Maxwell Stress Tensor and Field Forces

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Core Idea

The Maxwell stress tensor T_ij represents the flow of electromagnetic momentum. Its divergence gives the force density on matter, enabling calculation of electromagnetic pressure, tension, and forces between current-carrying conductors without explicit use of Lorentz force.

Explainer

The Lorentz force law f = ρE + J × B gives the force density on charges and currents directly. But integrating this over complex geometries is often difficult, especially when the charge/current distribution is itself a response to the field. The Maxwell stress tensor provides an equivalent but often more powerful method: instead of integrating over the sources, you integrate over a surface enclosing them. The force on everything inside the surface equals the flux of EM momentum through the surface — an approach analogous to using a Gaussian surface for flux instead of integrating over all charges.

The stress tensor T_ij has a concrete physical meaning: it is the flux of the i-th component of momentum in the j-th direction. The diagonal components represent pressure (force per unit area perpendicular to a surface), while the off-diagonal components represent shear stress (force per unit area parallel to a surface). Electric fields push along field lines (tension) and push outward perpendicular to them (pressure); magnetic fields similarly create tension along field lines and pressure perpendicular to them. The familiar result that field lines "want to be as short as possible" (tension) and "want to spread out sideways" (pressure) comes directly from the stress tensor's sign structure.

To find the force on an object, choose any closed surface S enclosing the object and evaluate F = ∮ T̄ · dA − ε₀μ₀ d/dt ∫S dV, where S = E × H is the Poynting vector. For static fields the time derivative vanishes and the force is purely the surface integral of the stress tensor. You can choose the surface however you like — close to the object's surface, or far away where the fields are simpler. This freedom to choose the Gaussian-like surface is what makes the method powerful.

Radiation pressure is a vivid application. A plane electromagnetic wave exerts pressure P = I/c on a perfectly absorbing surface (I = intensity). This follows directly from the Maxwell stress tensor: the wave carries momentum density g = S/c², and when absorbed the momentum is transferred to the surface. For a perfectly reflecting surface the pressure doubles to 2I/c because momentum reverses direction. This is not just a theoretical result — radiation pressure drives comet tails away from the sun, enables laser tweezers to trap cells, and is being exploited in proposed solar sail spacecraft. The Maxwell stress tensor is the machinery that makes these force calculations systematic.

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 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: KinematicsCircular Motion: Dynamics and Centripetal ForceMagnetic Dipole Moment from Current LoopsForce on Current-Carrying Conductors in Magnetic FieldsBiot-Savart LawAmpère's LawMagnetic Flux and Electromagnetic InductionFaraday's Law of Electromagnetic InductionLenz's LawInductance and InductorsEnergy Stored in Electric and Magnetic FieldsElectromagnetic Field Energy and ConservationPoynting Theorem and Energy ConservationPoynting Vector and Electromagnetic Energy FlowElectromagnetic Angular MomentumMomentum Density in Electromagnetic FieldsMaxwell Stress Tensor and Field Forces

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