Alfred Kastler's 1966 lecture recalls his 1950 proposal and distinguishes the early atomic beam work from later sealed-vapour experiments. Its Fig. 5 shows subsequent sodium radio wave resonances, including multiple-photon transitions.[ref]
The 1952 demonstration by Jean Brossel, Alfred Kastler and Jacques Winter used a sodium atomic beam, lamp light with circular polarization and fluorescence readout. Jean Brossel was a central experimental contributor; Alfred Kastler received the 1966 Nobel Prize in Physics alone.[ref][ref]
The lecture also describes a experiment: a pumping beam with circular polarization prepares the vapour, while a perpendicular probe converts transverse magnetic dipole moment Larmor precession into modulated absorption at a photodetector. Interrupting pump and RF together exposes decaying free Larmor precession. Its envelope measures transverse relaxation under that model; it is distinct from the sodium atomic beam fluorescence signal.[ref]
MIT's later rubidium experiment pumps natural / with a discharge lamp filtered to D1 (, near ). A polarizer and quarter-wave plate precede a heated rubidium/neon cell. Helmholtz coils set a weak static magnetic field. Separate transverse RF mixing increases absorption, measured by photodiode transmission.[ref]
Figure 1.
Vapour-cell preparation and optical transmission readout
. Original functional schematic of the later rubidium-cell apparatus. Geometry is schematic; lamp and interrogation drives are separate. Details.
Compare resonant and detuned RF with the optical beam fixed, then change the calibrated static magnetic field: a true magnetic sublevel resonance should move with its Zeeman splitting. Lamp drift, stray magnetic fields, imperfect circular polarization, optical attenuation and RF power broadening can change the observed signal. Consequently, a transmission dip alone does not determine every sublevel population. These are measurement-design considerations, not additional reported historical observations.
Optical pumping Created 2026-10-14 Updated 2026-10-18
Optical pumping redistributes populations among internal quantum states by selective photon absorption followed by spontaneous emission. It can prepare atoms for measurement and participate in sub-Doppler cooling.
The practical aim is to make otherwise almost equally populated magnetic sublevels behave differently. Repeated absorption and emission can store a population imbalance in the long-lived ground state; a change in photon absorption or fluorescence then reveals a perturbation of that prepared distribution. This combines preparation and measurement: a weak radio wave can reorganize the populations, while abundant optical photons supply the readout.
An imbalance among ground state magnetic sublevels need not be a population inversion between optical energy levels. Optical pumping also supplies excitation in some lasers, where an appropriate population inversion matters for gain. The preparation problem here concerns the distribution within the ground state. A two-level system with only one lower quantum state cannot describe this redistribution.
Circular polarization selects the sign of the absorbed photon's angular momentum along the beam. Choose that direction as and define by the absorption rule , where is the magnetic quantum number. Spontaneous emission can return an atom to a different magnetic sublevel, so absorption followed by emission is a population-transfer cycle. A sublevel that the chosen beam cannot excite is dark to that beam. Darkness is relative to the selected transition and electromagnetic polarization, rather than a claim that the atom cannot interact with any light.
A static magnetic field along defines a stable axis and gives Zeeman splitting. A transverse oscillating magnetic field can redistribute magnetic sublevel populations when its frequency matches an allowed splitting. With the appropriate optical transition, that redistribution restores photon absorption: transmitted intensity decreases, or collected fluorescence increases. These are alternative readouts whose detailed sensitivity depends on the transition, viewing direction and electromagnetic polarization.
Sisyphus cooling 2026-10-18
Finite optical pumping time lets an atom climb a light-shift hill before transfer into a lower magnetic sublevel. Spontaneous emission dissipates the gained potential energy; climbing alone is conservative.[ref]
To make the geometry and signs explicit, take an original choice of phase origin for equal opposing waves:
The real electric field is ; is wavelength. The fractions are squared projections onto the defined circular basis vectors, divided by total intensity. Their sum is one: interference changes electromagnetic polarization despite constant total intensity. At the field is respectively ; halfway between these positions it is linearly polarized. Specifying the vectors avoids an observer-dependent verbal handedness convention.
For an illustrative angular momentum transition, use the squared Clebsch-Gordan coefficients and for the strong and weak circular couplings from each lower magnetic sublevel. Interchanging circular components interchanges these strengths. The weighted sums are and . Rescaling their common negative shift gives
Both potential energies are negative relative to the unilluminated level. Each hill has height , and opposite hills are displaced by . An atom starting at the minimum at loses of kinetic energy if it reaches on that branch. A pump transfer there lowers its potential energy by , leaving it at a minimum. The next uphill segment ends at , where the favoured transfer is reversed. Actual transfers are stochastic and need not occur exactly at these extrema.
Figure 1.
Polarization geometry, shifted ground states and a Sisyphus energy cycle
. Original schematic: pumping arrows join occupied hilltops to opposite minima. Ideal completed cycles neglect recoil; actual transfers are stochastic. Details.
For one completed climb and pump, conservation of energy gives , while the ground-state potential energy returns to its starting value. Neglecting recoil and treating the scattered photon as the sole outgoing radiation change, . A potential drop is an internal-state reset, not an automatic equal upward kick in kinetic energy. Random emission nevertheless adds momentum fluctuations and recoil energy, so useful cooling requires the dissipated energy to compete with that heating.
The recoil energy sets a different scale from . Conventional Sisyphus cooling reaches the recoil regime when reducing the hill height also weakens cooling; it is not a claim of arbitrarily small temperature at vanishing intensity. Subrecoil techniques need further physics.[ref]
A Zeeman slower prepares a slow beam for capture; a narrow longitudinal velocity group is not by itself a cold three-dimensional cloud. The historical apparatus measured slowed-beam velocities with a separate fluorescence probe scanned in frequency, just after switching off the slowing beam. This avoided simultaneous-beam complications.[ref]
For an original resonance-tracking calculation, let atoms travel along with and the slowing beam along , so its atom-frame angular frequency is . Approximate the selected cycling transition by on one field branch; is its signed angular frequency shift per unit magnetic field. A multilevel atom may require a nonlinear outside that branch. Maintaining a chosen effective laser detuning requires
For chosen constant deceleration magnitude , gives and length . Substitution supplies a square-root magnetic field profile, plus a constant offset. The signs follow from the specified directions; reversing the selected transition's magnetic slope reverses the required field variation.
As a hypothetical design, take , and . The required length is and flight time . For chosen and , photon recoil velocity implies roughly directed absorption events. The mean required scattering rate is about . This budget must lie below the available scattering rate, with margin for capture and intensity variation. Optical pumping into unwanted hyperfine structure or magnetic sublevels can interrupt the cycle. Longitudinal slowing, transverse recoil heating and final cloud temperature are separate quantities.