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The α-recoil effects of uranium in the Oklo reactor

Abstract

Until recently, it was thought that chemical elements were synthesized only in stars. The discovery of the Oklo phenomenon1–6 in 1972 revealed, however, that there was a nuclear ‘fire’ on the Earth 1,700 Myr ago. We have now carried out a series of acid-leaching experiments on a sample of uranium ore from reactor zone no. 10 of the Oklo mines in Gabon, Africa, and observe anomalously high 234U/238U ratios accompanied by modestly increased 235U/238U ratios in uranium fractions. These results, which can be interpreted as being due to the α-recoil effects of 238U and 239Pu, provide a convenient way of calculating the conversion factor (or the fraction of uranium atoms converted to plutonium) of the natural reactors from radiochemical data, obviating the necessity for mass-spectrometric measurements.

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Sheng, Z., Kuroda, P. The α-recoil effects of uranium in the Oklo reactor. Nature 312, 535–536 (1984). https://doi.org/10.1038/312535a0

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