Abstract
THE successful accomplishment of separating the isotopes of mercury (NATURE, 106, 144, 1920; Phil. Mag. 43, 31, 1922) suggested an investigation to determine the extent to which samples of mercury from different sources might show the same atomic weight, i.e. the same density, which is to be expected only if the various minerals contain the isotopes in the same ratio.
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BRÖNSTED, J., HEVESY, G. The Atomic Weight of Mercury from Different Sources. Nature 109, 780 (1922). https://doi.org/10.1038/109780a0
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DOI: https://doi.org/10.1038/109780a0
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