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An atomic clock uses an atomic transition as a frequency reference for an oscillator; counting its calibrated cycles realizes a time interval. In a passive beam implementation, the chemical atoms are repeatedly prepared, interrogated and detected, while feedback control corrects the continuously running oscillator. The Ramsey separated oscillatory fields experiment explains how internal quantum phase becomes a measurable population signal.

The SI second fixes the unperturbed ground state hyperfine structure transition frequency of caesium-133 to exactly $9192631770\mathrm{Hz}$. This is a defining value for the ideal transition, rather than a guarantee that an operating apparatus has no shifts.^[ref]

An attosecond is one quintillionth of a second.

Attosecond physics resolves changes on the scale of $10^{-18}$ seconds, especially Electron dynamics. Its central trick is to convert a short optical event into an experimentally accessible energy or phase change. A broad optical spectrum provides the ingredients for a short optical pulse; their spectral phases determine when those ingredients add constructively. High harmonic generation supplies the optical spectrum, while RABBITT and attosecond streaking supply complementary timing measurements. XUV denotes extreme ultraviolet radiation.

There are two separate timing problems: characterize the incident optical pulse, then infer the response of the target. A photoelectron measurement mixes the incident spectral phase, the target's transition response and the probing electric field. Recovering one requires constraints on the others. These methods measure distributions of photoelectron energies over repeated shots, rather than photographing a moving atomic orbital.

One becquerel is a radioactive activity of one nuclear transformation per second.

A unit of time equal to $86400$ seconds.