Wave Packets and Their Construction
An electron gun fires. Something flies down the column, crosses a metre of vacuum in a few nanoseconds, and lands on a detector as a single bright point. Whatever flew was not a plane wave — Free Particle and Plane Waves showed those fill all space and can never be normalized — and it was not a classical bullet either, because aim enough of them at a double slit and the landing points build interference fringes. What flew was a wave packet: a superposition of plane waves, engineered by nature so the components reinforce in one small region and cancel everywhere else. The packet answers the question that closed the last article — if the eigenstates are all impossible, what does an actual free particle look like? The construction is pure Fourier analysis, earning its keep in quantum mechanics here. You will build from an amplitude recipe , learn to invert the recipe from the initial shape, and meet the trade that no packet can escape: squeeze the lump in position and you must widen the mix of wavenumbers — the uncertainty principle, appearing not as an axiom but as a theorem about waves. The Gaussian packet, worked in full, saturates that trade exactly and follows you from coherent states to scattering theory. Deliberately postponed: how the packet moves is Group Velocity versus Phase Velocity; how it spreads is Wave Packet Spreading and Dispersion. Here we master what a packet is — anatomy before dynamics.
- A wave packet is a normalizable superposition of plane waves: , with the amplitude saying how much of each is mixed in.
- The recipe is invertible — — so and are a Fourier-transform pair: two faces of one state.
- Plancherel's theorem makes the momentum reading consistent: is the probability density in wavenumber, so the density in momentum is .
- Localizing in costs spread in : , i.e. — the bandwidth theorem of Fourier analysis is the uncertainty principle.
- The Gaussian packet achieves equality, : it is the minimum-uncertainty state, Gaussian in both faces at once.
- Key idea: a particle's state is one function wearing two dresses — in position, in momentum — and Fourier reciprocity forbids both dresses from being narrow.
A physical free-particle state is a Fourier superposition of plane waves, : the amplitude is the momentum-space wavefunction, its modulus squared gives momentum statistics, and the Fourier reciprocity between the widths of and is the uncertainty principle in its rawest form.
Where this lives today
Attosecond science is wave-packet engineering by hand: shaping spectral amplitude and phase is how the 2023 Nobel experiments clocked electron dynamics at the 10⁻¹⁸ s scale, the bandwidth theorem dictating that a 100-as pulse needs tens of eV of spectral width. Ultrafast electron microscopes fight the same reciprocity in reverse — compressing packets in time broadens their energy spread, blurring spectra. And every atom interferometer begins by preparing atomic Gaussian packets whose two faces are set by laser cooling () and trap release ().
The physical picture
Strike a tuning fork and the sound is a pure, endless tone — the acoustic cousin of a plane wave. Strike a piano's low string, pedal down, and many neighbouring frequencies sound at once; they beat against each other, and the sound arrives in a lump. That is the whole trick of localization: waves of slightly different wavelength agree in one place — crest on crest, all in phase — and disagree everywhere else, trough cancelling crest. Add a narrow band of wavenumbers and you get a wide lump; add a broad band and the region of agreement shrinks to a needle.
Quantum mechanics adds only one ingredient to this ancient wave lore: through de Broglie's , wavenumber means momentum. So "which wavelengths are in the mix" is not a technicality of synthesis — it is the particle's momentum distribution. The recipe function that a sound engineer would call the spectrum, quantum mechanics calls the momentum-space wavefunction, the same object introduced for general states in Momentum-Space Wavefunction; here it takes its most concrete form. One state, two complete descriptions: answers "where," answers "how fast," and Fourier analysis is the dictionary between them. The concept-level tour of this construction in Free Particle and Wave Packets promised that machinery; now we build it for real.
The construction
Take the delta-normalized plane waves of Free Particle and Plane Waves and superpose them with an amplitude — the continuum version of expanding in an orthonormal basis:
where: — the complex amplitude density for wavenumber (momentum ); the — the symmetric convention that will make the inverse transform and Plancherel's theorem come out clean. Equation (1) is a synthesis: it assembles the position-space shape from momentum ingredients. If is sharply peaked at , the packet is nearly monochromatic and very wide; if is broad, the components dephase within a short distance and the packet is narrow. The recipe can be run backwards. Given the initial shape — prepared by a slit, a trap that was just switched off, an emission process — the amplitude of each ingredient is extracted by projecting onto the corresponding plane wave:
where: the only change from (1) is the sign in the exponent — analysis instead of synthesis. Together (1) and (2) say and are a Fourier-transform pair: neither is more fundamental, and either determines the other completely. This is Plancherel's theorem in action, and its physical backbone is proved in the first derivation card below. One consistency check makes the whole interpretation hang together. If integrates to one (total probability), what does integrate to?
where: the equality of the two integrals — Parseval's identity — is not an accident but a theorem. It licenses the Born-rule reading of the second face: is the probability that a momentum measurement finds in . Normalize once, in either representation, and both are normalized forever.
We are proving the two structural facts that make wave packets usable: that formula (2) really does invert formula (1), and that total probability is the same number whether computed in position or momentum space (Parseval's identity). The strategy is to substitute one integral into the other and let the plane-wave orthogonality relation from Free Particle and Plane Waves — the Dirac delta identity — collapse the double integral. Watch where the factors go: the symmetric split is exactly what makes both directions of the transform, and the probability bookkeeping, come out without stray constants.
Step 1. Substitute the synthesis (1) into the right-hand side of the claimed inverse (2), using a dummy variable inside:
Why the swap of integration order is the crux: it isolates the -integral of a pure phase — precisely the object the delta identity evaluates.
Step 2. Apply the plane-wave orthogonality relation :
The inverse is exact: (2) recovers the amplitude that (1) used. The pair is self-consistent.
Step 3. For Parseval, write with two independent expansions of and :
Step 4. The delta collapses one integral:
Why this is physics and not just analysis: the left side is total position probability, the right side total momentum probability. Their equality is what permits to be a genuine probability density — the momentum Born rule — with no separate normalization step.
The reciprocity law: narrow here means wide there
Fourier pairs obey a seesaw. Compress by a factor — replace by — and the transform dilates: (up to normalization). Whatever squeezes one face stretches the other. Made quantitative with root-mean-square widths, the seesaw becomes the bandwidth theorem:
where: and — the rms widths of and ; the second form follows by . Read the logic direction carefully: this is a theorem about any Fourier pair — radar pulses and audio filters obey it identically — and quantum mechanics inherits it the moment it declares to be the two faces of one state. Position–momentum uncertainty is not an extra postulate bolted onto wave mechanics; it is wave mechanics. (The operator-theoretic version, with its commutator machinery and its generalization to arbitrary observable pairs, is the business of the Generalized Uncertainty Principle in the formalism chapter.)
The Gaussian packet, worked in full
One family turns inequality (4) into an equality — the family you will meet in coherent states, path integrals, and every laser lab: the Gaussian. Start from the momentum recipe — a Gaussian bump of -half-width centred on a carrier :
where: — the length scale that will turn out to be exactly the packet's rms position width; — the mean wavenumber, giving the packet its mean momentum . The prefactor normalizes . What position shape does this recipe synthesize? The derivation card carries out the integral honestly.
Go deeper · Derivation B · 1 minSynthesizing the Gaussian packet
We are computing the position-space face of the Gaussian momentum recipe (5) by direct evaluation of the synthesis integral (1), and then reading off the two rms widths to exhibit the minimum-uncertainty product . The strategy is the completing-the-square manoeuvre for Gaussian integrals — the single most reused calculation in quantum mechanics, worth doing slowly once. Watch two things: how the carrier separates into a pure phase factor that the probability density never sees, and how the width migrates from the denominator of the -space exponent to the numerator of the -space one — reciprocity happening before your eyes.
Step 1. Insert (5) into (1) and shift variables to , so the integral centres on the carrier:
Why the shift: it factors out — the carrier wave — and leaves a real, centred Gaussian integral in .
Step 2. Complete the square in the exponent: , and use :
Step 3. Collect constants:
A Gaussian recipe synthesizes a Gaussian lump — the family is closed under Fourier transformation. Check normalization: integrates to 1.
Step 4. Read off the widths from the two densities. is a normal distribution with ; is one with . Therefore
Why equality lands exactly here: in the bandwidth theorem's proof (a Cauchy–Schwarz inequality), equality requires the two functions being compared to be proportional — a differential condition whose solution is precisely the Gaussian. Any other shape gives a strictly larger product.
The worked Gaussian rewards a moment of respect. Its three parameters answer the three physical questions: where is the particle ( here; add a factor to to centre it at ), how fast is it (), and how sharply is each defined (, ). At it is the most classical state quantum mechanics permits — both faces as narrow as the seesaw allows simultaneously. What happens next — the centroid gliding at the group velocity, the width growing as the components dephase — is precisely the subject matter of Group Velocity versus Phase Velocity and Wave Packet Spreading and Dispersion; the packet built here is their shared initial condition.
Momentum statistics without ever measuring position
The payoff of the two-face structure is that momentum questions are answered directly in the momentum face — no derivatives, no operators, just read the distribution like any probability density:
where: the formulas are the ordinary mean and variance of the distribution , scaled by . For the Gaussian (5): and , by inspection of a normal distribution — compare the same computation in position space, which requires integrating . The representation in which an operator is diagonal is the representation in which its statistics are effortless; that lesson, learned here concretely, becomes a central principle of the formalism chapter.
Limiting cases
| case | result | meaning |
|---|---|---|
| the plane-wave limit: perfect momentum, no location, normalization lost — the basis element of Free Particle and Plane Waves recovered | ||
| const (flat) | the opposite extreme: perfect position, all momenta equally mixed — equally unphysical | |
| Gaussian | exactly | the minimum-uncertainty packet; Gaussian in both faces at once |
| top-hat of half-width | oscillatory tails so heavy that rms diverges — see Example 2 | |
| at fixed | packet monochromatic | fractional momentum spread : the beamline idealization |
| carrier shift | the Fourier shift theorem: linear phase in one face = translation of the other |
Worked examples
Example 1 — an electron beam's coherence budget (confidence builder). An electron microscope prepares Gaussian packets of rms width nm riding a 100 eV beam. Find the momentum spread, the velocity spread, and the fractional momentum spread.
Step 1. Minimum-uncertainty momentum spread: .
Step 2. Velocity spread: .
Step 3. Beam momentum at 100 eV: (speed m/s).
Step 4. Fractional spread: . The packet is a nearly monochromatic wave a thousand crests long — which is exactly why plane-wave scattering amplitudes describe beam experiments so well.
Example 2 — the top-hat recipe and its heavy tails (exam level). A monochromator passes all wavenumbers in a flat band with equal amplitude, inside the band and zero outside, with . Find the packet shape, the location of its first zeros, and its rms width.
Step 1. Synthesize with (1). Shifting to : .
Step 2. The envelope is a sinc. Check normalization: . ✓
Step 3. First zeros where : — the central lobe is about 13 nm wide.
Step 4. Now the trap: the rms width. : the rms width diverges. The sinc's tails fall only as in probability — too slowly for a second moment. The honest width statements are the central-lobe width or the half-power width, and the bandwidth theorem is respected trivially (). Sharp edges in one Fourier face always buy slow decay in the other: the top-hat's rms is perfectly finite while is not.
Step 5. Moral: brick-wall spectral edges produce long oscillatory tails (diffraction ringing, the Gibbs phenomenon), which is why real monochromators taper their edges — and why the edge-free Gaussian is the shape with no ringing at all.
The man who taught waves to add
Origins · 1 minJoseph Fourier and how this was discovered
Fourier built the mathematics this article runs on — while studying how heat flows through solids. Orphaned at nine, nearly guillotined in the Revolution, then Napoleon's scientific advisor in Egypt and a French prefect, he wrote his masterpiece in stolen hours: the claim that any reasonable function can be assembled from sinusoids. His 1807 memoir was rejected — Lagrange himself refused to believe discontinuous functions could be built from smooth waves — and Fourier spent fifteen years sharpening the case until the 1822 Théorie analytique de la chaleur made it unanswerable. He never knew his integral would become the grammar of quantum mechanics: that "momentum content" would mean Fourier transform, or that his width-versus-bandwidth reciprocity would resurface as the uncertainty principle. Every packet synthesized in this article, every extracted from a , runs on machinery he built to explain warm iron.
Going further
References. Griffiths, Introduction to Quantum Mechanics, 3rd ed., §2.4 (the free particle) · Shankar, Principles of Quantum Mechanics, 2nd ed., Ch. 5 (Gaussian wave packets) · Sakurai & Napolitano, Modern Quantum Mechanics, 2nd ed., §2.4 · Cohen-Tannoudji, Diu & Laloë, Quantum Mechanics, Vol. I, Complement G_I · Townsend, A Modern Approach to Quantum Mechanics, 2nd ed., Ch. 6 Key relations underlying this article: the Fourier-pair normalization rests on the completeness relation ; both Gaussian derivations use the standard integral ; the Gaussian minimum-uncertainty product is with and ; and the time-dependent spreading width is , with characteristic spreading time — the latter is treated in full in Wave Packet Spreading and Dispersion.
Builds on: Free Particle and Plane Waves · Time-Independent Schrödinger Equation in One Dimension · Bound States versus Scattering States
Leads to: Group Velocity versus Phase Velocity · Wave Packet Spreading and Dispersion
Is φ(k) actually measurable, or is it just a mathematical device?
Measurable, and routinely. Switch off a trap and let the packet fly: after a long time of flight, position sorts by momentum (the fast components end up far away), so a camera image of the expanded cloud is up to scaling. This is exactly how cold-atom experiments photograph momentum distributions, and how Bose–Einstein condensation was seen in 1995 — as a sudden narrow spike growing in the middle of a time-of-flight image. Electron spectrometers do the same job with fields instead of flight time.
If real particles are packets, why do we solve scattering problems with plane waves?
Because a beam packet is monochromatic to a fraction of a percent (Example 1: 1000 crests, ), and amplitude ratios like reflection and transmission coefficients vary smoothly with . The packet answer is the plane-wave answer averaged over a percent-wide band — indistinguishable in practice. Plane waves compute the physics; packets certify that the idealization is controlled. When barrier features are sharp on the beam's bandwidth scale (resonances!), the packet's width does matter — a story taken up with the transfer-matrix tools later in this chapter.
Can a wave packet have several separate humps, or must it be one lump?
Any normalizable shape is legal — including two disjoint humps, exactly what a double slit or beam splitter produces. That is one particle in a superposition of two places, not two half-particles: a single detection fires in one hump only, with the humps' weights as probabilities. Recombine them and they interfere — proof both pieces were present.
What sets the width of a real particle's packet in the lab?
The preparation, not the particle. An aperture stamps its size onto ; a monochromator or the source's energy spread fixes ; laser cooling sets an atom's through the photon recoil budget. There is no intrinsic "true width" of an electron's packet — an electron leaving a hot filament and the same electron after a velocity selector carry different . The state describes the particle as prepared, which is why identical particles in different apparatus have different packets.
Is the packet-level uncertainty relation the same theorem as the Heisenberg uncertainty principle?
Same content for the position–momentum pair, different generality. Here is the Fourier bandwidth theorem — a statement about any transform pair, quantum or not. The operator formulation generalizes it to any two observables, with the bound set by their commutator (), of which position–momentum is the special case . That machinery, plus what "minimum-uncertainty state" means for other pairs, is the Generalized Uncertainty Principle of the formalism chapter.
Does the packet keep its shape as time runs?
Only for one instant is the question even fair — motion and shape change are dynamics, deliberately excluded here. The preview: each component accumulates its own phase ; the linear part of slides the envelope rigidly at the group velocity (Group Velocity versus Phase Velocity), and the quadratic part dephases the components so a free packet always spreads (Wave Packet Spreading and Dispersion). In a harmonic potential the spacing of 's becomes even and special Gaussian packets — coherent states — orbit forever without spreading; that miracle is the Coherent States of the Harmonic Oscillator story later in this chapter.