Observation of magnetically-induced transition intensity redistribution in the onset of the hyperfine Paschen-Back regime

Abstract

The Zeeman effect is an important topic in atomic spectroscopy. The induced change in transition frequencies and amplitudes finds applications in the Earth-field-range magnetometry. At intermediate magnetic field amplitude B∼B0=Ahfs/ΞΌBB\sim B_0 = A_\text{hfs}/\mu_B, where AhfsA_\text{hfs} is the magnetic dipole constant of the ground state, and ΞΌB\mu_B is the Bohr magneton (B0β‰ˆ1.7B_0\approx 1.7 kG for Cs), the rigorous rule Ξ”F=0,Β±1\Delta F = 0, \pm1 is affected by the coupling between magnetic sub-levels induced by the field. Transitions satisfying Ξ”F=Β±2\Delta F = \pm2, referred to as magnetically-induced transitions, can be observed. Here, we show that a significant redistribution of the Cs 6S1/2β†’6P3/26\text{S}_{1/2}\rightarrow 6\text{P}_{3/2} magnetically-induced transition intensities occurs with increasing magnetic field. We observe that the strongest transition in the group Fg=3β†’Fe=5F_g=3\rightarrow F_e=5 (Οƒ+\sigma^+ polarization) for B<B0B<B_0 cease to be the strongest for B>3B0B>3 B_0. On the other hand, the strongest transition in the group Fg=2β†’Fe=4F_g=2\rightarrow F_e=4 (Οƒβˆ’\sigma^- polarization) remains so for all our measurements with magnetic fields up to 9 kG. These results are in agreement with a theoretical model. The model predicts that similar observations can be made for all alkali metals, including Na, K and Rb atoms. Our findings are important for magnetometers utilizing the Zeeman effect above Earth field, following the rapid development of micro-machined vapor-cell-based sensors

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