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Non-dispersive wave packets in periodically driven quantum systems

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A. Buchleitner et al. / Physics Reports 368 (2002) 409–547 541<br />

procedure—we still need some means to prove that we really did populate the <strong>wave</strong> packet. As<br />

a matter of fact, to provide unambiguous experimental evidence, one has to test various characteristic<br />

properties of the <strong>wave</strong> packet, so as to exclude accidental co<strong>in</strong>cidences. A natural way is<br />

Floquet spectroscopy (see Section 8.2), i.e. prob<strong>in</strong>g the structure of the Floquet quasi-energy levels,<br />

<strong>in</strong> either the optical or the micro<strong>wave</strong> regime (via absorption, stimulated emission, Raman spectroscopy<br />

etc.). Another possibility is to explore unique properties of <strong>wave</strong> packet Floquet states. For<br />

example, as discussed <strong>in</strong> Section 7.1, these states exhibit extremely small ionization rates. Hence,<br />

an experimentally accessible quantity to identify these states is the time dependence of their survival<br />

probability, i.e., of the probability not to ionize dur<strong>in</strong>g an <strong>in</strong>teraction time t. It is given by<br />

[43,97]<br />

P(t)= |c | 2 exp(− t) ; (285)<br />

where the c denote the expansion coe cients of the <strong>in</strong>itial eld-free state <strong>in</strong> the Floquet basis, at<br />

a given value of micro<strong>wave</strong> amplitude F.<br />

If the selective population of the <strong>wave</strong> packet is successful, only one Floquet state contributes<br />

to P(t), and the decay of the population to the atomic cont<strong>in</strong>uum should manifest <strong>in</strong> its exponential<br />

decrease, as opposed to a multiexponential decrease <strong>in</strong> the case of a broad distribution of the<br />

c over the Floquet states [43,145,206–208,220]. Of course, the dist<strong>in</strong>ction between an exponential<br />

and an algebraic decay law requires the variability of the experimental <strong>in</strong>teraction time over more<br />

than one order of magnitude. This is a nontrivial task <strong>in</strong> experiments on atomic Rydberg states<br />

of hydrogen, s<strong>in</strong>ce the typical velocities of the atomic beam are of the order of 1000 m=s. That<br />

signi cantly restricts the <strong>in</strong>terval on which the <strong>in</strong>teraction time may be changed, tak<strong>in</strong>g <strong>in</strong>to account<br />

the typical size (<strong>in</strong> the cm-range) of the atom– eld <strong>in</strong>teraction region [133,228]. However,<br />

the feasibility of such measurements has already been demonstrated <strong>in</strong> micro<strong>wave</strong> experiments on<br />

rubidium Rydberg states, where the <strong>in</strong>teraction time has been scanned from approx. 100 to approx.<br />

100 000 eld cycles, i.e., over three orders of magnitude [220,221]. Note that, whereas the<br />

dynamics of the <strong>driven</strong> Rydberg electron along a Kepler ellipse of large eccentricity will certa<strong>in</strong>ly<br />

be a ected by the presence of a non-hydrogenic core, non-<strong>dispersive</strong> <strong>wave</strong> <strong>packets</strong> as the ones<br />

discussed <strong>in</strong> Sections 3.4 and 3.5 can certa<strong>in</strong>ly be launched along circular trajectories, s<strong>in</strong>ce the<br />

Rydberg electron of the rubidium atom essentially experiences a Coulomb eld on such a circular<br />

orbit.<br />

To use the character of the decay as a means to identify the <strong>wave</strong> packet, the micro<strong>wave</strong> eld<br />

amplitude should be su ciently large to guarantee that other Floquet states localized <strong>in</strong> the chaotic<br />

sea (see Section 7.1) decay rapidly. Otherwise, the observation of a mono-exponential decay simply<br />

suggests that we succeeded <strong>in</strong> populat<strong>in</strong>g a s<strong>in</strong>gle Floquet state—not necessarily a <strong>wave</strong> packet<br />

[220]. The appropriate choice of the driv<strong>in</strong>g eld amplitude F, such that appreciable ionization<br />

is achieved for the longer experimentally accessible <strong>in</strong>teraction times, should therefore allow for<br />

the experimental identi cation of the mono-exponential decay from the <strong>wave</strong> packet to the atomic<br />

cont<strong>in</strong>uum, but also—by vary<strong>in</strong>g F—of the variations of the decay rate with F, which is predicted to<br />

uctuate wildly over several orders of magnitude, see Section 7.1. Note, however, that this requires<br />

an excellent homogeneity of the micro<strong>wave</strong> eld (e.g., provided by a high-quality micro<strong>wave</strong> cavity),<br />

as the uctuations take place over rather small <strong>in</strong>tervals of F.

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