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Ph.D. Thesis - Physics

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Figure 7-4: Scaling of the three secular frequencies in an elliptical trap as a function of<br />

ion height (trap scale). The 1/r0 scaling is assumed. Frequencies are angular, in units of<br />

2π s −1 . Blue corresponds to ωˆy, green to ωˆx, and red to ωˆz.<br />

We note, with the addition of ions, that the crystal transitions from an almost perfectly<br />

2-D shape to a 3-D shape whose extent along ˆz is still considerably less than that along<br />

ˆx and ˆy. We would now like to study how the extent into the vertical direction changes<br />

with ion number. To impart a sense of this, the order of magnitude of vertical extent of the<br />

crystal is plotted vs. ion number in Fig. 7-7.<br />

The results of this calculation are interesting: for small ion numbers, the crystal is<br />

almost perfectly planar, in that the extent along ˆz is orders of magnitude less than that<br />

along ˆx and ˆy, which is essentially zero. At 26 ions, the crystal transitions into a 3-D<br />

shape, for which the ˆz extent is about a tenth of the others. It alternates between this<br />

and the planar shape as additional ions are added, until above 30 ions it remains in the<br />

approximately planar 3-D state.<br />

Another important note is that this elliptical trap was made with a higher eccentricity<br />

than is probably required for breaking the degeneracy. For testing purposes, we decided<br />

to err on the side of caution. With this eccentricity, however, the crystal is less regular<br />

than it would be with a higher degree of symmetry. This situation has been studied by<br />

authors including those of Ref. [BKGH08]. In fact, it may be possible to create more-<br />

regular planar crystals for larger number of ions by increasing the ˆz motional frequency<br />

through the addition of a dc quadrupole field. In Ref. [BH09], it is noted that the condition<br />

for planar crystals in an ion trap is given by the following condition:<br />

ω2 ˆz<br />

ω2 ˆx<br />

<br />

70N<br />

><br />

π3 156<br />

1/2<br />

, (7.1)

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