Compton effect, increase in wavelength of X-rays and other energetic electromagnetic radiations that have been elastically scattered by electrons; it is a principal way in which radiant energy is absorbed in matter. The effect has proved to be one of the cornerstones of quantum mechanics, which accounts for both wave and particle properties of radiation as well as of matter. See also light: Early particle and wave theories.
The American physicist Arthur Holly Compton explained (1922; published 1923) the wavelength increase by considering X-rays as composed of discrete pulses, or quanta, of electromagnetic energy. The American chemist Gilbert Lewis later coined the term photon for light quanta. Photons have energy and momentum just as material particles do; they also have wave characteristics, such as wavelength and frequency. The energy of photons is directly proportional to their frequency and inversely proportional to their wavelength, so lower-energy photons have lower frequencies and longer wavelengths. In the Compton effect, individual photons collide with single electrons that are free or quite loosely bound in the atoms of matter. Colliding photons transfer some of their energy and momentum to the electrons, which in turn recoil. In the instant of the collision, new photons of less energy and momentum are produced that scatter at angles the size of which depends on the amount of energy lost to the recoiling electrons.
Because of the relation between energy and wavelength, the scattered photons have a longer wavelength that also depends on the size of the angle through which the X-rays were diverted. The increase in wavelength, or Compton shift, does not depend on the wavelength of the incident photon. The wavelength of the photon after (λ′) and before (λ) the scattering event differs by λ′ − λ = (h/mc)(1 − cos θ). Here h is Planck’s constant, m is the rest mass of the electron, c is the speed of light, and θ is the angle through which the photon is scattered.
The Compton effect was discovered independently by the Dutch physical chemist Peter Debye in early 1923.