Maxwell Stress Tensor and Radiation Pressure

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stress momentum radiation-pressure

Core Idea

The Maxwell stress tensor T_ij encodes electromagnetic momentum density g = ε₀(E × B) and represents stresses exerted by fields. Radiation carries momentum and exerts pressure on absorbing surfaces. This provides a unified view of electromagnetic forces through momentum conservation.

Explainer

You already know from the Poynting vector that electromagnetic fields carry energy flowing at rate S = (1/μ₀)E × B per unit area. A natural question follows: if electromagnetic waves carry energy, do they also carry momentum? The answer is yes — and the Maxwell stress tensor is the mathematical tool that makes momentum conservation in electromagnetic systems precise in exactly the same way that Poynting's theorem made energy conservation precise.

The electromagnetic momentum density is g = ε₀(E × B) = S/c², meaning the momentum stored per unit volume in the field is proportional to the energy flux divided by c². This is not merely an analogy to mechanical momentum — it is real momentum that can be transferred to matter. When a light wave hits an absorbing surface, it deposits momentum, producing a measurable radiation pressure: P = I/c for a perfectly absorbing surface (intensity divided by the speed of light) and P = 2I/c for a perfect reflector. The force from sunlight on a square meter of surface is tiny (about 5 micronewtons), but it is real — solar sail spacecraft use it for propulsion.

The Maxwell stress tensor T_ij is the object that systematizes this. Just as a mechanical stress tensor tells you the force per unit area exerted across a surface in a material, T_ij tells you the flux of the i-th component of electromagnetic momentum in the j-th direction. The total electromagnetic force on all matter inside a volume V can be written as a surface integral of T over the boundary: F_i = ∮ T_ij dAⱼ − d/dt ∫ gᵢ dV. The first term is the momentum flowing in through the surface; the second term is the rate of change of momentum stored in the fields inside. In steady state, the surface integral alone gives the force — you can calculate the force on any object (conductor, dielectric, current loop) by integrating the stress tensor over a surface enclosing it, without needing to know the microscopic charge distribution.

The conceptual payoff is unification: mechanical force, radiation pressure, and electromagnetic momentum are all aspects of a single conservation law for total (mechanical + field) momentum. Just as energy is conserved locally by Poynting's theorem, momentum is conserved locally by the stress tensor formulation. This framework extends naturally to radiation from accelerating charges and to the momentum carried by photons in quantum electrodynamics, where each photon carries momentum p = ħk = E/c — the macroscopic radiation pressure is just the classical average of countless photon impacts.

Practice Questions 5 questions

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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 VacuumPoynting Vector and Electromagnetic Energy FlowMaxwell Stress Tensor and Radiation Pressure

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