraction) ModelDivision: Fair Sharing ModelDivision as Equal SharingDivision as GroupingBasic Division FactsDivision Facts Within 100Two-Digit by One-Digit DivisionDivision with RemaindersRemainders and Quotients in DivisionDivision Word ProblemsIntroduction to Long DivisionFactors and MultiplesPrime and Composite NumbersEquivalent FractionsRelating Fractions and DecimalsDecimal Place ValueReading and Writing DecimalsComparing and Ordering DecimalsAdding and Subtracting DecimalsMultiplying DecimalsDividing DecimalsDividing FractionsMixed Number ArithmeticOrder of OperationsInteger Order of OperationsVariable ExpressionsCombining Like TermsOne-Step EquationsTwo-Step EquationsSolving Multi-Step EquationsEquations with Variables on Both SidesAngle Pairs: Complementary, Supplementary, and VerticalParallel Lines and TransversalsCorresponding AnglesAlternate Interior AnglesTriangle Angle Sum TheoremExterior Angle TheoremTriangle Inequality TheoremSimilar Triangles: AA SimilaritySimilar Triangles: SSS and SAS SimilarityProportions in Similar TrianglesRight Triangle Trigonometry IntroductionTrigonometric Ratios ReviewRadian MeasureConverting Between Degrees and RadiansThe Unit CircleGraphing Sine and CosineGraphing Tangent and Reciprocal Trigonometric FunctionsDerivatives of Trigonometric FunctionsAntiderivativesIterated Integrals and Fubini's TheoremDouble Integrals in Cartesian CoordinatesDouble Integrals over Rectangular RegionsDouble Integrals in Polar CoordinatesDouble Integrals: Definition and SetupIterated Integrals and Fubini's TheoremDouble Integrals over Rectangular RegionsDouble Integrals over General RegionsApplications of Double Integrals: Area, Mass, and MomentsCenter of MassConservation of Linear MomentumElastic CollisionsInelastic CollisionsCoefficient of RestitutionCollision Analysis and Real-World ApplicationsTwo-Body Collisions in the Center-of-Mass FrameReduced Mass and Two-Body ProblemsKinematics in Two DimensionsProjectile MotionCircular Motion: KinematicsRotational KinematicsTorqueMoment of InertiaRotational Kinetic EnergyThe Work-Energy TheoremConservation of Mechanical EnergyWork-Energy Principle for ParticlesLinear Impulse-Momentum for ParticlesAngular Impulse and Momentum for Rigid BodiesConservation of Angular Momentum

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