Isotopic disequilibrium effects in leaching of natural uraninite and thorianitc

Details Isotopic disequilibrium effects in leaching of natural uraninite and thorianitc Isotopic disequilibrium effects in leaching of natural uraninite and thorianitc

Sep 1987

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1987gecoa..51.2593v&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 51, Issue 9, pp.2593-2594

Physics

1

Scientific paper

Fractional leach rates of 228 Th that are greater than those of 232 Th
from natural uraninite and thorianite have been interpreted by Eyal and
Fleischer in terms of -decay damage to the crystal lattice. An
alternative interpretation proposed here is that the enhanced leaching
of 228 Th is due to its presence as interstitial ions.

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