Abstract
A survey of the α-satellites from Ge (32) to Mg (12) reveals new lines in the Kα series, from the element Ca (20) to Va (23). The Kα3.4 doublet is resolved over five additional elements, from Ca (20) to Mn (25). The Kα3 line is shown to have two components, Kα3 and Kα3, over the range of elements Al (13) to Cl (17). Microphotometer records, tracings of which are shown, reveal a significant reversal in the relative intensity of Kα3 and Kα4. This reversal is an atomic phenomenon and is not dependent upon chemical combination.

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