Atom interferometry 2026-10-14
Cold atom 2026-10-18
In 2014, Gabriele Rosi and colleagues used atom interferometry: two rubidium-87 clouds prepared by laser cooling in vacuum, apart, received shared three-pulse Raman transitions spaced by . Fluorescence readout and paired-fringe ellipse fitting yielded differential wave phase. Twenty-four tungsten alloy cylinders, about total, moved between C and F. Cloud subtraction rejected shared vibration; configuration subtraction isolated the source change.[ref]
Precision Measurement of the Newtonian Gravitational Constant Using Cold Atoms by Gabriele Rosi and others. Main text pp. 3–5; Methods pp. 13–14; Fig. 1 caption p. 21
Precision Measurement of the Newtonian Gravitational Constant Using Cold Atoms by Gabriele Rosi and others. Main text pp. 3–5 and Fig. 1 caption p. 21
Details.Calibration used timed flight and light-sheet crossings; mirror tilt compensated Earth rotation. Wave vector reversal rejected unwanted shifts. Modeling included source Newtonian gravitational potential, atom trajectories, cloud distributions and moving supports. Source positioning, mass density variation and cloud geometry limited the reported combined relative standard uncertainty to parts per million.[ref]
Precision Measurement of the Newtonian Gravitational Constant Using Cold Atoms by Gabriele Rosi and others. Main text pp. 5–6; Methods pp. 14–18; Table 1, p. 27
To understand the subtraction without reproducing that full analysis, consider an ideal atom interferometer in uniform vertical acceleration during each pulse sequence. Let be its signed effective vertical wave vector component and the pulse spacing. Its acceleration-dependent wave phase is ; labels U and L denote upper and lower clouds. The double difference is thenA background field identical in C and F cancels even if it differs between the two clouds. In a fixed-geometry, linear-response model, write , where is calculated from the source mass density, calibrated pulse sequence and atom trajectories. Thus . Measuring wave phase accurately is one part of the task; calculating accurately is another. The real nonuniform field and finite clouds require the trajectory-dependent analysis described above rather than this uniform-field approximation.
G. T. Foster 2026-10-13
Guglielmo Maria Tino Created 2026-10-14 Updated 2026-10-31
Laser cooling Created 2026-10-14 Updated 2026-10-18
Laser cooling uses laser light to reduce the random velocities of chemical atoms, and therefore their translational temperature. The striking ingredient is selective photon absorption: an atom moving towards a beam sees a Doppler shift that can make it absorb more strongly. Each absorbed photon transfers momentum along the beam; repeated absorption and spontaneous emission can then remove kinetic energy. Doppler cooling makes this selection with the atom's motion, while sub-Doppler cooling also exploits its internal quantum states.
Cooling makes chemical atoms move slowly enough for longer interrogation in atomic clocks and atom interferometry, and easier loading into an optical trap. The same radiation pressure that pushes an atom can cool it: with suitably tuned opposing beams, whichever direction the atom moves, it receives the stronger push against that motion.
Marco Prevedelli Created 2026-10-14 Updated 2026-10-31
M. J. Snadden 2026-10-13
Laser cooling removes atomic kinetic energy through a velocity-dependent optical force, with scattered photons carrying away energy and entropy. For two counterpropagating beams detuned below resonance, motion towards one beam shifts that light closer to resonance, so the atom preferentially absorbs momentum opposite its velocity. At small velocity the net force is with . Three orthogonal beam pairs form optical molasses. Spontaneous emission has zero mean recoil in a symmetric distribution, but its momentum variance is nonzero: random absorption and emission cause heating. The cooling and heating balance sets a finite temperature.
For a weakly saturated two-level transition, write and let be the excited-state population decay rate. A useful one-axis Doppler cooling expression isThis limit belongs to the weak-intensity Doppler cooling model, with recoil energy small compared with . Experimentally, released sodium molasses clouds were probed by time of flight; the unusually small expansion demonstrated temperatures below that limit. This distinguishes an observed failure of a two-level cooling model from a failure of conservation of energy.[ref]
Nobel Lecture: Laser cooling and trapping of neutral atoms by William D. Phillips. pp. 729–732, Doppler limit, optical molasses, and release/time-of-flight thermometry
Multilevel atoms permit polarization-gradient cooling: spatially varying light polarization produces different light shifts of ground-state sublevels. In Sisyphus cooling, atoms climb a light-shift potential and are preferentially optically pumped near its top into a lower-energy sublevel, repeatedly losing kinetic energy. The optical pumping and emitted light supply dissipation. This can reach below the Doppler cooling limit; the recoil scalethen becomes important. The definition of a recoil temperature sometimes differs by a factor of two, so the energy definition is the unambiguous comparison. Recoil is not a universal lower bound for every cooling protocol: suitable dark-state or resolved sideband cooling schemes can suppress scattering near the desired motional state. Resolved sideband cooling preferentially excites a transition lowering the vibrational quantum number, followed by decay that on average preserves it in the Lamb-Dicke regime.[ref]
Nobel Lecture: Superposition, entanglement, and raising Schrödinger’s cat by David J. Wineland. Section IV, cooling of quantized ion motion
Optical molasses supplies damping rather than a position-restoring force. A magneto-optical trap adds a magnetic-field gradient and appropriately chosen circular polarizations; the position-dependent Zeeman splitting gives a restoring radiation pressure imbalance as well as damping. In real alkali atoms, repumping light returns population that would otherwise accumulate in an uncoupled hyperfine level. Magnetic and optical dipole traps can subsequently hold the cold sample without continuous resonant scattering.
Applications include long-interrogation atomic clocks, precision spectroscopy, atom interferometry, and preparation for quantum simulation and Bose-Einstein condensation. Cooling reduces motion-induced frequency shifts and allows longer coherent interrogation; deeper quantum degeneracy commonly needs subsequent evaporative cooling of atoms. Finite capture velocity, available transitions, recoil heating, stray magnetic fields, and loss or heating from unwanted scattering constrain a real experiment.
Raman transition 2026-10-14
