The behavior of slow, fully stripped Ar¹⁸⁺ ions near metallic surfaces has been studied. These ions capture, while touching the surface, a large number of electrons in outermost shells, leading to the formation of ``hollow'' atoms. The timing of the hypersatellite-satellite cascade filling the double K-vacancy states is studied in this paper by using the internal clock constituted by the ``tops'' of the temporal sequence filling stepwise the L shell of the ion.
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Briand et al. (1991) studied this question.
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