Diamagnetic correction to the ${}^9$Be${}^{+}$ ground-state hyperfine constant

Abstract

We report an experimental determination of the diamagnetic correction to the ${}^9$Be${}^{+}$ ground state hyperfine constant $A$. We measured $A$ = $-625008837.371(11)$ Hz at a magnetic field $B$ of 4.4609 T. Comparison with previous results, obtained at lower values of $B$ (0.68 T and 0.82 T), yields the diamagnetic shift coefficient $k$ = $2.63(18)\times 10^{-11}$ T${}^{-2}$, where $A(B)=A_0\times (1+k{B}^2)$. The zero-field hyperfine constant $A_0$ is determined to be $-625008837.044(12)$ Hz. The $g$-factor ratio ${g_I}^{\prime }/g_J$ is determined to be $2.1347798527(10)\times 10^{-4}$, which is equal to the value measured at lower $B$ to within experimental error. Upper limits are placed on some other corrections to the Breit-Rabi formula. The measured value of $k$ agrees with theoretical estimates.

13 pages, 10 figures. Accepted by Physical Review A

References in corpus (2)

• Relativistic and QED corrections to the g factor of Li-like ions
• g factor of Li-like ions with nonzero nuclear spin

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