Oklo

Coordinates: 1°23′40″S 13°9′39″E / 1.39444°S 13.16083°E / -1.39444; 13.16083
Source: Wikipedia, the free encyclopedia.
The natural nuclear fission reactors of Oklo:
  1. Nuclear reactor zones
  2. Sandstone
  3. Uranium ore layer
  4. Granite

Oklo is a region near the town of

Haut-Ogooué province of the Central African country of Gabon. Several natural nuclear fission reactors were discovered in the uranium mines
in the region in 1972.

History

Gabon was a French colony when prospectors from the

Orano Cycle) discovered uranium in the remote region in 1956. France immediately opened mines operated by Comuf (Compagnie des Mines d'Uranium de Franceville) near Mounana
village to exploit the vast mineral resources, and the State of Gabon was given a minority share in the company.

For 40 years, France mined uranium in Gabon. Once extracted, the uranium was used for electricity production in France and much of Europe. Today the uranium deposits are exhausted, and the mine is no longer worked. Currently, mine reclamation work is ongoing in the region affected by the mine operations.

Natural nuclear fission reactor

Some of the mined uranium was found to have a lower concentration of uranium-235 than expected, as if it had already been in a reactor. When geologists investigated they also found products typical of a reactor. They concluded that the deposit had been in a reactor: a natural nuclear fission reactor, around 1.8 to 1.7 billion years BP – in the Paleoproterozoic Era during Precambrian times, during the Statherian period – and continued for a few hundred thousand years, probably averaging less than 100 kW of thermal power during that time. At that time the natural uranium had a concentration of about 3% 235U, and could have reached criticality with natural water as neutron moderator allowed by the special geometry of the deposit.[1][2][3][4][5][6][7]

See also

References

External links

1°23′40″S 13°9′39″E / 1.39444°S 13.16083°E / -1.39444; 13.16083

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