Davisson–Germer experiment Created 2026-10-14 Updated 2026-10-25
The Davisson–Germer experiment turned elastic scattering from nickel into evidence for a matter wave. The search became a deliberate wave test in 1926, with diffraction beams found early in 1927. The earlier crystal investigation had begun in 1925; the de Broglie wavelength proposal was already present in the 1924 thesis.[ref]
A heated tungsten ribbon supplied electrons; gun apertures selected a narrow beam. Two apertures were apart; the gun ended from a nickel crystal cut parallel to its planes. An adjustable electric potential difference set the speed. The beam struck normally inside an evacuated, field-free enclosure with target and outer electrodes at one potential. A double-box collector, from the target with a entrance, selected directions. A retarding electric potential difference rejected slower electrons; the inner collector fed a sensitive galvanometer. Moving the collector scanned colatitude; rotating the crystal scanned azimuth.[ref]
The readout was collected electric current, not a photograph of electron paths. Voltage scans held the gun-plate current constant because incident-beam current could not be held constant; the overall current trend therefore needed caution. A strong feature developed at near colatitude. Surface heating distinguished crystal beams from adsorbed-gas beams; finite apertures and background shifted or broadened apparent peaks.[ref]
At the bright beam's colatitude, an azimuth scan revealed three companion directions, matching crystal symmetry. The test compared wavelengths inferred from diffraction angles and known crystal spacings with wavelengths inferred from accelerating voltage and momentum; the 1937 lecture displayed this comparison against . Agreement across beam directions supplied more evidence than one angular peak.[ref]
Figure 1.
Original Davisson–Germer azimuth scan at 54 volts and colatitude 50 degrees
. Clinton J. Davisson and Lester Halbert Germer, Nature 119 (16 April 1927), p. 559, figure 2: galvanometer deflection against azimuth, recording scattered electron electric current at fixed colatitude. Scan cropped by Cirosantilli2 in 2023. Via Wikimedia Commons, public domain in the United States (PD-US-expired). Source.
The inference is about coherent quantum phases in scattering probabilities. It does not establish a wavy particle trajectory, and a collector-current experiment does not resolve individual detection events. Predicting the full intensity additionally requires the material's scattering amplitude, its surface condition, and instrumental angular acceptance; the de Broglie wavelength alone predicts none of those strengths. The following finite-row electron diffraction model isolates phase addition without attempting to reproduce the nickel measurements.
Schrödinger equation Created 2026-09-24 Updated 2026-10-20
The Schrödinger equation governs the evolution of a quantum state between instances of measurement in quantum mechanics. For a particle of mass moving in a prescribed real potential energy , its position wavefunction satisfies
Here is the Planck constant, is the Laplace operator, and the Hamiltonian operator combines kinetic energy with potential energy. Specify an initial wavefunction, an operator domain and any boundary conditions: the differential expression alone does not completely specify a physical model. The Born rule then turns the evolving probability amplitude into position probabilities through and integration over a region.
This scalar Schrödinger operator describes nonrelativistic quantum mechanics, with relevant momenta much smaller than , where is the speed of light. It omits the constant rest energy , assumes fixed particle number, and suppresses active spin dynamics and coupling to a magnetic vector potential. A free electron with a fixed, uncoupled spin state can still use this scalar model; the Pauli equation supplies the additional spin components and magnetic coupling when needed. A prescribed real describes a closed evolution model or an approximation in which the source of that potential energy is treated as external. Dissipation, particle creation and a general measurement in quantum mechanics need further modelling.
For a time-independent self-adjoint Hamiltonian operator, the spectral theorem defines unitary time evolution by
Initial states in the operator domain satisfy the differential equation in the Hilbert space sense; the unitary operator also evolves all other states in that Hilbert space. Time-dependent Hamiltonian operators need suitable regularity and domain hypotheses; their evolution is not generally the exponential of .
The local reason for conservation is especially tangible. Multiply the Schrödinger equation by the complex conjugate , subtract its conjugate multiplied by , and use the fact that the real potential energy terms cancel. For smooth wavefunctions this gives the probability continuity equation
The divergence theorem identifies the change in probability inside a region with minus the outward probability current. Decay at infinity, or appropriate probability-conserving boundary conditions, preserves wavefunction normalization. Conservation of total probability does not require a stationary probability density.
Its usefulness comes from being a linear partial differential equation: quantum superpositions of solutions are solutions, while different quantum phases can produce interference. For a fixed Hamiltonian operator, the time-independent Schrödinger equation finds the energy eigenstates; each then acquires just its own time-dependent quantum phase. One eigenvalue problem therefore organizes both allowed energies and the evolution of arbitrary quantum superpositions, with a continuous spectrum included when required. This is the attractive bridge between a spatial wave problem and a clock: energy differences determine the rate at which relative quantum phases change. It makes atomic spectral lines, quantum tunnelling and quantum scattering calculable from a specified model.
For an explicit example without confinement, take a free particle on the whole line, , initially in a Gaussian wave packet with position standard deviation and mean momentum :
Unlike a single plane wave, this wavefunction satisfies wavefunction normalization. A Fourier transform writes it as a quantum superposition of plane waves. Their dispersion relation is , so each Fourier component gains the factor . Completing the square in the resulting Gaussian integral gives
with the square root chosen continuously from . Its position probability density and standard deviation are
The centre moves with the group velocity and the wave packet spreads because different wavenumbers have different group velocities. This is unitary wave dispersion, without a random force or loss of probability. Independently, the initial momentum standard deviation is and the initial position-momentum covariance vanishes. Free evolution gives in the Heisenberg picture, hence
This independently checks the spreading law. The Gaussian integral of is one at every time; the decreasing peak is exactly offset by increasing width.
As hypothetical preparation parameters, choose a free electron with and . Using and gives
The rounded electron mass uses the 2022 adjustment.[ref] At , the centre is and ; at , they are and . The mean kinetic energy stays
It includes both mean motion and the momentum spread. The mean speed is about and the momentum spread corresponds to , making the nonrelativistic model accurate for the appreciably occupied part of this ideal Gaussian distribution. Its mathematically unbounded tails are an idealization.
Figure 1. . Calculated electron position probability densities for the hypothetical preparation above, together with the position standard deviation. The area under every curve is one. The dashed width curve illustrates pure translation without spreading for comparison; it is not the free solution. No curve represents measured data. Source. Details.
The complex width also explains where the probability goes. Write , where is the dimensionless quantum phase. Differentiating the exact solution gives
Relative to the moving centre, the probability current points outward on both sides for . This is a flux statement, not an additional assumption about individual particle trajectories. At and , the relative flow speeds are , about . The probability within a moving interval of half-width falls from about initially to at , exactly because of this outward probability current.
Figure 2.
Curved quantum phase drives spreading probability current
. The same free Gaussian wave packet at . With , removing the carrier and a spatially constant quantum phase leaves . The right panel plots : negative to the left, positive to the right. Flux through the marked moving interval endpoints explains its decreasing probability. Source. Details.
Historically, the 1926 Quantisierung als Eigenwertproblem (Erste Mitteilung) by Erwin Schrödinger began with the stationary hydrogen atom problem. It distinguishes discrete negative energies from a positive continuous spectrum; it is not yet the general evolution equation displayed above.[ref] The opening of quantum mechanics discusses its original vibrating-string analogy.
In the 12 December 1933 lecture The fundamental idea of wave mechanics by Erwin Schrödinger, Erwin Schrödinger explains the move from independent rays to waves through diffraction, then applies that analogy to atomic physics. His closing pages explicitly acknowledge the difficulty of reconciling wave language with observed particle tracks. This retrospective physical argument motivates the model; it does not derive the modern Born rule from classical mechanics.[ref]
The dates separate proposal from measurement: the de Broglie wavelength belongs to the 1924 thesis, the Schrödinger equation to 1926, and the Davisson–Germer experiment's electron diffraction beams to 1927.[ref] That linked experiment describes the prepared nickel crystal, evacuated electron gun, angular collector scans, retarding-potential selection and heating controls. Its measured collector electric current tests wave-dependent scattering probabilities; it neither measures a wavefunction directly nor establishes this equation uniquely.