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Carbonaceous matter, association with uranium

Gentry et al. (1976) have recently shown, on the basis of isotopic analyses, that uranium introduction may have occurred far more recently than was previously supposed. However, they find also that, in some instances, the uranium was introduced before coalification was complete since the haloes have been compressed with the coal as it increased in rank. These results are consistent with laboratory and field work by Szalay (1964) who showed that the insoluble humic acids in peat are capable of concentrating uranium from very dilute solutions in natural waters. Sorption occurs as uranyl humate , the process following the normal kinetics of the Langmuir adsorption equation. (Where uraninite occurs in association with peat or other carbonaceous matter, the uranium may thus have been initially sorbed as a uranyl compound which was later reduced to uraninite.)... [Pg.494]


See other pages where Carbonaceous matter, association with uranium is mentioned: [Pg.492]    [Pg.492]    [Pg.860]    [Pg.860]    [Pg.495]    [Pg.500]    [Pg.500]    [Pg.501]    [Pg.502]    [Pg.503]    [Pg.504]    [Pg.7005]    [Pg.323]   
See also in sourсe #XX -- [ Pg.492 , Pg.500 ]




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Carbonaceous

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