Plane Waves in Vacuum

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waves propagation vacuum

Core Idea

Plane wave solutions to the wave equation have the form E = E₀e^{i(k·r - ωt)} where ω = ck. The transverse nature of electromagnetic waves (E and B perpendicular to k and to each other) follows from Maxwell's equations. The dispersion relation ω = ck is exact in vacuum, independent of frequency.

Explainer

From the electromagnetic wave equation you know that both E and B satisfy ∇²E = (1/c²)∂²E/∂t², a linear PDE with constant coefficients. The most natural solutions are plane waves: fields of the form E = E₀ e^{i(k·r − ωt)}, where k is the wave vector pointing in the direction of propagation and ω is the angular frequency. These solutions are "plane" because at any fixed time, the field is identical everywhere on a plane perpendicular to k — the phase k·r − ωt is constant on such planes, which are the wavefronts. Every other solution — beams, pulses, standing waves — can be built as a superposition of plane waves through Fourier decomposition.

Substituting the plane wave ansatz into the wave equation immediately gives the dispersion relation: k² = ω²/c², or equivalently ω = ck. This tells you that all electromagnetic waves in vacuum travel at the same speed c, regardless of frequency. This non-dispersive character distinguishes vacuum from any material medium — in glass or water, different frequencies travel at different speeds (which is why prisms split white light into colors). The dispersion relation ω = ck is linear in k, which implies the group velocity and phase velocity are both equal to c, and a wave packet of any bandwidth travels without spreading.

The truly remarkable consequence comes from applying Gauss's law ∇·E = 0 to the plane wave. Taking the divergence of E = E₀ e^{i(k·r − ωt)}, the spatial derivative acts on the exponent to pull down a factor of ik, giving ik·E₀ = 0. This means k·E₀ = 0: the electric field is perpendicular to the propagation direction. The wave is transverse. Similarly, Gauss's law for magnetism (∇·B = 0) forces k·B = 0 — the magnetic field is also transverse. Faraday's law then fixes the relationship between E and B: B = (k × E)/ω = k̂ × E/c. The three vectors k, E, and B form a right-handed orthogonal triplet, with |B| = |E|/c. This geometry — not assumed but derived from Maxwell's equations — is the fundamental structure of all electromagnetic radiation.

The plane wave solution is also the foundation for understanding polarization: since E₀ can point in any direction perpendicular to k, there is a two-dimensional space of polarization states. Linearly polarized waves have E₀ pointing along a fixed direction; circularly polarized waves are superpositions of two orthogonal linear polarizations with a 90° phase offset. The energy flux carried by the wave — the Poynting vector S = E × H/μ₀ — points in the k direction with magnitude |S| = |E|²/(μ₀c) = c²ε₀|E|², averaging over a cycle to give the intensity. All of this rich structure follows from the single elegant fact that Maxwell's equations in vacuum admit plane wave solutions with ω = ck.

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 RepresentationsLine Integrals of Vector FieldsWork and CirculationLine Integrals of Scalar and Vector FunctionsFaraday's Law of Electromagnetic InductionDisplacement Current and Maxwell's EquationsMaxwell's Equations in Differential FormDerivation of the Electromagnetic Wave EquationPlane Waves in Vacuum

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