Single-Photon Atomic Cooling - Raizen Lab - The University of ...
Single-Photon Atomic Cooling - Raizen Lab - The University of ...
Single-Photon Atomic Cooling - Raizen Lab - The University of ...
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process repeats. If however, it decays into the |J = 1/2,mJ = 1/2〉 state then<br />
it is trapped in a cycling transition and has no way <strong>of</strong> returning to the |J =<br />
1/2,mJ = −1/2〉 state. Note that the atom initially in the |J = 1/2,mJ =<br />
−1/2〉 state climbed a potential hill to reach the region <strong>of</strong> σ + polarization<br />
where it was optically pumped into the |J = 1/2,mJ = 1/2〉 state which has<br />
lower energy due to a larger downward light shift. <strong>The</strong> atom therefore lost<br />
the energy it used to climb the potential hill when it was transfered into the<br />
other ground state. This excess energy is carried away by the spontaneously<br />
emitted photon which has a higher frequency than the photon which excited<br />
the atom into the J ′ = 3/2 manifold. After decay, the atom finds itself at the<br />
bottom <strong>of</strong> a potential valley in the |J = 1/2,mJ = 1/2〉 state. If it climbs to<br />
the top <strong>of</strong> this potential valley it will be in a region <strong>of</strong> σ − polarization and<br />
will be pumped into the |J = 1/2,mJ = −1/2〉 state losing more energy in the<br />
process. This repeated cycle <strong>of</strong> climbing a potential hill only to be pumped<br />
into a valley is called the ‘Sisyphus’ effect after a character in Greek mythology<br />
condemned by the gods to a similar fate.<br />
This simple picture suggests that this cooling mechanism works until<br />
the atoms no longer have sufficient energy to climb the potential hills and are<br />
stuck in the valleys. A final temperature can be estimated with this picture<br />
in mind [70]<br />
kBT ≈ Udip ∝ I<br />
. (2.83)<br />
|∆|<br />
where Udip can be estimated from Eq. 2.53. Of course this technique also<br />
has a limit and cannot be used to cool atoms to 0 K as ∆ → 0 . When the<br />
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