Lorentz Force on Moving Charges

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magnetism forces charged particles

Core Idea

The force on a moving charged particle in a magnetic field is F = q(v × B), perpendicular to both velocity and field. This force does no work, changing only direction, not speed. The magnitude is F = qvB sin θ. This is the fundamental mechanism by which magnetic fields deflect moving charges.

Explainer

From your study of the cross product, you know that v × B produces a vector perpendicular to both v and B, with magnitude |v||B|sinθ where θ is the angle between them. The Lorentz magnetic force F = q(v × B) is exactly this cross product scaled by the charge q. The direction follows the right-hand rule: point fingers along v, curl toward B, and the thumb points in the direction of the force on a positive charge. For a negative charge, the force is reversed.

The most striking feature of the magnetic force is that it does no work. Work requires a force component along the direction of motion, but F = q(v × B) is always perpendicular to v by definition of the cross product. If no work is done, the kinetic energy (and therefore speed) cannot change. The magnetic force can only redirect a particle — it acts as a pure steering force. This has a remarkable consequence: a charged particle moving perpendicular to a uniform magnetic field undergoes uniform circular motion. The magnetic force provides the centripetal acceleration, giving mv²/r = qvB, so the orbital radius is r = mv/(qB). Faster particles and heavier particles orbit in larger circles; stronger fields produce tighter orbits.

The magnitude formula F = qvB sinθ tells you that the force is maximum when v ⊥ B (sinθ = 1) and zero when v ∥ B (sinθ = 0). A particle moving exactly parallel to the field experiences no magnetic force at all — only when it has a component of velocity perpendicular to B does the force appear. This selectivity makes the Lorentz force geometrically sensitive in ways that an electric force is not.

These principles underlie technologies from mass spectrometers (where radius r = mv/qB separates ions by mass-to-charge ratio) to particle accelerators (where magnetic fields bend high-energy beams around circular tracks) to the aurora borealis (where Earth's magnetic field funnels charged solar wind particles toward the poles). The combination of the electric and magnetic contributions, F = q(E + v × B), is the complete Lorentz force law, unifying how charged particles respond to all electromagnetic fields.

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 MomentsTriple Integrals in Cartesian CoordinatesTriple Integrals in Cylindrical and Spherical CoordinatesChange of Variables and the Jacobian DeterminantApplications of Triple Integrals: Volume and MassVector Fields and Their RepresentationsElectric FieldMagnetic FieldsLorentz Force on Moving Charges

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