In the Schrödinger picture, a time-independent Hamiltonian gives , where . The Heisenberg picture transfers this evolution to each observable:
Both pictures give the same probabilities and expectation values. Differentiating yields the Heisenberg equation of motion
The last term is an explicit change of the measured operator. If it is absent and , the observable is conserved.
The corresponding classical equation is . The correspondence principle relates the Poisson bracket to , with suitable operator ordering and a classical limit. For , the canonical commutation relation gives
Taking means gives Ehrenfest theorem. Its second equation contains , which need not equal . A narrow wave packet in a slowly varying force field can follow the classical equations approximately; a quadratic potential makes the equality exact for the means.
For a quantum harmonic oscillator, direct solution gives and . These have the classical form as operator identities. A coherent state supplies a localized center moving on the classical orbit, whereas an energy eigenstate has stationary density and , even at large excitation. Thus large quantum numbers alone do not create a localized classical trajectory. Classical behavior also concerns state preparation, relative fluctuations and the resolution of the measurements.
Build a narrow-band wave packet from plane waves with wavenumbers close to :
The Taylor expansion of the dispersion relation is , where . Put to obtain
The carrier's wave phase travels at the phase velocity , while the envelope has constant shape at constant . Its group velocity is therefore
The approximation neglects higher derivatives of the dispersion relation. Those derivatives cause the wave packet to spread or distort over sufficiently long propagation times; the result describes the local envelope speed of a sufficiently narrow band.
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.
For the deep-water gravity wave, the phase velocity and group velocity follow from its dispersion relation:
The wave packet travels at , while the individual crests travel at . Let its effective length be , where is the carrier wavelength. A fixed observer is inside the wave packet for , and crests arrive with wave period . Thus
Crests enter the rear of the moving wave packet and disappear at its front, so the five visible at one instant are not five permanently identifiable crests. The count uses the intended narrow-band, approximately unchanged wave packet and neglects the precise visibility of its end crests.
Twice the quadratic coefficient from the previous part is the band curvature . Thus the band effective masses are
Here and . In the weak-potential regime ,
Both have units of mass; their magnitudes are much smaller than in this asymptotic regime. The upper energy band has a local minimum and positive effective mass, while the lower energy band has a local maximum and negative effective mass. The exact lower-branch sign changes at in the two-wave formula; the intended weak-coupling limit lies below that threshold.
The physical meaning follows from the semiclassical equations for an electron wave packet in one energy band:
An upper-band electron near its minimum accelerates in the direction of the applied force, whereas a lower-band electron near its maximum accelerates opposite to it. At the extremum itself the group velocity is zero. A nearly filled lower energy band is conveniently described by electron holes with positive electric charge and positive effective mass . Negative curvature is a response of a crystal energy eigenstate, not a negative bare electron mass. These statements assume slow forcing that does not induce transitions across the band gap.
Time dependence in quantum mechanics describes how a prepared quantum state changes and thereby changes the probabilities of later measurements. For an isolated system, the Schrödinger picture assigns this evolution to a state vector , governed by the Time-dependent Schrödinger equation
The Hamiltonian is a self-adjoint operator; it has units of energy, while has units of action, so has units of inverse time. For a particle with potential energy , this becomes
Given a suitable initial wavefunction and the physical boundary conditions, this first-order equation determines its subsequent propagation. Its linearity means that the evolution of a quantum superposition is the corresponding quantum superposition of evolved states.
For a real potential energy, this equation and its complex conjugate imply the local continuity equation
Here is the probability density and the probability current. Vanishing net boundary flux preserves wavefunction normalization, as required by the Born rule.
The time-evolution operator packages the solution for every initial state:
Because , differentiation gives
Therefore : this is unitary time evolution, preserving inner products and all state norms. It is reversible, with , and obeys the composition law .
For a time-independent Hamiltonian, the solution is the operator exponential
If the Hamiltonian varies with time, the analogous simple exponential of its integral is valid when for all relevant times. Otherwise time ordering is essential:
The meaning is explicit in the first terms of the ordered series,
the later-time operator stands on the left. In the position representation, the same propagation is expressed by the quantum-mechanical propagator
Its initial value is the Dirac delta function .
A time-independent Hamiltonian has energy eigenstates satisfying . A single such initial state evolves as
It is a stationary state: its global phase changes, but its probability density and the distributions of time-independent observables do not. Its energy is sharp. Any quantum superposition entirely within one degenerate energy eigenspace also acquires one common global phase and is stationary. Stationarity does not require zero probability current; for instance, on the ring has a constant density and persistent circulation when .
An arbitrary normalized state can instead contain different energy eigenvalues:
A continuous spectrum requires corresponding integrals. For the discrete case, an energy measurement gives with fixed probability (summed over degeneracies), but relative quantum phases change with time. Consequently
The interference terms can oscillate at angular frequencies . For two populated energy levels, this supplies a characteristic period when the interference term is nonzero. Thus fixed energy populations do not imply a stationary spatial distribution.
For a normalized state and an observable , its expectation value is
This is the statistical mean over repeated preparations and measurements. In an eigenbasis of energy eigenstates for a time-independent Hamiltonian and a time-independent ,
Only matrix elements connecting different energies can generate these oscillations. If , its expectation value is constant for every initial state, provided it has no explicit time dependence.
Differentiating the expectation value and substituting the Schrödinger equation for both the bra and ket proves the general Ehrenfest theorem:
Equivalently,
These manipulations require the state to lie in the relevant operator domains. Taking gives , so energy is conserved under a time-independent Hamiltonian.
For , the canonical commutation relation gives
Hence the particularly useful position-and-momentum form of Ehrenfest theorem is
It resembles Newton's second law, but the mean force generally differs from the force at the mean position. If a narrow wave packet samples a region where the force varies little, gives approximate classical motion. For a quadratic potential energy this replacement is exact. In particular the quantum harmonic oscillator obeys
The centroid follows the classical harmonic oscillator, although this does not specify the full evolving wavefunction or its width.
The Heisenberg picture expresses the same physics by assigning evolution to observables instead:
The expectation value is unchanged, and differentiation yields . Thus state propagation, evolving expectation values, and the classical correspondence in Ehrenfest theorem are mutually consistent descriptions of the same unitary time evolution.
A nondispersive wave has a linear dispersion relation over the relevant range, so every Fourier transform component has the same phase velocity and group velocity . A wave packet then translates without spreading in an ideal homogeneous lossless medium.
For wave dispersion, depends on frequency or wavenumber. Different components accumulate different phases, and in general the group velocity differs from the phase velocity; variation of group velocity across the spectrum produces spreading of a wave packet. The membrane material can be nondispersive while confinement in a membrane waveguide introduces wave dispersion along its length.
Here is potential energy, is the stationary state's total energy, and is its spatial probability amplitude. The wave function has time factor ; is a position probability density for a normalized state. Stationary plane-wave scattering solutions are idealizations described by probability-current ratios, or components of a normalizable wave packet.
Above an upward step, a classical particle is fully transmitted with reduced speed. Quantum mechanically the abrupt wavelength change generally produces both reflected and transmitted amplitudes even though both regions are classically allowed. With unit incident amplitude and no wave arriving from the right,
The reflected component has signed wavevector and the same wavenumber magnitude as the incident component. A finite potential jump with constant mass and no delta interaction requires continuity of and :
The probability current gives probability reflection and transmission and , with . The amplitude may exceed one without violating conservation of total probability, because the transmitted group speed is smaller.
For , let . The bounded right-hand solution is , an evanescent wave tail with amplitude penetration scale . It carries no outgoing probability current in an infinitely long forbidden half-space, so reflection is total. This differs from transmission through a finite potential barrier, where a second boundary can support quantum tunnelling.
For a downward step, replace by . The same boundary conditions give a nonzero negative , corresponding to a reflected amplitude with phase reversal. If reflection were forbidden, would require both and , impossible for a nonzero step. Reflection therefore does not require a classical potential barrier; the discontinuity of wavenumber mismatch is enough.
For the specified electron energies, , so the requested amplitude coefficients are
The corresponding probability coefficients are approximately and . electron mass cancels from these ratios; there is no need to invent an additional material effective mass.
The time-independent Schrödinger equation is the energy eigenvalue equation for a particle of mass . The Hamiltonian operator is the sum of the kinetic operator and the prescribed potential energy . Here is the reduced Planck constant. A corresponding stationary state is . The Born rule identifies as probability density for a state with wavefunction normalization ; integrating it over an interval gives a position probability. A plane wave scattering state is not a normalizable wavefunction on the whole line, but its probability currents give the reflection and transmission fractions of an incident wave packet.
There is a notation discrepancy in the sources: the original PDF prints an unbarred in the kinetic term, whereas the local TeX uses . The standard physical equation uses the reduced Planck constant , where is the Planck constant; that convention is used below. Reading the printed literally as the Planck constant would scale all lengths in this model by relative to the standard answers, but would leave the amplitude ratios unchanged.
For , both sides allow oscillatory wavefunctions. A classical particle always crosses the potential step and slows because its kinetic energy falls from to . In quantum mechanics there is generally both reflection and transmission even though the particle is above the step. Define the positive wavenumbers
With no wave incident from the right, write
A finite potential step with constant mass makes both the wavefunction and its first derivative continuous. The two boundary conditions at are
Solving gives the reflected and transmitted wavefunctions
For the specified electron energies, , so the relative probability amplitudes are
The transmitted probability amplitude exceeding one is compatible with conservation of quantum probability, since the outgoing speed is smaller. In fact the probability current gives
These are the quantum reflection probability and transmission probability, which must be distinguished from the requested relative amplitudes.
mass as band curvature. In a periodic potential, a weakly forced electron is usefully described by a wave packet confined to one energy band. Its group velocity is
Differentiating the velocity gives
This effective-mass tensor describes the band response, not a change of the electron's bare rest mass. Along a principal direction, a steep upward curvature gives a small positive mass and a flatter curvature a larger one. Near a band maximum the electron curvature and effective mass are negative; the corresponding missing-electron description uses positive electron hole masses. Anisotropy produces distinct principal masses, and strong nonparabolicity makes them momentum dependent. The single-band semiclassical description assumes fields weak and slowly varying enough to avoid substantial interband transitions.
Lattice symmetry and Bloch's theorem. Use the active spatial translation operator . A lattice-periodic scalar potential satisfies , while the kinetic term is translation invariant. Therefore . The lattice translations also commute with one another, so they can be diagonalized simultaneously with , including within a degenerate energy subspace.
For a common eigenstate, write . Unitarity gives , and the group law gives . On primitive Bravais vectors , choose . Every lattice vector is an integer combination of these generators, hence
The vector is defined modulo a reciprocal lattice vector. The band index labels the different energy eigenstates with the same translation character. Define . The phase factors cancel under a lattice translation, proving Bloch's theorem in its usual form:
This is the Translation-character proof of Bloch theorem; the commutator guarantees a basis of such states, even when an arbitrary superposition of different translation characters is not itself a translation eigenstate.
Periodic Hamiltonian. Acting once with momentum gives . Applying it again and cancelling the common plane-wave factor yields
The Bloch Hamiltonian acts on lattice-periodic functions in a unit cell. Expanding its square separates a zero-momentum Hamiltonian, a term linear in and an identity term quadratic in .
Expansion about the zone centre. Let , , and normalize all these states using a unit-cell inner product. For the real scalar Hamiltonian in the question, a nondegenerate zone-centre eigenfunction can be chosen real. Then
because opposite unit-cell faces cancel. Equivalently, time-reversal symmetry forbids a nonzero electric current in this nondegenerate spinless state. This explains why no linear energy term appears; it should not simply be omitted without a symmetry or extremum argument.
The first-order energy shift is therefore . In the second-order sum the quadratic term is proportional to the identity and has no off-diagonal matrix elements. Only the linear momentum vertex contributes. Second-order nondegenerate perturbation theory gives the momentum matrix-element expansion of band energy
Hermitian operator makes the two reciprocal matrix elements complex conjugates. All other periodic eigenstates at enter the sum. The remainder is even because time-reversal symmetry gives near this isolated state. At a degeneracy the denominators signal the need for degenerate perturbation theory instead.
mass ratio and the printed formula. Write . Differentiating the quadratic energy yields
For a specified unit direction , the resulting scalar mass ratio is
In an isotropic three-dimensional band, averaging equivalent directions gives
Coupling to lower bands contributes positively to inverse mass; coupling to higher bands contributes negatively. Their signs and matrix elements determine the actual curvature.
The original PDF prints . Taken literally as a three-dimensional Laplacian, this misses a factor of three for an isotropic scalar mass. The correct identities are
The printed expression would return even for the free dispersion . It is correct in one dimension, or if its second derivative is interpreted directionally. For completeness, its literal three-dimensional trace ratio would instead be ; that is the trace of the dimensionless inverse-mass tensor, not the usual scalar .
The unit-normalized Fock vacuum is characterized by
Choose the relativistic normalization of a one-particle state from the outset:
Since any two creation operators commute, any permutation of their order gives exactly the same state vector. Thus these multiparticle quantum states are symmetric under exchange and describe bosons, without a minus sign or any additional exchange phase.
The Hilbert space is the bosonic Fock space, the direct sum of the symmetric -particle Hilbert spaces, including the zero-particle sector. Sharp-momentum kets are distributionally normalized; square-integrable wave packets provide ordinary Hilbert space vectors. For repeated occupation of a discrete mode, a unit-normalized number state uses . That factorial does not belong in the above labelled continuum-ket convention.
The canonical momenta are , so
Different species commute at equal times, so these products have no ordering ambiguity and is Hermitian. Write . Substituting the mode expansion of a free field and using the spatial Fourier transform identity gives
Subtract the expression with species interchanged. The two-annihilator terms cancel after , as do the two-creator terms. Commuting different species in the remaining terms yields
There is no infinite vacuum contribution to the Noether charge to subtract: the contractions that would generate a species-diagonal constant are absent.
The bosonic canonical commutation relations give
Define the creation operators
Their commutators with are . Since , the one-particle states have
The fixed-momentum states are delta-function normalized; a square-integrable wave packet of either species is a normalizable state with the same Noether charge eigenvalue. In this basis , so it measures a difference of occupation numbers. The equal-time identity , independently checks the sign against a.
Continue with . Along a characteristic , the chain rule gives
Thus the initial wave packet evolves as . Similarly, along , the left component is constant, giving
A feature initially at therefore appears at for the right component and for the left component. The profiles translate without changing shape at the speed of light, which is 1 in these units. For positive-energy plane waves, the right component has and the left component has , another way to identify their propagation directions.
The conclusion concerns the massless Dirac equation. For , the components couple as in c, and a positive-energy packet has group velocity , rather than a universal speed . For example, a massive positive-energy rest solution has and , so neither component alone describes an independently moving light-speed packet.
For the Schrödinger equation with a real scalar potential and no vector potential, the probability current is
Together with the probability density , it satisfies the continuity equation . Substituting gives
A complex wavefunction requires both its real and imaginary parts in the sketch. Choosing the irrelevant constant phase so that is real, they are and , while the probability density is horizontal. It is the spatial phase gradient of a Schrodinger wavefunction that determines the sign of the probability current. In particular, and have the same real part but opposite probability currents, so the slope of the real part cannot determine the direction.
A nonzero plane wave on the whole real line is not square integrable. The displayed density is understood with box normalization, generalized normalization, or as a local description of a broad wave packet; it does not define a normalized probability distribution on the whole line.
Figure 1. . The plotted example has positive wavevector. Reversing the wavevector reverses the imaginary part and the probability current while preserving the real part and the probability density. Details.
Write for the cross-sectional area, and use consistently for the longitudinal coordinate: the paper's later is the same coordinate. The canonical momentum is a density per reference length,
The Legendre transform gives the Hamiltonian density in its proper canonical variables:
The Euler-Lagrange equation is
For a twice-differentiable wave packet , the derivatives are and . Thus the nontrivial packet solves the wave equation when
The negative sign gives the opposite propagation direction. Here has units , has units , and has units . The result follows from the supplied axial stiffness in the Lagrangian. For a freely contracting thin elastic rod the relevant longitudinal modulus is normally Young's modulus, rather than the bulk modulus; the question's given Lagrangian fixes which coefficient is being used.
For a rightgoing wave packet, put and assume decays sufficiently rapidly. Then
The shift charge becomes
It is time independent. It vanishes for a localized displacement packet that returns to the same displacement at both ends, but need not vanish for a localized strain pulse joining different asymptotic displacements.
For the dilation charge, substitute :
The change of variables removes all time dependence. This charge also need not vanish; choosing an origin at the packet's energy centroid can make it zero. Conservation assumes the integral exists and there is no boundary flux, rather than merely assuming that the energy is finite.
Classical translational statistics. Write the number density as and the thermal de Broglie wavelength as . Quantum exchange is negligible when wave packets rarely overlap:
The equivalent state-counting statement is that the mean occupation of each thermally relevant one-particle state is much smaller than one. The equations in this question count one internal species; with equally populated spin states the relevant density per species is .
Let be the dimensionless quantum gas fugacity, with the lowest one-particle energy chosen as zero. Both quantum distributions can be written
If , then for all , recovering Maxwell–Boltzmann statistics. Conversely, low occupation even at the spectrum's bottom requires for bosons or for fermions; either condition implies
A single high-energy state can be sparsely occupied even in a degenerate gas, so the condition must hold across the relevant spectrum, not just for one arbitrarily chosen energy. Also, classical translational statistics does not imply that all internal excitation energies or other quantum effects can be ignored.
Grand partition function, density and pressure. Noninteracting particles have independent occupations of each one-particle state. Put . Summing the allowed occupations gives
Therefore
The grand potential is for this homogeneous gas. Replacing the sum by and using gives
The mean number is , giving
For bosons, the grand sum requires when the ground energy is zero. A macroscopic condensate at the limiting must be separated from the continuum integral in the condensed phase. The following small- calculation is in the normal, nondegenerate regime, so that complication does not enter.
Density expansion and inversion. Expand the occupation as a geometric series:
The Gaussian wavevector integral for its th term is
It follows that
For the inverse series, put and try . Substitution gives , hence
The leading equality directly connects the density and occupancy criteria for classical behavior.
Pressure and its first quantum correction. Expanding the logarithm in the pressure expression gives one extra factor compared with the density series:
Insert the inverse series. To second order in ,
Thus
The first quantum correction at fixed density and temperature is
It is negative for bosons and positive for fermions, and vanishes in the classical density limit.
Virial coefficient. Define the number-density virial expansion by
The coefficient has units in this convention. Comparing terms gives
This is the exchange contribution to the second virial coefficient. It arises without a pair-interaction potential; the underlying gas is noninteracting. A molar-density convention would multiply this by the Avogadro constant. For equally populated internal species, exchange occurs within each species and the coefficient in terms of total density is smaller by a factor .
Why the two signs differ. Bosonic exchange symmetry enhances the probability of nearby identical bosons, whereas fermionic exchange symmetry suppresses nearby identical fermions in the same internal state. In the dilute regime, the normalized equal-time pair detection correlation is
The exchange part follows by squaring the Gaussian one-particle coherence factor . At zero separation this gives for bosons and for one-component fermions. Integrating the exchange pair weight provides a direct coefficient check:
Bunching therefore acts like an effective statistical attraction in the dilute equation of state, lowering the pressure needed at fixed density. Exclusion acts like an effective statistical repulsion, raising it. Neither description asserts an actual interparticle force. Different internal fermion species do not exclude each other from a common spatial location in the same way, explaining the importance of the species convention.
Write the cosine in i as two complex exponentials. On a ray , the oscillatory phases are . The stationary phase method requires . By ii, the largest absolute horizontal group velocity for the occupied mode is
Inside this region there are stationary wavenumbers supporting appreciable wave packet contributions. Outside it no stationary wavenumber exists; oscillatory cancellation suppresses the large-time response. This explains "mainly confined": the initial Lorentzian profile already has nonzero algebraic tails, so the displayed region is not the exact support of the solution. Near its boundary the stationary points meet and the usual nondegenerate stationary-phase formula needs a transition approximation.
Phase velocity Created 2026-09-24 Updated 2026-10-14
The phase velocity is the motion of a constant-wave phase surface. For a one-dimensional plane wave with real and real , fixing gives
Each wave crest of this monochromatic travelling wave advances at that signed phase velocity. Its magnitude is the phase speed , where is the wavelength and is the temporal period when . Choosing makes positive mean rightward phase velocity and negative mean leftward phase velocity. Reversing both signs leaves the real plane wave and its phase velocity unchanged. At there are no spatial crests to track, so is undefined; a finite limit as is a limiting phase speed, not the speed of a spatially uniform oscillation.
In several dimensions, a plane wave has wave phase . Constant-wave phase planes obey . Their normal phase velocity is
Tangential motion within a plane does not move that wavefront, which is why the normal direction fixes the vector convention. In an anisotropic medium the group velocity need not point along this wavevector. Likewise the horizontal phase velocity of a tilted wavefront is its crossing speed along a horizontal line, rather than a component of the normal phase velocity.
For the nondispersive wave branch , a wave crest and a wave envelope both move at . For deep-water surface gravity waves, gives and group velocity . With the illustrative choices and , the model predicts and . These are calculated values for negligible surface tension and sufficiently large , not measurements. A wave crest moves forward through the wave packet, so timing a crest does not time the packet's journey.
There is a direct laboratory meaning to this distinction. MIT's 2005 surface-wave lab uses a long water tank, a controllable hydraulic paddle, and an absorbing beach. Resistance probes convert submerged length into voltage; calibration converts their readouts into free surface elevation versus time. Two probes a known distance apart, backed by a ruler and stopwatch, let students time a wave crest and separately time a feature of the wave packet. The lab records depth and varies frequency and wave amplitude.[ref]
For a clean measurement of phase velocity, fit the periodic portion of both records or follow one identifiable wave crest. A phase difference is only known modulo : probe spacing below half the shortest relevant wavelength, or continuity while sweeping frequency, avoids assigning the wrong whole-cycle delay. Then compare the timed phase velocity with . Tracking pepper grains instead measures fluid-particle motion, which has a different meaning from either phase velocity or group velocity.
The Klein-Gordon packet velocities example makes the distinction especially sharp: its phase velocity exceeds , yet its narrow wave envelope moves below . A carrier wave labels successive oscillations; its speed alone does not establish information velocity. The front velocity depends on the full causal model, including angular frequencies far outside the carrier's narrow range.
Pulse 2026-10-24
A pulse is a localized disturbance that passes a fixed location during a bounded or effectively bounded time interval. A travelling wave pulse may be written with localized . Its width and peak amplitude describe its extent and size; a wave packet additionally emphasizes a carrier and an envelope.