Physical Review · 1946 · 18 citations · 6 references
Natural SciencesChemistryEarth SciencesElemental AnalysisGeochemistryNuclear ChemistryActivity MeasurementAlpha DecayNuclear DecayRadioactive DecayRadiochemical AnalysisStable Isotope AnalysisElemental AbundancesHalf-life MeasurementIsotopic Abundance RatiosIsotopic AbundancesNuclear Half-lifeRadioactive Half-lifeUranium AnalysisUranium Isotopic Composition
The half-life of ${\mathrm{U}}_{234}$ has been determined by two independent methods. The first method involves a re-measurement of the relative isotopic abundance of ${\mathrm{U}}_{234}$ and ${\mathrm{U}}_{238}$ in normal uranium; from this measurement the half-life of ${\mathrm{U}}_{234}$ can be obtained in terms of the known half-life of ${\mathrm{U}}_{238}$. The value obtained by this method is 2.29\ifmmode\pm\else\textpm\fi{}0.14\ifmmode\times\else\texttimes\fi{}${10}^{5}$ years. The second method involves the determination of the specific $\ensuremath{\alpha}$-activity of ${\mathrm{U}}_{234}$ from the total specific $\ensuremath{\alpha}$-activity and relative isotopic abundances of several enriched uranium samples. The value obtained by this method is 2.35\ifmmode\pm\else\textpm\fi{}0.14\ifmmode\times\else\texttimes\fi{}${10}^{5}$ years. Both values for the half-life are somewhat smaller than the currently accepted value of 2.69\ifmmode\pm\else\textpm\fi{}0.27\ifmmode\times\else\texttimes\fi{}${10}^{5}$ years.
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