In nuclear physics, atomic recoil is the result of the interaction of an atom with an energetic elementary particle, when the momentum of the interacting particle is transferred to the atom as a whole without altering non-translational degrees of freedom of the atom. It is a purely quantum phenomenon. Atomic recoil was discovered by Harriet Brooks, Canada's first female nuclear physicist, in 1904, but interpreted wrongly. Otto Hahn reworked, explained and demonstrated it in 1908/09.[1] The physicist Walther Gerlach described radioactive recoil as "a profoundly significant discovery in physics with far-reaching consequences".[2]
If the transferred momentum of atomic recoil is enough to disrupt the crystal lattice of the material, a vacancy defect is formed; therefore a phonon is generated.
Closely related to atomic recoil are electron recoil (see photoexcitation and photoionization) and nuclear recoil, in which momentum transfers to the atomic nucleus as whole. Nuclear recoil can cause the nucleus to be displaced from its normal position in the crystal lattice, which can result in the daughter atom being more susceptible to dissolution. This leads for example to an increase in the ratio of 234U to 238U in certain cases, which can be exploited in dating (see Uranium–thorium dating).[3][4]
In some cases, quantum effects can forbid momentum transfer to an individual nucleus, and momentum is transferred to the crystal lattice as a whole (see Mössbauer effect).
- ^ Hahn 1966, pp. 58–64.
- ^ Gerlach & Hahn 1984, p. 39.
- ^ M. B. Anderson; et al. (Dec 8, 2010). "Precise determination of the open ocean 234U/238U composition". Geochemistry, Geophysics, Geosystems. 11 (12). doi:10.1029/2010GC003318. S2CID 129292401.
- ^ Simon Turner; et al. (Jan 8, 2021). "Carbonaceous chondrite meteorites experienced fluid flow within the past million years". Science. 371 (6525): 164–167. doi:10.1126/science.abc8116. PMID 33414218. S2CID 231138500.