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Title: Preferential leaching and natural annealing of alpha-recoil tracks in metamict betafite and samarskite

Journal Article · · J. Mat. Res.; (United States)
OSTI ID:5276120

Leaching experiments on naturally occurring, metamict betafite and samarskite minerals in a bicarbonate--carbonate solution show strongly enhanced release to the solution of short-lived /sup 228/Th relative to its parent isotope /sup 232/Th (by a factor of 3 to 6), but only slightly enhanced dissolution (by a factor of 1.2 to 2) of long-lived /sup 234/U and /sup 230/Th relative to /sup 238/U and /sup 232/Th, respectively. The betafite (a complex Ca--U--Ti--Nb oxide of the pyrochlore group, A/sub 2-//sub m/B/sub 2/X/sub 6/Y/sub 0-1/xH/sub 2/O) and samarskite (a complex Y--Fe--U--Nb oxide with varying stoichiometry between ABO/sub 4/ and AB/sub 2/O/sub 6/) are x-ray and electron diffraction amorphous having experienced doses of 2.2--2.8 x 10/sup 17/ alpha-decay events/mg (24--31 dpa) and 3.8--4.4 x 10/sup 17/ alpha-decay events/mg (39--45 dpa), respectively. The isotopic fractionation is attributed to the radiation damage created by the alpha-decay events. Individual alpha-recoil tracks are preserved for some time as disordered regions of higher chemical reactivity in already fully damaged, aperiodic areas that result from the alpha-decay events. The annealing time of the alpha-recoil track within the aperiodic atomic array of the metamict state is calculated to be 29,300 +- 8100 years for samarskite and 42,700 +- 13,700 years for the betafite. These data plus data on an earlier studied betafite sample (annealing time = 2000 +- 1300 years) give an average annealing time of 25,000 +- 21,000 years.

Research Organization:
Department of Geology, University of New Mexico, Albuquerque, New Mexico 87131
OSTI ID:
5276120
Journal Information:
J. Mat. Res.; (United States), Vol. 3:2
Country of Publication:
United States
Language:
English