Abstract
The solubility of hydrogen in nickel and cobalt at atmospheric pressure has been measured over large temperature ranges. Large departures from Arrhenius behavior have been found for polycrystalline nickel and cobalt, but equilibrations using a nickel single crystal did not show curvature in the Arrhenius plot. The measured solubility data have been interpreted using a solid solution model involving sites of differing energy at which solute atoms can be located.
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