de Broglie wavelength Created 2026-09-28 Updated 2026-10-14
The de Broglie wavelength is the distance over which a matter wave accumulates one full spatial quantum phase cycle in its propagation direction:
Here is the Planck constant, is the momentum, and is the angular wavevector. The scalar in means the positive momentum magnitude, not a signed component. Reversing a momentum reverses the wavevector without making the wavelength negative. At zero momentum there is no finite spatial phase period: the limiting wavelength diverges.
This relation makes microscopic diffraction accessible with particles: increasing the momentum shortens the wavelength until it is comparable with the spacings in a crystal scattering problem. The electron accelerating-voltage wavelength gives a practical way to tune this scale, while the Davisson–Germer experiment tests it by comparing electron diffraction directions with independently known crystal geometry. The same relation applies to neutral particles in a neutron interferometer; electric charge is not a requirement for a matter wave.
The wavelength belongs to the wavefunction, not to a sinusoidal path of a particle. A free-particle momentum convention makes the distinction especially clear: a plane wave has a rotating complex quantum phase but a constant probability density. A localized wave packet contains a range of momenta and therefore generally has a range of wavelengths, rather than one exact spatial period.
Electron diffraction 2026-10-14
Electron diffraction is interference between scattered Electron probability amplitudes. It connects the de Broglie wavelength of the incident beam to the arrangement of the scattering material. In elastic scattering from a fixed crystal, , and constructive crystal scattering selects wavevector transfers in the reciprocal lattice. The physical momentum transfer to the Electron is in this convention.
Bragg's law expresses the same condition as , where is the spacing of the chosen lattice planes, the diffraction order, and the angle to those planes. The angle between incoming and outgoing propagation directions is for that reflection geometry. In normal-incidence backscattering, a detector's angle from the outward surface normal instead gives ; neither detector colatitude nor angle to the surface normal should silently replace . A finite-row electron diffraction model uses a different spacing, the spacing between sites along a surface row, and makes that distinction explicit.