An electromagnetic wave is a propagating disturbance of the electric field and magnetic field obeying the Maxwell equations. In source-free vacuum its speed is
the speed of light. An electromagnetic wave can travel through vacuum: a conducting medium is unnecessary. A single traveling plane electromagnetic wave has mutually perpendicular electric field, magnetic field, and propagation direction. This statement applies to that wave; arbitrary near and far field configurations need not share these directions or the relation .
The visualization compares perpendicular components on a common scale: has the same units as . The curves are field values along space, rather than paths traced by particles. Their common phase moves toward , while the Poynting vector records the associated energy flux.
The electromagnetic wave equation gives a propagation law, while the full Maxwell equations additionally enforce the field directions and relative amplitudes. This is why solving an independent scalar wave equation for each component is insufficient to construct an electromagnetic wave. [ref].
For a uniform plane-wave beam of cross section , mean intensity is . Hence . A sinusoidal peak amplitude is times the rms amplitude. A Gaussian beam requires a stated waist or diameter convention before inferring its on-axis field from total power.
A closed rectangular perfect conductor cavity has discrete normal modes selected by zero tangential electric field at the walls. Each frequency has the displayed form. With all three indices positive there are two independent polarizations of an electromagnetic wave; modes with exactly one zero index have one, and those with two zero indices are absent. For example the family can have , independent of . It satisfies the wall conditions because is normal to the faces and tangential to the side walls. Omitting such zero-index families is harmless for leading bulk density of states, but changes the low-temperature physics of a thin cavity.
For a plane electromagnetic wave in a homogeneous, linear, lossless, isotropic medium with permittivity and magnetic permeability , the wave impedance relates the field amplitudes by . Its units are ohms. Impedance differences determine the normal-incidence amplitude Fresnel equations, and , with a common tangential electric-field axis.
The ratio of transmitted to incident normal time-averaged power for a specified wave and interface. Converting a field-amplitude transmission coefficient into power requires the appropriate impedances or flux normalization. For a displacement wave on a string with impedance , ; using an electric-field amplitude in electromagnetic waves instead gives the corresponding electromagnetic flux ratio. Amplitude squared alone is sufficient only when the relevant incident and transmitted normalizations agree.
The energy flux carried into a transmitted wave, integrated over the relevant cross section. The power transmission coefficient compares this with incident power. A displacement or field-amplitude transmission coefficient must be converted with the appropriate wave impedances; its squared modulus alone need not be the power fraction. This distinction applies both to electromagnetic waves and transverse string waves.
An electromagnetic waveguide confines an electromagnetic wave across its axis while allowing it to travel along the axis. Conducting walls or changes of refractive index select transverse normal modes: reproducible cross-sectional field patterns with their own longitudinal wavenumbers. A hollow metal pipe and an optical fiber are different realizations of this principle. Their usefulness is to deliver electromagnetic energy along a chosen route instead of letting it spread freely.
For a uniform vacuum-filled conducting guide, write a normal mode's axial and time dependence as . Here is angular frequency, is the longitudinal wavenumber, and is the transverse eigenvalue selected by the wall boundary conditions. The electromagnetic wave equation separates into
The geometry consumes part of the available squared wavenumber: when , this branch is an evanescent wave rather than a propagating normal mode. The waveguide cutoff frequency is therefore a property of a specified branch and geometry. A transverse electromagnetic mode in a suitable two-conductor geometry can have and no positive geometric cutoff. An optical fiber needs its own dielectric boundary conditions, rather than the metal-wall formulas below.
The rectangular electromagnetic waveguide makes these ideas explicit with a single sine profile. The scalar-potential conducting waveguide modes give a broader construction. At an open aperture, a confined field can radiate into the electromagnetic aperture angular spectrum; it need not remain one guided normal mode.
An optical waveguide confines an optical normal mode transversely while permitting longitudinal propagation. A higher-refractive index layer between lower-index layers provides a simple dielectric realization. In a double heterostructure laser, overlap of the guided field with the carrier-rich active layer improves useful optical gain.
A guided electromagnetic wave whose electric field has no component along the propagation axis. Its magnetic field can have a longitudinal component. In an empty perfectly conducting rectangular electromagnetic waveguide, transverse wave numbers determine a nonzero cutoff frequency. This differs from a transverse electromagnetic mode, in which both fields are transverse.
A dielectric slab surrounded by lower-index material confines waves with an oscillatory core profile and evanescent exterior tails. In an isotropic, nonmagnetic symmetric slab, an even transverse-electric field has core profile and matches to exponential tails through . The transverse constants also satisfy for vacuum exterior.
Set , , and . The circle in the first quadrant falls from , while rises from zero to its first pole. A unique first-branch intersection exists for every . It yields a nodeless even bound field. At exactly zero index contrast there is no confined mode; as contrast tends to zero from above its tail extends without bound.
For dependence , a Helmholtz equation generates transverse-magnetic fields , , , , for . The conducting wall requires a Dirichlet boundary condition on . A transverse-electric representation is , , , , with a Neumann boundary condition. These are families of modes, not a completeness assertion for multiply connected guides and their possible TEM fields.
For an aperture normal to , let be its tangential electric field traces extended by zero outside the aperture. With the outgoing branch of , the Weyl plane-wave representation and the curl aperture integral give a spectrum proportional to . Each wave is transverse to . The longitudinal electric component is regenerated by oblique diffraction even when it vanishes at the input. For and a unit prefactor on the stated curl integral, the spectrum has an overall factor ; a doubled half-space Green kernel gives factor one. The normalization must follow the chosen Green kernel and equivalent-current convention.
Take a straight hollow rectangular electromagnetic waveguide with vacuum interior , and axis , where . Its four walls are ideal perfect conductors. The time-dependent Maxwell equations require zero tangential electric field and zero normal oscillating magnetic field at these walls. Real metal has finite electrical conductivity, so real guides lose electromagnetic energy by Joule heating; the perfect-wall model isolates confinement and wave dispersion from that loss.
The simplest propagating transverse electric mode of a rectangular waveguide is . “Transverse electric” means , not that the magnetic field is also wholly transverse. With real peak scale , its complex amplitudes, including the common axial factor, can be written
The physical fields are the real parts after multiplication by . In particular, is zero at , maximal at , and independent of . At it is normal to the metal, so it need not vanish there. The electric field crosses the narrow gap, while its strength varies across the broad dimension.
Figure 1.
Original vacuum-filled rectangular guide: the TE10 electric-field profile across a 30 mm by 12 mm cross-section
. The arrows show the electric field at an axial plane and time where its common wave phase factor is positive; their length follows . They are field directions, not particle trajectories. The profile is uniform along and vanishes at the side walls. The guide axis points out of the cross-section. All dimensions and the operating frequency are chosen model values. Details.
For an original example choose , and , where . With , this gives
Here is vacuum wavelength and is guided wavelength. The next cutoff is at ; starts at . Thus only can propagate at the chosen frequency, although a source or discontinuity can additionally excite local evanescent waves. These are calculated values, not specifications or measurements of a commercial guide.
In a hollow rectangular electromagnetic waveguide with perfect conductor walls and axis , a transverse magnetic polarization has and a nonzero longitudinal electric field . The wall boundary conditions impose around the transverse rectangle. Separation of variables therefore gives , with . Setting either index to zero makes the entire field vanish. Thus there is no or branch. The transverse eigenvalue is , with dispersion relation . This exclusion is specific to this geometry and these boundary conditions.
The waveguide cutoff frequency separates oscillatory axial propagation from exponential decay for a particular normal mode. For the vacuum-filled rectangular electromagnetic waveguide, the dispersion relation is
For a transverse electric mode of a rectangular waveguide, are nonnegative integers but not both zero. For a mode with and nonzero , both indices must be positive. The lowest cutoff for is consequently , or ordinary frequency .
A square cross-section instead gives equal and cutoffs. The absence of a transverse electromagnetic mode is specific to this hollow pipe, rather than all electromagnetic waveguides.[ref]
For , choose real for propagation toward . For , a field decaying into a semi-infinite guide has
A finite section can contain both growing and decaying axial solutions set by its two ends; the single decaying solution is not a complete finite-section transmission calculation. At exact cutoff , the two axial solutions become a constant and a linear function of : there is no finite axial wavelength for a traveling sinusoid.
In the chosen guide at , the branch has . Its amplitude decay length is ; after , its normalized wave amplitude is . This is geometric evanescence even with ideal walls, not Joule heating. A single decaying branch has zero cycle-averaged axial Poynting vector: substituting makes a quarter-cycle out of phase with . Coupling across a finite section requires the complete boundary-value solution.
Figure 1.
Original TE10 model: propagating dispersion above cutoff and spatial amplitude decay below cutoff
. The left panel uses and to plot . The secant slope is phase velocity divided by ; the tangent slope is group velocity divided by . The right panel is the single decaying branch at , not an experimental transmission curve or a curve for dissipated power. Details.
For a propagating branch of an ideal vacuum-filled rectangular electromagnetic waveguide, the phase velocity tracks constant wave phase along the axis, whereas the group velocity describes a sufficiently narrow, weakly distorted wave packet. Using gives
Thus , , and . Differentiating the dispersion relation proves the second formula; dividing it by proves the first. This is the same mathematical structure as Klein-Gordon packet velocities. In the stipulated example,
Over , the corresponding narrow-envelope delay is , approximately . Timing a carrier wave crest would give ; it does not time the arrival of a newly introduced message.
There is an independent energy check. For the forward fields, the average axial Poynting vector is . Integrating across the guide gives average power and average electromagnetic energy per unit length :
The transverse sine and cosine squared each integrate to ; then makes the integrated electric and magnetic contributions to equal. The axial energy transport therefore agrees with the group velocity in this ideal model.
As , and ; exactly at cutoff is undefined. Strong wave dispersion close to cutoff also limits the narrow-packet approximation. Neither a large phase velocity nor a pulse peak establishes superluminal information velocity; front velocity asks a separate causal question. In a uniform filling with constant positive permittivity and magnetic permeability , replace by , giving . Frequency-dependent material response or significant loss requires differentiating the actual dispersion relation, so this product is not universal.
A transverse electric mode of a rectangular waveguide has while its axial magnetic field is generally nonzero. For time dependence and axial dependence , set . The Maxwell equations reconstruct the transverse components from :
The axial complex amplitude satisfies a transverse Helmholtz equation, . Zero tangential electric field at each perfect conductor wall becomes a Neumann boundary condition on . Separation of variables gives
The index counts half-periods across , and across . Either index can vanish, allowing ; both cannot vanish. Indeed a spatially constant axial oscillating magnetic field would give nonzero changing magnetic flux through the cross-section, whereas the line integral of tangential electric field around its metal boundary is zero. The integral form of Faraday's law excludes this candidate. Dividing the reconstruction formulas by would be invalid and cannot produce the separate transverse electromagnetic mode.
For , choose . The formulas recover exactly the , and in rectangular electromagnetic waveguide. In particular, the transverse magnetic field accompanies and ensures zero divergence; an oscillating longitudinal magnetic field on its own is not the guided solution.
Below the lowest waveguide cutoff frequency, the axial wave number of the mode is , with . For a real peak scale and time convention , , and . The electric field and magnetic field are in quadrature. A single decaying mode in a lossless semi-infinite guide consequently has zero time-averaged Poynting vector, although its instantaneous field stores energy.
The guided wavelength is the distance for a change of axial wave phase in a propagating normal mode. For the vacuum-filled rectangular electromagnetic waveguide,
for , with and . It exceeds the vacuum wavelength at the same frequency. This longer axial spacing is consistent with : multiplying by gives the phase velocity, not the group velocity.
Two oppositely traveling fields at the same frequency form a standing wave. For a perfect electric short at , the total electric field is proportional to , so successive axial electric nodes are separated by
Thus neighboring minima in a slotted line scan give half a guided wavelength. In the original , example, implies , not . Combined with the chosen , the inferred broad dimension is . Below cutoff, is imaginary and is not a physical periodic spacing.
MIT's documented slotted-line waveguide measurement shorts one end of a rectangular electromagnetic waveguide and excites it through a probe coupled by capacitance. A second such probe moves through a longitudinal slot, aligned with the wall electric current to reduce disturbance. Its output locates axial standing wave nulls. The book's standing-wave setup chooses a frequency above the first waveguide cutoff frequency and below higher-mode cutoffs. Lowering it below the first cutoff instead reveals spatial decay away from the source. The text supplies apparatus and an observable comparison, rather than a table of measured null positions.[ref]
The inference can be checked without assuming that detector output is proportional to electric field amplitude. At fixed measured frequency, record several minima at coordinates ; then estimate when the minima are consecutive. This uses positions alone. Compare the result with the guided wavelength prediction using independently measured and . The spacing above is a synthetic example, not a reading from the MIT apparatus.
Additional proposed controls are to keep probe insertion fixed, repeat the scan in both directions, recheck source frequency, and compare shallow probe settings for shifts in the minima. These test probe loading, mechanical backlash and drift. A deliberately reflecting termination supplies the standing wave; varying its position should translate the pattern without changing adjacent-null spacing in a uniform single-mode region. Source-adjacent evanescent waves, unintended reflections, additional propagating normal modes, detector noise and finite positional resolution can spoil that inference. A disappearing remote signal alone does not distinguish below-cutoff decay from loss or poor excitation, and a scan at one frequency does not measure a pulse's group velocity.
Relative to a propagation plane, transverse magnetic polarization has its magnetic field perpendicular to that plane. At a perfectly conducting corrugation its scalar magnetic component obeys a Neumann condition. It reduces to a scalar two-dimensional problem, but not to the Dirichlet problem for the transverse electric component.
Relative to a propagation plane, transverse electric polarization has its electric field perpendicular to that plane. For a conducting corrugation independent of the perpendicular coordinate, the scalar electric component obeys the Helmholtz equation with Dirichlet data at the metal surface.
With permittivity and permeability depending only on and time dependence , a transverse electric polarization obeys the displayed equation. Maxwell's equations give and . The latter satisfies . At normal incidence ; the nonzero magnetic component is .
The refractive index compares the phase velocity of light in a medium with the vacuum speed of light . For a transparent, uniform medium with isotropy and a positive-index propagation branch,
Here is the angular frequency, is the wavenumber, and is the speed of a surface of constant wave phase. The refractive index is a dimensionless quantity; it is a property of a specified material response at a specified frequency, rather than a universal number attached to the word “glass”. More general absorbing or negative-index media require the conventions discussed in refractive index and electromagnetic response. [ref]
For an original model example, choose at vacuum wavelength . The phase velocity is , the frequency is , and the medium wavelength is . These are stipulated model values, not measured properties of glass or water. A value at this single frequency does not determine a pulse's group velocity.
The usefulness of refractive index is that one measured response connects several different observations: Snell's law predicts refraction, optical path length predicts accumulated wave phase, and changes with frequency describe optical dispersion. Even at normal incidence, where a light ray does not bend, a changed refractive index changes wavelength and wave phase. The following comparison isolates that effect; the oblique geometry is developed in wavefront.
Figure 1.
Chosen refractive index : shorter wavelength, slower wavefronts, unchanged interface frequency
. The top panel compares equal normalized electric field components at one time on either side of a stationary interface at normal incidence. The lower panel tracks constant-wave phase crests in space and time. Curves represent incident and transmitted components, with their amplitudes normalized separately; reflected light and interface amplitude matching are omitted. The chosen single-frequency model contains no measured material data. Details.
The ratio compares vacuum light speed with the phase velocity at a specified frequency. In a dispersive material it differs from the group index; the Cherenkov radiation cone uses the phase index.
For a plane wave proportional to , the complex refractive index separates phase propagation from attenuation. In a nonmagnetic medium , so and . The passive branch has . If and , then and . These signs assume the convention for the complex permittivity.
The imaginary part of the complex refractive index makes wave amplitude decay as . Since intensity is proportional to amplitude squared, its absorption coefficient is .
The relative refractive index of medium two with respect to medium one is , using their absolute refractive indices at the same frequency. For transparent media with isotropy and positive refractive indices, Snell's law gives , with the angles measured from the interface normal. Thus a refraction measurement in air directly determines an index relative to air. Converting it to an absolute refractive index requires the refractive index of that air; replacing it by one is an approximation.
For a linear stationary interface, phase matching at a planar wave interface preserves frequency: the incident and transmitted electric fields must oscillate together at each boundary point. Their phase velocities can differ, so their wavelengths differ. Writing , the definitions give
This explains the compressed wavefront spacing in the figure without changing the time between crests at the interface. Moving interfaces or time-dependent material responses need not preserve frequency. [ref]
The notation labels refractive index by vacuum wavelength; it does not mean the wavelength inside the material. Dependence on , equivalently on frequency, is optical dispersion. The field driving the material induces oscillating electric charges; their emitted electromagnetic fields combine with the applied field to change the resulting wave phase. This collective response motivates refractive index, rather than a picture of independently delayed little pieces of light. [ref]
To distinguish three speeds, track a wavefront for phase velocity, a narrow wave envelope for group velocity, and the earliest newly introduced disturbance for front velocity. For a transparent differentiable propagation branch,
The denominator is the group refractive index. It describes envelope transit when loss and reshaping are small. It need not equal , and neither phase velocity nor a reshaped pulse peak generally measures signal arrival. The front velocity article explains the separate relativistic causality constraint and why a detector threshold is not an exact causal-front measurement.
For a uniform linear medium with isotropy and local constitutive response, Maxwell equations give . Here is permittivity and is magnetic permeability. Since , the relative permittivity and the relative magnetic permeability obey
If both responses are real and positive with negligible loss, and the ordinary positive-index branch is intended, then . If additionally , then . All these responses must be evaluated at the electromagnetic wave's frequency; a static relative permittivity cannot simply be substituted at an optical frequency. [ref]
With loss, use a complex index and explicitly fix the phase convention for complex amplitudes. For with , its wave amplitude has factor . A forward attenuating branch has , while its wave phase is controlled by . The complex relation alone leaves a choice of sign: the physical solution also needs causality and the appropriate radiation or decay condition. In negative-index media the physically selected real part can be negative. The positive square root is therefore not a universal rule for complex or negative-index media. Direction and polarization of an electromagnetic wave also matter in a plane wave in an anisotropic dielectric, for which one scalar index need not describe every propagation branch.
A prism minimum-deviation index measurement infers a transparent sample's relative refractive index from two angles: its known apex angle and the smallest deviation of a selected spectral line. A spectrometer combines a source and slit, a collimator, a rotating optical prism table, and a viewing optical telescope with an angular readout. The collimator supplies a nearly parallel beam; the optical telescope locates its emergent direction. This turns an otherwise difficult measurement of the phase velocity of light into a measurement of angles.
For the symmetric path through a uniform optical prism, with the same external medium at both faces and positive refractive indices,
The angles are measured from face normals. This is the minimum deviation relation, not a formula for an arbitrary prism orientation. An absolute refractive index additionally requires .
Figure 1.
Prism minimum-deviation index measurement: symmetric ray geometry and an independently calculated deviation minimum
. The original model chooses and at one fixed wavelength. The left panel marks face normals, equal internal angles, apex angle and deviation from the undeflected incident direction. The right panel calculates deviation versus incidence from two applications of Snell's law; the marked minimum is the only orientation used for the index inference. No points are experimental observations. Details.
For example, stipulate and . Then and . Substitution recovers . These synthetic values illustrate the geometry; they are not readings for the prism in the laboratory protocol below.
A Michigan State University teaching experiment uses a mercury lamp, slit, collimator, prism table and optical telescope, with a subsidiary angular scale read to one arcminute. First focus the optical telescope on a distant object; with the prism removed, align its crosshair to a narrow vertical slit image, focus the collimator, and establish the direct-beam zero. Insert and centre the prism. Select the green mercury spectral line, tabulated at , then rotate the prism while tracking its image with the optical telescope. Locate the turning point where continued prism rotation reverses the image motion, and read the deviation. Re-establish the minimum separately for each other spectral line. The protocol assumes ; that assumed apex angle is not an independently measured result. [ref]
For an uncertainty-aware implementation, repeat the turning-point search from both prism-rotation directions, recheck the direct-beam reference, and record individual readings before averaging. Independently determine or include its calibration uncertainty; record the chosen spectral line, sample identity, temperature and surrounding-air conditions. These are proposed controls deduced from the inference, not claimed additional instructions or results of that manual. Finite slit width, unresolved spectral lines, imperfect collimation, table tilt, angular calibration and sample nonuniformity can limit the inferred refractive index. One arcminute readout resolution alone does not establish one arcminute total measurement uncertainty. A single selected wavelength gives one index, not a measured optical dispersion curve.
A short geometric derivation uses and . Reversibility exchanges entrance and exit. At the symmetric stationary path, and ; applying Snell's law gives the displayed index relation. The plotted calculation checks that this stationary point is a minimum on the chosen transmitting branch. To assess local sensitivity, differentiate the inferred index using angles in radians:
This first-order relation exposes both angular contributions; it is not an instruction to add signed systematic errors as independent random errors. In the synthetic example, a deviation error of arcminute at fixed changes the inferred relative refractive index by approximately .
A transverse electric polarization with constant permeability and conserved transverse wavenumber satisfies , with and . Substitution reduces it to the Bessel equation. The profile is singular at , so each side requires its own boundary conditions.
In source-free vacuum the electric field and magnetic field obey
A brief derivation takes the curl of Faraday's law and substitutes the Ampère-Maxwell equation. The vector calculus identity , together with source-free Gauss's law, leaves . The same argument gives the magnetic field equation. The operator is the Laplacian, applied componentwise.
A monochromatic vacuum plane electromagnetic wave has phase , where is the wavevector, the angular frequency, and . Its field amplitudes obey and .
For the linear polarization and orientation in the visualization, choose a right-handed Cartesian coordinate system and put
Constant phase means , so propagation is along . The cross product fixes the positive Poynting vector. Both fields reverse together every half-period and are in phase. Reversing the propagation direction with the same electric orientation reverses the magnetic orientation.
These fields are spatially uniform across every transverse plane. An infinite plane electromagnetic wave is an idealization with infinite total electromagnetic energy; it is useful as a local approximation and as a building block for superposition. For frequency , and wavelength , independently of .
For a source-free plane electromagnetic wave in vacuum, let be its null propagation Lorentz four-vector. In signature , take , , and define the dual electromagnetic field tensor by , . Lower both indices with the Minkowski metric. Direct contraction gives
Both contractions vanish exactly when the transverse plane electromagnetic wave Maxwell equations hold. Being zero covectors, they remain zero in every inertial frame. Thus the transformed spatial wavevector is perpendicular to both transformed fields, even though the separate three-dimensional dot products are not themselves Lorentz scalars for arbitrary fields.
One contraction alone is insufficient without the other Maxwell equations. In particular, adding a magnetic field parallel to leaves unchanged but violates . Conversely the two scalar perpendicularity conditions alone do not impose the required relation between field strengths and directions.
The polarization of an electromagnetic wave describes the path traced by its transverse electric-field vector at a fixed point. A monochromatic wave may be linearly, circularly, or elliptically polarized; in vacuum it has two independent transverse polarization states.
For a vacuum plane electromagnetic wave, a Lorentz boost multiplies both transverse Jones vector amplitudes by the same positive Doppler factor when the basis is carried to the aberrated ray. Their ratio and phase difference therefore remain unchanged. All Stokes parameters gain the same squared factor, leaving normalized parameters, ellipse shape, handedness and degree of polarization unchanged. This does not mean the propagation direction or the components in an arbitrarily fixed pair of spatial axes remain unchanged.
The Faraday effect is magnetic field-induced circular birefringence: opposite circular polarizations acquire different wave phases, rotating transmitted linear polarization. For a transparent medium with isotropy before applying the magnetic field, in the linear magnetic-response regime at fixed vacuum wavelength and temperature ,
Here is the Verdet constant, is the material path length, and is the applied magnetic flux density component along the ray. This is the external bias, distinct from the oscillating magnetic field of the light itself. Michael Faraday discovered the effect in 1845.[ref]
Fix the sign before using the formula. On the forward path choose a right-handed Cartesian coordinate system, propagation along , and measure from toward for the electric field's oscillation line. Positive is counterclockwise in the -right, -up end view seen from , looking toward the source. Then and positive means positive rotation for positive . This convention differs from the clockwise-positive convention in optical rotation. A linear polarization line is unchanged by ; a measured orientation determines accumulated rotation only modulo , unless continuity selects a branch.
For uniform , the formula reduces to . Its appeal is that a weak change of refractive index becomes a visible change of orientation. Magnetic reversal measurement of Faraday rotation turns this into an inference of or of the magnetic field path integral. Faraday rotation on a round trip explains the directional behavior used by an optical isolator. In an astronomical cold plasma, the high-frequency limit instead leads to the rotation measure law ; that wavelength dependence is not a universal law for transparent solids.
The Verdet constant is the coefficient relating Faraday rotation to the magnetic flux density path integral. Its SI units are . It depends on material, wavelength and temperature; a sign requires the stated viewing convention.[ref]
The name commemorates Émile Verdet. For nonuniform material or temperature, use when the local scalar description remains valid. A single central magnetic field reading cannot generally replace this weighted integral. Strong additional linear birefringence or appreciable circular dichroism requires following the full polarization of an electromagnetic wave, rather than treating the output as merely a rotated line.
The factor of one half follows from superposition, without assigning ambiguous right/left names to the circular polarizations. Use the complex amplitude convention and fixed transverse unit vectors
For equal transmitted wave amplitudes, let the accumulated wave phases be and . Their sum is
The common wave phase sets the timing of the electric field oscillation; the real direction in parentheses sets its linear polarization. Opposite circular polarizations have changed their relative wave phase, yet their sum still oscillates along a line. Unequal transmitted wave amplitudes would generally give elliptical polarization instead.
In a uniform sample, with refractive indices and vacuum wavenumber , the phase difference is . Thus
The second relation identifies the small signed circular birefringence responsible for the rotation in this basis. Unlike a waveplate, whose separated modes have orthogonal linear polarizations, this ideal rotator has modes with opposite circular polarizations.
Figure 1.
Equal opposite circular polarizations acquire a relative wave phase and give Faraday rotation
. Original normalized model: common wave phase is removed, and the relative wave phase grows linearly with path fraction. The top panels add the real circular-component electric field vectors at the same time. Orange lines mark the resulting linear polarization direction. The lower panel compares relative wave phase with its half-angle rotation. No material measurements are plotted. Details.
Faraday rotation exhibits optical nonreciprocity: with the bias magnetic field held fixed, a retracing beam gains another rotation in the same laboratory sense. Natural optical activity in a reciprocal medium instead unwinds on retracing the path.[ref]
To reconcile this with the signed formula, retain the laboratory axes for comparing physical lines. For the backward ray choose a right-handed ray basis , , . Its magnetic flux density component is , so its local rotation increment is . But positive is negative laboratory : the backward increment is therefore in the laboratory orientation plot. Reversing the ray reverses both the longitudinal component and the basis used for its signed angle. Reversing only one creates the false prediction of cancellation.
In fixed laboratory transverse components, define the rotation matrix
For an ideal mirror at normal incidence that contributes the same complex amplitude factor to both transverse components, the round-trip map is . The common mirror factor does not change the oscillation line. A reciprocal natural rotator instead gives . This comparison assumes a retraced straight path and no additional polarization-changing elements.
For example, a chosen single-pass Faraday rotation produces a returned line at to the original laboratory axis. A chosen reciprocal natural rotator returns it to . The same addition makes an ideal optical isolator possible: polarizers at and surround a Faraday rotator. Forward light follows and passes. Returning light selected at reaches at the entrance polarizer and is rejected by Malus's law. Real transmission loss and incomplete extinction limit the isolation.
Consider an original model at fixed vacuum wavelength and temperature . Stipulate a transparent sample with Verdet constant , length , uniform adjustable , and a field-independent analyzer-zero offset . These are chosen values, not measured glass properties. On a continuously tracked small-angle branch,
Taking half the difference gives ; half the sum recovers . Hence . A field-reversal difference of is twice the single-field rotation, not that rotation itself. More generally this subtraction removes every contribution that is even under , provided the sample and apparatus remain otherwise matched.
Figure 1.
Chosen Faraday rotation model: reversing the magnetic field removes a constant angular offset
. Lines and marked values are exact synthetic predictions for , and offset . Left: observed orientation and its odd part. Right: normalized Malus's law curves at ; shifted maxima recover the three orientations. The analyzer line illustrates a signed intensity response. No points are experimental observations. Details.
An ideal polarimeter analyzer at laboratory angle reads normalized light intensity . Here is the light intensity immediately before the analyzer, separately calibrated for each condition. A scan locates the maximum at modulo . At , expansion about zero gives , with angles in radians. At crossed extinction, the response instead begins as and loses the sign near zero. The favorable slope follows directly by differentiating Malus's law; its sign reverses if the angular convention is reversed.
A William & Mary teaching experiment places a glass rod inside a solenoid. Align a polarized helium-neon laser through the rod's centre onto a photodiode after a rotatable polarimeter analyzer. First scan the analyzer from maximum to minimum transmission in steps and record detector voltage, establishing the angular response. A function generator and electronic amplifier then drive sinusoidal electric current through the solenoid; a multimeter measures the electric current and an oscilloscope reads the photodiode. Trigger the oscilloscope from the generator, remove the large constant detector component by AC coupling, and average repeated traces. Convert the small synchronized voltage modulation to rotation using the calibrated angular slope. The manual fits rotation against magnetic flux density, using its stated coil calibration and converting measured root mean square current to peak current. This is a specified laboratory procedure, rather than measured results reproduced here.[ref]
To test the inference, add matched zero-electric current readings before and after each reversal, hold the analyzer fixed during paired readings, and compare equal positive and negative electric currents. A blocked beam tests electrical pickup in the detector channel. These are proposed controls. Joule heating scales as current squared, so reversing electric current at equal magnitude helps separate an odd rotation from even heating effects; it does not remove drift between readings. Record temperature and allow repeatable settling. Changes in transmission, mechanical motion, stressed-glass birefringence and detector pickup can imitate a signal. Synchronized averaging suppresses unsynchronized noise, but cannot reject an artifact synchronized to the drive.
Quantitative extraction of the Verdet constant also needs the integral of magnetic flux density through the rod: a finite solenoid can have a nonuniform axial magnetic field. Use its calibrated path integral, or justify a uniform-field approximation; do not silently multiply a central field by the whole rod length. A signed reversal or phase-sensitive readout tests the part odd in applied magnetic field. Its agreement with the simple rotation law supports the model under these controls, rather than proving that every change of transmitted light intensity is Faraday rotation.
For the high-frequency Faraday effect in a cold plasma, the rotation measure is the coefficient in . It is a density-weighted line integral of the line-of-sight magnetic field; the coefficient depends on the units. A sign convention for the line of sight fixes its sign. Correlations across an extended source can constrain a foreground magnetic energy spectrum, subject to statistical assumptions.
For constant electron density, common path length , and a solenoidal isotropic spectral tensor, the rotation-measure correlation contains the window . As becomes large compared with the correlation length, this window acts as within the integral. The transverse projector then has component one, yielding the displayed two-dimensional Fourier transform. For finite , the windowed integral retains longitudinal modes and endpoint corrections. The method of using such rotation measure correlations to infer magnetic spectra is developed by Enßlin and Vogt.
Invert the two-dimensional Fourier transform in the long-path projection of a magnetic correlation, then perform the angular integration in polar coordinates. The angular integral is , a Bessel function of the first kind, giving the displayed Hankel transform with the stated Fourier-Hankel normalization for an isotropic spectrum. The result recovers the scalar tensor coefficient , whose shell-integrated magnetic energy spectrum has an additional factor .
A linear polarizer transmits one linear polarization and suppresses the orthogonal one. Two ideal crossed polarizers block light unless an intervening medium changes its polarization of an electromagnetic wave. A twisted nematic field effect uses this selection to convert field-driven reorientation into brightness modulation.
A prism polarizer associated with William Nicol. Its birefringent crystal arrangement selects one transmitted polarization; two such prisms can serve as the polarizer and analyser in a polariscope.
A polarizing element used to examine the polarization of incident light. Rotation converts that polarization information into an intensity variation, described by Malus's law for an incident linearly polarized beam and an ideal linear analyser.
A reciprocal optical circular polarizer can be assembled from a linear polarizer followed by a quarter-wave plate whose axes make to the transmitted linear state. Forward passage converts unpolarized light into circular light of half the ideal incident intensity. Reverse passage encounters the retarder first; it leaves unpolarized light unpolarized until the linear polarizer transmits half as linear light. Thus the one-pass intensity can be equal in both directions even though the outgoing polarization differs. Use a coherency matrix, not a single Jones vector, for unpolarized input.
The Stokes parameters describe intensity, two linear-polarization components and circular polarization. and depend on the chosen transverse basis. On the celestial sphere, transform as spin-two fields rather than as ordinary scalars.
A wave is linearly polarized when its oscillating electric field always lies along one fixed line. For a transverse plane wave, that line is perpendicular to the wavevector. Unlike circular polarization, the field oscillates along the line rather than rotating through directions.
An ideal linear polarizer transmits the fraction of incident linearly polarized light when its axis makes angle to the polarization. For a single photon, the corresponding conditional transmission probability is , by the Born rule; rejection has probability . The classical field calculation projects its electric-field amplitude onto the transmission direction and squares that amplitude to obtain intensity. This is a conditional probability given the incident polarization and is not automatically the joint probability of passing one analyzer and failing another.
An electromagnetic wave has circular polarization when its transverse electric field has constant magnitude and rotates once during each period. In complex-amplitude notation, two orthogonal components have equal magnitude and a relative phase of one quarter-cycle.
At the surface of a perfect conductor, the tangential electric field and normal magnetic field vanish. An incident plane electromagnetic wave is therefore accompanied by a reflected wave whose tangential electric field cancels the incident field at the surface.
The linear carrier acceleration equation and Faraday's law imply this conserved local quantity. Setting its initial value to zero gives the second London equation and London screening. An undamped response alone does not select that initial value, so it must not be used to infer expulsion of a pre-existing magnetic field for every magnetic history.[ref]
If a metal surface is and the incident field is independent of , Maxwell's equations separate into TE polarization and TM polarization. The metal condition that the tangential electric field vanish sets in the TE sector. In the TM sector , so the same condition gives . This explains why the TE problem agrees with scalar Dirichlet acoustics while the TM problem has different rough-surface boundary forcing.
At normal incidence, the reflected electric amplitude is the negative of the incident amplitude at the surface, while the reflected magnetic amplitude has the same sign. Their superposition forms a standing wave with an electric node and a magnetic antinode at the conductor.
Across an interface with unit normal from medium one to medium two, Maxwell equations imply , , , and . Here and are the free surface electric charge and electric current densities.
Without free surface charge or current, the tangential components of and and the normal components of and are continuous across an interface.
Equality of the boundary fields for every tangential position and time forces equal frequency and equal tangential wavevector for incident, reflected, and transmitted plane waves.
For refractive indices and ,
Total internal reflection occurs when a wave travels from higher to lower refractive index above the critical angle for total internal reflection, leaving no propagating transmitted plane electromagnetic wave normal to the interface.
At an infinite planar interface, total internal reflection returns all incident normal power in the reflected plane electromagnetic wave. Assume homogeneous dielectrics with isotropy, linearity, no dielectric loss, magnetic permeability , and positive real refractive indices . Above the critical angle for total internal reflection, both TE polarization and TM polarization have unit optical reflectance despite the external evanescent wave.[ref]
This makes total internal reflection useful for guiding light in an optical fiber: suitable internal incidence angles keep energy inside successive boundaries. Its more surprising feature is that perfect optical reflectance coexists with an external electric field. The evanescent field in total internal reflection can interact with a nearby object, as the frustrated total internal reflection experiment demonstrates.
For an original idealized example, choose , at vacuum wavelength . At angle of incidence , Snell law for electromagnetic waves gives an angle of refraction , so a transmitted light ray still emerges. At , its direction becomes tangent to the boundary. At , the proposed sine of a real angle of refraction would be : the transmitted wavevector must instead have an imaginary normal component. These are predictions for the stipulated media, not measured properties of a particular block.
Figure 1.
Constructed ray geometry just below, at, and above the critical angle for refractive indices 1.5 and 1; arrows indicate directions rather than relative powers
. Details.
A real semicircular-block experiment isolates this threshold. The University of Maryland laboratory instructions place a laser, motor-driven rotation stage and photodetector together; an aperture limits the detector voltage. The semicircular block is centered on the rotation axis, with the photodetector aligned along its flat face. The instructions identify a strong grazing-beam signal and a weaker signal just before the critical angle for total internal reflection. The readout is detector voltage versus stage angle. Retracing the incident laser beam identifies normal incidence for alignment.[ref]
The semicircular shape supplies a geometric control: a light ray passing radially through the curved face enters at normal incidence, avoiding additional entrance refraction. The weaker signal near the flat face locates a limiting angle of refraction; a vanishing remote-detector signal alone would not establish that the external electric field vanishes. Beam width and alignment limit angular resolution; no measured threshold or decay depth is supplied.[ref]
For refractive indices , the critical angle for total internal reflection satisfies . Above it, the transmitted normal wavenumber is imaginary and the transmitted field is an evanescent wave.
The critical angle for total internal reflection is the boundary between outgoing refraction and an evanescent wave, rather than an angle at which the external electric field abruptly disappears. Write and . At the threshold, Snell law for electromagnetic waves has , hence
Here inverse sine selects . For and , and . The threshold is independent of polarization of an electromagnetic wave under the stated assumptions.
A short proof using phase matching at a planar wave interface reveals all three cases at once. Choose a Cartesian coordinate system with boundary , incident medium , and transmitted medium . With vacuum wavenumber , the shared tangential wavevector component is . The dispersion relation in medium two gives
Below , choose the positive real square root for an outgoing plane electromagnetic wave. At , : there is a grazing wave, with zero normal average power but no exponential confinement in . Above , choose with , so the wave amplitude decays into the second half-space.
If , no nongrazing angle of incidence produces this threshold. As from below, ; as that ratio tends to zero, . These limits explain why a larger refractive index contrast permits confinement over a wider range of internal angles.
The evanescent field in total internal reflection oscillates and advances in wave phase along the boundary while its wave amplitude decays away from it. With the coordinates above and time dependence , a TE polarization has complex amplitude
The physical electric field is . The decaying sign excludes a field that grows without bound at . Dielectric-interface boundary conditions determine ; for nongrazing incidence it is generally nonzero.[ref]
Zero normal energy flux follows directly from Maxwell equations. The wavevector is ; the relation gives
Consequently, the cycle-averaged Poynting vector is
The electric field and are a quarter-cycle apart, so their product has zero cycle average. Tangential energy flux survives. This is a local calculation for the single decaying evanescent wave in the infinite second half-space.
To check reflected power independently, put . The existing transverse-electric Fresnel reflection coefficient becomes . Its numerator and denominator are complex conjugates, so , while supplies the surface electric field relative to the incident wave amplitude. Thus a unit optical reflectance does not require a zero transmitted field. The same normal power balance holds for TM polarization; its reflected wave phase generally differs from the TE polarization phase. A mixture can therefore change its polarization of an electromagnetic wave on reflection even though all normal incident power returns.
Define the amplitude evanescent penetration depth as the distance at which the electric field wave amplitude falls to of its surface value:
The squared-field envelope decays twice as fast:
The same normalized exponential decay describes the tangential average Poynting vector for the TE polarization above. An intensity penetration depth convention often means ; it must not be confused with amplitude depth or interpreted as outgoing normal light intensity.
For the stipulated , , and ,
At the normalized wave amplitude is approximately , and its squared envelope is approximately . At , these become and , respectively. The quantity inside the square root is dimensionless, so has inverse-length units and both depths have length units.
Figure 1.
Constructed evanescent-field model at 633 nm: amplitude and squared-field decay at 50 degrees, and their penetration depths as incidence increases above the critical angle
. Details.
The sharp angular dependence has a simple explanation. For with small and measured in radians, a first-order Taylor expansion gives
Thus as : exponential confinement disappears continuously. With fixed refractive indices, decreases as the angle of incidence increases and approaches as . This is a limit of the normalized depth; exactly grazing incidence supplies zero incident normal power. Real beam widths, angular spreads and optical dispersion matter when applying these ideal plane electromagnetic wave predictions near the threshold.
Frustrated total internal reflection occurs when a nearby second high-index dielectric couples to the evanescent field in total internal reflection, allowing power to cross a finite low-index gap. The extra boundary changes the dielectric-interface boundary conditions; the gap field need not be a single decaying evanescent wave. Consequently, the zero normal Poynting vector calculation for two infinite half-spaces does not forbid transmission in this three-medium geometry.
Harvard’s actual demonstration uses two right-angle glass prisms, a helium-neon laser, a small clamp and two perpendicular screens as detectors. The contact faces are cleaned and placed opposite each other, with the clamp protecting the corners. Increasing pressure narrows the intervening air film; the observed beam routing changes gradually from total internal reflection toward onward transmission. The broad-gap reflecting configuration supplies the comparison for the narrow-gap transmitting configuration. This is a qualitative readout: the page explicitly says the gap is not measured.[ref]
The inference is that the lower-index region can mediate electromagnetic energy transfer when another boundary is nearby. The demonstration does not determine a numerical evanescent penetration depth, resolve gap uniformity, or establish a three-layer transmission coefficient. For the constructed example, identifies the scale over which the isolated-interface field remains appreciable; substituting for a gap transmission fraction would omit the changed boundary fields and their interference. A quantitative gap calculation must solve the full Maxwell equations with both boundaries.
The Fresnel equations give reflection and transmission amplitudes for both transverse-electric and transverse-magnetic polarization of an electromagnetic wave at a planar interface. They follow by applying interface conditions for electromagnetic fields to incident, reflected and refracted plane electromagnetic waves.
The specular reflection of a wave at a planar dielectric interface with amplitudes described by the Fresnel equations. Below the critical angle, the reflected fraction is generally nonzero even when transmission is allowed; above the critical threshold, ideal lossless total internal reflection has unit reflected power. The reflected electric-field sign depends on polarization and the chosen basis conventions.
With one fixed tangential electric-field direction, normal-incidence reflection from impedance to gives . Using one fixed tangential magnetic-field direction reverses the reflected wave's sign, giving . Reversing the chosen reflected basis can produce the same change. The reflectance is invariant, but coherent amplitudes require a consistent convention throughout. Two internal reflections at identical opposite interfaces give the same round-trip product in either convention.
For a ray meeting an interface at nonzero incidence angle, the plane spanned by the incoming wavevector and the surface normal. transverse electric polarization has electric field perpendicular to this plane, while transverse magnetic polarization has electric field in it. At exact normal incidence, the surface normal and ray alone do not select a unique plane.
For reflection or refraction at a flat isotropic interface, p-polarization has its electric field in the incidence plane and perpendicular to its wavevector. At a lossless nonmagnetic dielectric interface, its reflected amplitude vanishes at Brewster's angle. This does not mean that its field is generally parallel to the interface surface.
For reflection or refraction at a flat isotropic interface, s-polarization has its electric field perpendicular to the plane containing the incident wavevector and interface normal. At an isotropic dielectric boundary it is an eigenpolarization of the Fresnel reflection problem. The label is relative to the specified interface, not an absolute direction in space.
For real wave impedances at normal incidence, the electric-field transmission coefficient gives transmitted power fraction . Reflection gives . Enforcing both tangential electric and magnetic boundary conditions gives and , which satisfy .
For an interface between two lossless, isotropic, nonmagnetic media with unequal refractive index values , Brewster's angle is the incidence angle at which the reflected amplitude in transverse magnetic polarization vanishes. The Fresnel equations and Snell's law give ; the reflected and transmitted rays are perpendicular there. The usual formula assumes equal magnetic permeabilities.
For sunlight reflected from a horizontal flat dielectric interface, incidence angle is measured from the vertical while solar elevation is measured from the horizontal. The Brewster condition therefore gives . Reflected light has its electric field perpendicular to the vertical incidence plane, so its surviving linear polarization is horizontal. This ideal result assumes real refractive indices, negligible absorption, nonmagnetic media and a smooth interface.
At a transparent nonmagnetic dielectric interface, the Fresnel reflection coefficients differ for s and p linear polarization. At Brewster incidence the reflected p amplitude vanishes and reflected unpolarized light becomes s polarized. For a horizontal reflecting surface this is horizontal glare. Away from Brewster incidence it is generally partial polarization. Refraction and internal reflection in droplets also select the two components differently, explaining polarization of rainbow light without a biological mechanism.
A vacuum ray incident normally on a dielectric moving parallel to its surface becomes oblique in the material rest frame, with . For a transparent nonmagnetic dielectric, the rest-frame Brewster angle satisfies , giving . The reflected electric field is perpendicular to the plane containing the ray and the velocity. A real refractive index is assumed; dispersion makes the condition implicit through the rest-frame frequency, and absorption generally removes exact extinction.
In the sharp planar, nonmagnetic ionosphere model with frequency above the plasma frequency, the refractive index is . From air, the Brewster angle satisfies . At that angle the reflected p-polarized wave vanishes, while s polarization retains a nonzero reflected component. A ground-to-ground single reflection from height spans . This is below the critical angle for total internal reflection for total internal reflection, which reflects both polarizations in this lossless isotropic model. The distinction diagnoses ordinary Brewster reflection rather than total internal reflection.
When the permeabilities agree, the signed reflected-to-incident electric-field ratio for polarization normal to the plane of incidence is
For incidence from lower to higher refractive index it never vanishes.
For equal permeabilities on the two sides of an interface, tangential-field continuity and Snell law for electromagnetic waves give
for consistently signed electric amplitudes normal to the plane of incidence.
For , , and a plane wave with electric polarization , the source-free Maxwell equations imply
If is an eigenvector of , then , the dispersion relation is , and the Poynting vector is parallel to .
In vacuum the Poynting vector
is the local energy flux, measured in watts per square metre. Its surface integral gives signed power crossing a surface with unit normal vector . Positive flux follows the chosen normal; for a closed surface the usual convention is outward. Power depends on the normal component and area, rather than just the field magnitude.
The Poynting vector applies to steady fields as well as electromagnetic waves. In a driven resistive electrical circuit, surrounding fields can carry energy into the conductor, where electrical work becomes Joule heating. This turns a circuit-level power balance into a spatial description of energy delivery. [ref].
The Poynting flux through an oriented surface is the normal component of the electromagnetic energy-flow vector. Integrating it over area gives outward electromagnetic power. A scale estimate of the form energy density times propagation speed must still specify the field and geometric regime.
Time-independent crossed electric and magnetic fields can carry a nonzero energy flux . A steady coaxial circuit is an example: radial electric and azimuthal magnetic fields carry energy axially from source to load. Static energy density does not imply zero flux.
For static electric fields and magnetic fields, Ampère's law and give . Stokes theorem on an oriented separating surface then gives
where each perfect conductor crossing it has constant electric potential and signed electric current . The line term is absent for a closed surface and must vanish in the limiting sense at infinity for a noncompact surface. Under that condition the incoming Poynting flux equals terminal power. If the signed electric currents sum to zero, the result is independent of the reference for electric potential.
For a resistive upper strip at with and an ideal lower strip at zero potential, the narrow-gap approximation gives and . The Poynting vector has both an axial flux and an upward flux into the lossy conductor. Axial power decreases by along the line, exactly equal to the integrated upper-surface flux. The ideal lower conductor receives no steady dissipation.
The Poynting theorem is the local energy balance of classical electromagnetism. For vacuum field laws, with current density , the electromagnetic energy per unit volume is
and
Thus a decrease in local electromagnetic energy can supply outward energy flux or work on electric charge. The term is power transferred to matter per unit volume. Its sign matters: positive values remove field energy, while negative values describe matter supplying the field. The magnetic part of the Lorentz force supplies no work term.
For a fixed volume , the divergence theorem gives the directly measurable balance
For example, entering a region with leaving and transferred to matter means stored electromagnetic energy increases at . In source-free vacuum only the boundary flux changes the stored energy; a nonzero local Poynting vector can still have zero net closed-surface flux.
A brief proof takes the dot product of the Ampère-Maxwell equation with and uses Faraday's law with . The identity turns the remaining terms into the divergence of the Poynting vector. [ref].
For a good conductor with surface electric-field peak amplitude , the surface impedance of a good conductor gives the displayed time-averaged Poynting vector component into the conductor. The factor one half in is required for peak phasors. Its loss with depth obeys . Electromagnetic energy becomes Joule heating locally; averaged field-energy storage has zero time derivative.
For circular plates of radius , separation , and a thin axial resistor , the quasistatic capacitance is . During discharge, . A circular Ampere-Maxwell law contour between the plates encloses wire current and opposing displacement current , giving . The electric field has magnitude , so the Poynting vector points radially inward with magnitude . Its flux through the cylindrical side is the displayed inward power. The field inside that cylinder releases per unit time; adding the incoming flux gives the resistor's full Joule heating rate . End fringing, wire radius and magnetic-energy corrections are neglected.
For a real linearly polarized monochromatic vacuum plane wave, the local Poynting vector is proportional to . Its flux through a closed surface generally oscillates at , with zero cycle average, although particular volume geometries can cancel it identically. For a circularly polarized plane wave of constant amplitude the Poynting vector is spatially and temporally constant, so the net flux through every closed surface is exactly zero. A nonzero constant local energy flux must not be confused with the net closed-surface flux.
In vacuum the electromagnetic energy density is
and the field energy in a region is .
In a linear isotropic nondispersive medium with time-independent permittivity and magnetic permeability , the stored electromagnetic energy per volume is . For a short derivation, the Maxwell equations in matter and the divergence identity for a cross product give . The constitutive relations turn the first two terms into , proving the Poynting theorem. Choose when the electric field and magnetic field both vanish. Dispersive or time-dependent material response requires a different accounting of stored energy.
In vacuum-permeability magnetohydrodynamics, the magnetic energy in a volume is . Its volume density equals the magnetic pressure.
For reversible quasistatic magnetic circuits with flux linkages , currents and mechanical coordinate , write . The Legendre transform obeys . Thus , while . In a linear reciprocal system numerically, but the variables held fixed in their force derivatives differ. The coenergy formulation includes the effect of electrical sources maintaining the currents; it avoids reversing the sign of the magnetic force by differentiating stored energy under the wrong constraint.
The shell-integrated magnetic energy spectrum distributes magnetic energy over wavenumbers. With a solenoidal isotropic spectral tensor normalized to and the inverse Fourier transform measure , one has . In Gaussian units, integrates to the energy density . A spectrum per unit mass or normalized to has different constant factors. Scale-local fluctuation estimates give proportional to at when the spectrum is normalized consistently.
For a single traveling vacuum plane electromagnetic wave, gives equal electric and magnetic contributions to electromagnetic energy:
For the fields with linear polarization along and magnetic orientation along specified above,
Angle brackets mean an average over one period at fixed position. The factor comes from averaging squared cosine; is the peak amplitude, whereas the root mean square field is . The equal energy contributions oscillate together, rather than trading energy as in an RLC circuit. [ref].
For , using and ,
A surface normal to therefore has average crossing power . This is incident power; the amount absorbed depends on the surface. Doubling the field amplitude quadruples the average flux.
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