In SI units, the Maxwell equations in vacuum with prescribed charge density and current density are
When and , take the curl of the third equation and substitute the fourth. Using the curl of the curl identity and gives the electromagnetic wave equation:
For example, , is a plane electromagnetic wave provided . The electric field, magnetic field and propagation direction are mutually perpendicular.
The Maxwell equations are linear, so the superposition principle applies to fields. However, the Poynting vector is quadratic:
One may add the average wave intensities only when the cross terms vanish under the actual detector average. For co-propagating plane electromagnetic waves of parallel linear polarization, averaging over optical cycles but potentially resolving the difference frequency gives
If the detector integrates for , the last term acquires , with sinc function convention , evaluated at the midpoint phase. Thus suppresses beats, and the infinite-time average adds the wave intensities exactly for distinct fixed frequencies. Random mutually uncorrelated wave phases also remove the cross terms in an ensemble average; orthogonal linear polarizations remove them for co-propagating waves in polarization-insensitive detection. Merely having different frequencies does not remove a resolved beat signal: two nearly equal frequencies with fixed relative wave phase are a concrete counterexample. For different propagation directions, the relevant addition is of average Poynting vectors, or their components through the chosen detector surface.
For a sinusoidal plane electromagnetic wave in vacuum, write the maximum electric field as . The magnetic field maximum is , so the cycle-averaged Poynting vector magnitude, or light intensity, is
Each photon carries energy , where is the Planck constant. Therefore the photon number flux density, namely the number per unit normal area per unit time, is
Multiplying by an illuminated normal area gives the photon arrival rate. Each absorbed photon transfers momentum at normal incidence, giving the radiation pressure on a perfectly absorbing surface
These are time-averaged quantities. At oblique angle of incidence , the normal radiation pressure is ; the simple displayed expression assumes normal incidence.
A pure quantum state is a unit ray in a complex Hilbert space: normalization fixes total probability, a common phase is unobservable, and superpositions retain relative phases. Observables are self-adjoint operators. For an ideal projective measurement with spectral projector , the Born rule gives and the Lüders rule gives conditional state . This preserves an eigenspace, not necessarily a unique vector when the outcome is degenerate. Between measurements, a closed system evolves unitarily according to . Composite systems use tensor products; quantum statistics additionally restrict identical-particle states. These are a framework supported by many experiments, not separate logical deductions from any one experiment.
In the photoelectric effect, monochromatic light illuminates a clean metal and a retarding potential measures the largest emitted electron kinetic energy. frequency controls the stopping energy, , while in the one-photon regime intensity mainly controls the emission rate. A threshold frequency and a stopping-energy slope support quantized energy exchange rather than gradual absorption of arbitrary classical-wave energy by each electron. Contact potentials, surface contamination, dark current and spectral impurities require controls. Robert Andrews Millikan tested the frequency–stopping-potential relation with careful surface and electrical control.[ref]
The Stern-Gerlach experiment sends a collimated neutral silver beam through an inhomogeneous magnetic field onto a detector. The force is approximately in an appropriate strong-field electronic description. Two resolved components rather than a continuous classical orientation spread support discrete angular-momentum projections. Field-off beam profiles and magnetic-gradient/beam-width controls distinguish splitting from ordinary broadening. In the modern description the silver ground electronic state has ; the 1922 experiment preceded the electron-spin interpretation. Ideal sequential analyzers along different axes illustrate incompatible observables and state preparation, but were not the original apparatus.[ref]
In the Davisson–Germer experiment, accelerated electrons scatter from a nickel single crystal and an angularly scanned collector measures the scattered intensity. Changing voltage and crystal orientation changes narrow diffraction maxima. The inferred wavelength agrees with , with nonrelativistic . vacuum, crystal cleaning, energy selection and background measurements matter: adsorbed surface gas can produce additional diffraction features. This supports matter-wave amplitudes and interference, with measured intensities related to their squared magnitude; it does not mean an electron must follow a classical orbit through the apparatus.[ref] Together these experiments motivate quantized outcomes, wave amplitudes and probabilistic measurement while leaving a distinction between observed evidence and the general postulates used to organize it.
temperature changes alter dimensions, resistances, refractive indices and offsets; gradients can generate thermoelectric voltages. Identify the dominant heat paths and the experiment's temperature coefficients before choosing insulation. Reduce convection with an enclosure or, where appropriate, vacuum; reduce conduction through supports and leads with suitable geometry and thermal anchoring; use thermal radiation shields and low-emissivity surfaces to reduce radiative exchange. vacuum alone does not remove heat conduction through wires or thermal radiation.
In first-order thermal isolation, a sample with heat capacity and thermal conductance to its surroundings obeys
Thermal mass and insulation suppress rapid fluctuations but only delay slow ambient drift: the zero-frequency gain remains one. Active temperature control, a stable reference environment, adequate equilibration time and an appropriate sensor location address long-term stability. Self-heating produces a steady offset ; increasing insulation can worsen that offset and settling time. Check temperature gradients rather than relying on a remote thermometer.
Match materials or use differential/reference measurements to reduce expansion and resistance drift; keep dissimilar-metal junctions isothermal to suppress thermoelectric offsets. Log temperature alongside the signal and deliberately vary environmental temperature to measure residual coupling, using a physically justified correction with uncertainty. Interleave calibrations and allow equilibration after changing power. Feedback must remain stable, and heater/sensor electronics should not introduce electrical interference into the measurement.
Quantum tunnelling is supported by transport and decay through barriers that classical particles of the same energy cannot traverse. Three complementary examples are:
Together these test barrier penetration in nuclear decay, vacuum-gap transport and semiconductor transport. Their detailed currents depend on state supply and matching as well as the barrier transmission probability.
Thermal agitation in a resistor produces Johnson-Nyquist noise, even without an applied mean current. In the classical low-frequency regime, its one-sided open-circuit voltage spectrum is and its equivalent short-circuit current spectrum is . In an Effective noise bandwidth ,
For a matched load, available thermal noise power is . A resistor and load at the same temperature exchange noise power without a net heat flow.
Cooling reduces the rms amplitude as if Electrical resistance and bandwidth remain fixed. A cryogenic bath or refrigerator, thermal anchoring and controlled heat input can maintain a steady low temperature. Radiation shields, an insulating vacuum, thermally anchored leads and limited measurement dissipation reduce heat leaks and self-heating. Temperature sensing and stable feedback control reduce slow temperature-induced drift; keeping temperature constant does not remove microscopic thermal fluctuations.
Figure 1.
At fixed resistance and bandwidth, thermal-noise power scales with temperature and rms amplitude with its square root
. Source. Details.
Bandwidth restriction, suitable impedance and a low-noise amplifier complement cooling. Warm leads, contacts and the amplifier can otherwise dominate the observed noise. At fixed mean current, shot noise is not generally reduced merely by cooling, and low-frequency excess noise need not follow the Johnson law. At frequencies with , quantum noise expressions replace the classical approximation.[ref]
A Michelson interferometer splits a collimated beam at a partially reflecting beam splitter. Two mutually perpendicular arms reflect from mirrors and recombine at the same beam splitter; the superposed returning beams produce interference fringes at the detector. Translate one mirror along its arm while holding the other fixed.
Figure 1.
Original Michelson geometry for measuring wavelength by counting fringes while one mirror moves
. Details.
If that mirror moves a measured distance , the round-trip optical path difference changes by in air, approximated as vacuum. Every change of one wavelength moves one complete bright-dark-bright fringe cycle past a fixed detector point. Count such cycles to obtain
Use a spectral line selected with a suitable optical filter, and count many interference fringes to reduce the fractional uncertainty of the distance and count. Keep the two arms within the source's optical coherence length and maintain overlap and alignment. If the vacuum wavelength is required for an arm filled with air of known refractive index , the corrected relation is at stable .
Draw the Fabry–Pérot etalon with parallel mirrors and an incident beam making internal angle with their normal. Every emerging transmitted contribution has undergone one more internal round trip than its predecessor.
Figure 1.
Successive transmitted paths and a common outgoing wavefront for a tilted beam in an air-gap etalon
. Details.
The extra internal path is , but successive contributions leave at laterally separated points, a distance apart. Comparing their phases on the same outgoing wavefront subtracts the path projection . Their net optical path difference in air is
Hence, in the reflection-phase convention implicit in the supplied transmission formula,
For a gap of refractive index , replace by and use the vacuum wavelength. Coating reflection phases can add a round-trip offset; the expression above assumes that offset is absorbed in the resonance order, or is zero modulo as in the stated ideal model.
A wave propagates an organized disturbance through space. What oscillates depends on the medium: displacement in a string or solid, pressure and density in a fluid, electric fields and magnetic fields in an electromagnetic wave, or a quantum wavefunction. The propagation law follows from the restoring mechanism, inertia and relevant boundary conditions. A common linear equation is , whose plane waves obey . The resulting phase velocity and group velocity coincide, so a narrow wave packet can travel without dispersive spreading. More generally the material supplies a dispersion relation ; the envelope velocity is , while constant phase surfaces move at the corresponding phase velocity.
Mechanical waves make the balance of restoring force and inertia particularly visible. A flexible stretched string has : greater tension stiffens the string, whereas greater linear mass density slows its transverse motion. Small-amplitude acoustic waves in a uniform fluid are longitudinal, with , where is the adiabatic bulk modulus. For an ideal gas, . Pressure changes in rapid sound oscillations are approximately adiabatic because little heat crosses a wavelength in one period. Fluids do not support ordinary bulk shear waves, whereas an elastic solid supports both longitudinal and transverse waves. In an isotropic solid their speeds are and , where is the shear modulus.
A material can be dispersive even when its equilibrium properties are uniform. In a liquid with a free surface, gravity and surface tension act as restoring mechanisms. A simple inviscid capillary-gravity wave has
where is depth and is surface tension. Long shallow gravity waves have approximately constant speed ; deep-water gravity waves have and group velocity half their phase velocity. Short capillary waves have a different dispersion dominated by surface tension. Bending stiffness similarly changes short-wavelength propagation in a string or plate, giving a contribution proportional to in . Different restoring mechanisms can therefore control different wavelength ranges of the same medium.
Electromagnetic waves propagate in vacuum without material displacement, because Maxwell equations couple changing electric and magnetic fields. They are transverse and travel at . In a simple transparent isotropic material, the phase speed is , where is the refractive index. Real material polarization depends on frequency. A Lorentz oscillator model for bound charges explains why permittivity and refractive index become strongly frequency dependent near material resonances, accompanied by absorption. In a birefringent medium, different field polarizations have different propagation constants, permitting wave plates and mode-dependent delays. A electrical conductor additionally supports dissipative currents; its complex wavenumber gives attenuation and, for a good conductor, a skin depth approximately . Energy removed from the wave becomes heat rather than disappearing.
At an interface, frequency is conserved for stationary media, and tangential wave phase must match. These conditions give Snell's law for refraction and constrain reflected and transmitted directions. Amplitudes follow from continuity of the appropriate fields or mechanical forces. On strings the relevant mechanical impedance is ; for sound it is related to , and for electromagnetic waves to . A mismatch gives wave reflection, and a lossless boundary conserves the total incident, reflected and transmitted power. Multiple reflections can reinforce or cancel, as in a Fabry–Pérot etalon. Total internal reflection and other boundary conditions confine waves in waveguides. Transverse modes then become discrete, and even an otherwise nondispersive material develops longitudinal cutoffs and wave dispersion. A membrane strip, for example, obeys .
Propagation also involves transport and loss. The Poynting vector gives electromagnetic energy flux; mechanical energy transport is force or pressure times velocity, averaged over a cycle. Wave absorption, viscosity, electrical resistance and imperfect boundaries dissipate energy. Scattering redistributes energy into other directions and modes, while geometric spreading reduces local intensity without necessarily dissipating anything. These mechanisms should be distinguished when interpreting a decreasing measured amplitude. In strongly absorbing or rapidly varying dispersive regimes, the derivative called group velocity is not automatically the speed of a sharp signal front; pulse reshaping and the medium's causal response must be considered.
Finally, quantum matter waves illustrate how the same propagation mathematics can describe a different physical quantity. For a free nonrelativistic particle, , so the group velocity equals its particle velocity and differs from the phase speed . In a periodic crystal, Bloch's theorem replaces the free dispersion by energy bands. Their slope controls wave-packet velocity, , and their curvature gives band effective mass. Thus mechanical confinement, material response and microscopic periodicity all reshape propagation through their allowed modes and dispersion, while the physical interpretation of the wave and its transported quantities remains essential.
A bubble is a thin water layer surrounded by air. At a locally flat patch, let its thickness be , its refractive index be , and the internal angle of refraction be . The two principal reflected light contributions are the reflection at the first surface and the contribution that enters the layer, reflects at its second surface and leaves again. The first reflection, from lower to higher refractive index, introduces a phase shift; the second does not. Their optical path difference is , so their phase difference is, modulo ,
where is the vacuum wavelength. Constructive interference in reflected light therefore occurs approximately when
Destructive interference occurs at . In the weak-reflection approximation, the reflected light intensity at each wavelength is proportional to . This is a smooth spectral filter, with broad maxima and minima: it does not select three pure wavelengths corresponding to display primaries. Ordinary illumination contains many visible wavelengths, and the eye combines their remaining contributions through color vision. The result is a mixture of colours, often pastel or desaturated.
The layer thickness varies over the bubble because of drainage and flow; the bubble's curvature also changes the local angle of refraction and the viewed optical path difference. The spectral filter therefore changes continuously across the surface and in time. Very thin regions become dark because the two reflected contributions nearly cancel across the visible optical spectrum. Thin-film interference explains both the changing colours and this dark limit.
Figure 1.
Two reflected paths through a thin film and the broad spectral filtering that produces mixed colours
. Details.
The ray sketch shows a local patch and is not to scale. The plotted curves use a chosen constant at normal incidence and illustrative thicknesses; they show the spectral filter rather than calibrated perceived colours.
For a plane wave propagating along in vacuum, Maxwell equations give , with . Hence
Taking , the period average of the squared cosine is . Thus
The fields are in phase, so the travelling-wave energy flux never reverses. The peak amplitude convention is essential; using a root-mean-square electric field would remove the factor .
displacement current completes Ampère's law:
In vacuum . Taking the divergence and using gives , exactly the continuity equation. Without the added term a time-dependent charge distribution would contradict the curl equation.
A charging parallel-plate capacitor illustrates the physics. For plate area , , so the gap displacement current is , equal to the conduction current in its leads. An Ampère contour therefore gives the same magnetic circulation whether its spanning surface crosses the wire or the gap. No electrons have to cross an ideal vacuum gap. In matter, includes the polarization response as well as the vacuum term. Combined with Faraday induction, the displacement term permits source-free electromagnetic waves.
Since , a magnetic field can locally be represented by a magnetic vector potential,
It is not unique: leaves its curl unchanged. In magnetostatics, choose the Coulomb gauge . Ampère's law then gives in vacuum. For a localized steady current distribution with the usual decay condition,
Its curl gives the Biot–Savart field. For a uniform field, one convenient choice is . Stokes's theorem relates to magnetic flux through a spanning surface. In time-dependent electrodynamics, ; changing by requires to preserve the electric field. Gauge freedom simplifies calculation without changing the electromagnetic observables.
State a time convention before using complex response: take fields proportional to , with and for a passive wave entering the material. In a homogeneous Ohmic medium, Maxwell equations with give
The ohmic-conductor complex wavenumber describes both phase advance and amplitude decay. Real constant conductivity is only a low-frequency approximation. In the Drude model, gives
with a fixed positive ionic background and no additional bound-electron contribution in this simple model. The plasma frequency marks the inertial electron-response scale. More elaborate band structure, interband transitions and nonlocal transport limit this scalar treatment.[ref]
In the collisionless nonmagnetic limit, the dispersion relation is . For ,
A crest can move faster than without carrying a new signal faster than light. Below cutoff the ideal wave is evanescent, with penetration length ; it does not propagate as an ordinary real- bulk wave. Evanescence in the lossless limit is not Joule dissipation. Nonzero collision rate gives a dissipative conductivity and smooths this ideal cutoff picture.
For a good conductor with approximately real , the spatial branch becomes
A field amplitude falls as , while intensity falls as . The phase velocity is in this limit. Magnetic and electric amplitudes are not related by the vacuum ratio: with the chosen time convention. Its positive real part is the surface resistance. The local mean heating is , consistent with electromagnetic energy flowing into the metal. skin depth is an amplitude length; interpreting it as an intensity length gives a factor-of-two error.
A transmission-line mode propagates chiefly through the dielectric between conductors, even though finite metal conductivity causes loss at its boundaries. With per-length parameters , the telegrapher's equations give, for the same convention,
Writing a forward wave as , , gives . In the low-loss regime and , set to obtain
This low-loss transmission-line attenuation separates series conductor loss from dielectric leakage loss. Average forward power falls as . In the normal skin-effect regime, reduced conducting area makes the AC conductor resistance increase roughly as ; dielectric loss can supply a separate frequency dependence. Reflection from a mismatched termination changes delivered power without being, by itself, dissipation in the line.[ref]
To test loss, compare several lengths of otherwise identical line with matched terminations, calibrate connectors and incident/reflected power, and monitor temperature. Separate amplitude attenuation from phase delay and from standing-wave minima. Bulk penetration, line attenuation and dielectric propagation speed are related electromagnetic quantities but describe different experimental geometries.
Figure 1.
Conducting-wave propagation
. Chosen dispersion and decay models. Details.
In charge- and current-free vacuum, Maxwell equations reduce to
Taking a curl and using gives
and the same wave equation for . For a plane wave , , and . Thus the fields are transverse, mutually perpendicular and in phase; polarization describes the electric-field trajectory at a fixed point.
The energy density and Poynting vector are
For a linearly polarized sinusoid with peak electric amplitude , the mean intensity is . Electromagnetic momentum density is ; normal absorption produces radiation pressure , while ideal retroreflection doubles it. Linear superposition permits interference and standing waves, whose local electric and magnetic fields need not have the traveling-plane-wave equality point by point.
Use peak-amplitude phasors with time factor and . Faraday's law of induction and the Ampere-Maxwell law give
In the good-conductor limit , take the root with positive attenuation into the slab:
The real physical field is . A thick slab excludes a returning wave from its rear face. The skin depth is the electric-field amplitude decay length; the intensity decay length is .
Faraday's law of induction fixes . The surface impedance of a good conductor and the complete transmitted magnetic field are consequently
The sign of the imaginary part belongs to the stated time convention. Average the Poynting vector using complex conjugation and the factor one half appropriate to peak phasors:
As an independent energy check, , the mean Joule heating per unit volume.
Ohm's law gives and . Hence the averaged Lorentz force per unit volume is
Integrating through the illuminated half-space gives the positive inward radiation pressure
Finally let be the vacuum wave impedance. Tangential-field boundary conditions at normal incidence give the electric-amplitude reflection coefficient . Since ,
Here by surface energy balance. Combining the leading formulas gives , the nearly perfect-reflector limit. The displayed reflection expansion also assumes a good conductor relative to the incident vacuum wave, .
An electrostatic field calculation begins by specifying the charge information, material response and boundary conditions. In vacuum, prescribed volume and surface electric charge densities can be superposed directly using Coulomb's law. For a volume distribution,
Differentiating this electric potential gives the electric field. This is useful for known source distributions, but in the presence of conductors the induced surface electric charge is usually an unknown rather than an independently specified input.
Gauss's law is especially effective when symmetry fixes the direction and magnitude of the electric field on a suitable closed surface. A spherical charge distribution gives a radial field, an infinitely long uniform line gives a cylindrical field, and a uniform infinite sheet gives a planar field. In an arbitrary geometry, the flux law remains true but does not alone determine the pointwise electric field. A multipole expansion is another useful approximation: far from a localized charge distribution, successive monopole, dipole and higher terms separate the effects of total charge and its spatial structure.
For a boundary-value formulation, use the electrostatic equations
They imply Poisson equation , or Laplace equation where . A conductor in electrostatic equilibrium is an equipotential with zero internal electric field. Its exterior normal electric field fixes the surface electric charge through . One must specify whether each conductor is grounded, maintained at a prescribed voltage, or isolated with prescribed total electric charge.
Uniqueness of Poisson equation justifies methods that construct a convenient candidate solution. With fixed boundary electric potential and suitable behaviour at infinity, a solution satisfying the field equation is the solution. With normal-derivative boundary conditions, the source and flux must be compatible, and the electric potential is determined only up to an additive constant.
For example, a point charge a distance above a grounded infinite plane has the same upper-half-space electric potential as and a mirrored image charge below it. Their potentials cancel on the plane. The image is a mathematical source in the excluded region, not a second physical charge. Separation of variables similarly constructs solutions suited to rectangular, cylindrical or spherical boundaries; matching coefficients enforces the prescribed boundary data.
In dielectrics, the distinction between total and free charge is essential. In a linear isotropic material,
Only where permittivity is constant may this be reduced to . At an ordinary interface, and the tangential electric field are continuous, while the jump in normal electric displacement field is the free surface charge. Applying Gauss's law to total charge with , or its displacement-field form to free charge, gives consistent descriptions; mixing their sources and permittivities does not.
A useful interface example is the image charge at a dielectric interface. If lies in medium 1, the source-side potential is represented by
where is distance to the real charge and to its mirrored position. The other-side potential can be written , where . Continuity of and of normal fixes both coefficients. The equal-permittivity limit gives no image; the conductor limit gives .
For a sphere of radius and relative permittivity in a uniform external electric field , matching the spherical solutions gives a uniform internal electric field and an external induced electric dipole moment:
This illustrates how a material boundary modifies an otherwise simple applied electric field.
For complex boundaries or spatially varying materials, finite difference methods or the finite element method solve the same boundary value problem numerically. A sound calculation checks its boundary conditions, charge or flux balance and convergence with mesh refinement. The governing equations, source classification and uniqueness argument remain the organizing principles even when an analytic formula is unavailable.
Assume a hollow square electromagnetic waveguide with perfectly conducting walls, filled with vacuum or air. For side , the waveguide cutoff frequency is
A transverse electric mode can have one zero index, but not both. A transverse magnetic mode requires both indices positive. Thus the lowest cutoff belongs to the two degenerate transverse electric modes and , with
The corresponding cutoff vacuum wavelength is . Strictly, a travelling mode carrying power along the guide needs : at the cutoff itself, the axial wavenumber and group velocity are zero. The number above is therefore the lower frequency threshold, not a propagating mode with nonzero longitudinal energy flux exactly at that frequency. A dielectric filling would replace by the wave speed in that medium.
The symmetry is electromagnetic reciprocity applied to mutual inductance. For thin closed circuits in vacuum, the magnetic vector potential generated by circuit B is
Stokes theorem converts the magnetic flux through circuit A into its magnetic vector potential circulation. Dividing by gives Neumann's mutual-inductance formula,
The dot product and separation are unchanged by interchanging A and B, so
Each has units . The winding orientations must be used consistently to determine the common sign. The same reciprocity holds in ordinary linear reciprocal magnetic media; it is not an unrestricted statement about biased nonreciprocal materials. Equivalently, a reversible magnetic energy function has equal mixed derivatives with respect to the two currents.
Maxwell's displacement current is the electric-field contribution needed to make Ampère's law consistent with charge conservation. In macroscopic form,
The displacement current density has units . Since , it contains the vacuum field term and, in matter, the polarization-current contribution. It need not represent free charge moving through a material.
Taking the divergence gives . Gauss's law, , then yields the continuity equation . Without the displacement term, Ampère's original law would incorrectly require every current distribution to be divergence-free even while charge accumulates.
A charging parallel-plate capacitor makes this concrete. Ignoring fringing, , so the displacement current across its dielectric gap is , equal to the conduction electric current in its wire. The integral law
therefore gives the same answer whether the spanning surface cuts the wire or passes through the gap. Together with Faraday's law, this field term also permits self-consistent electromagnetic waves in vacuum, with speed .