Porous fission fragment tracks in fluorapatite
- Department of Materials Science and Engineering, University of Michigan, Ann Arbor, Michigan 48109-2104 (United States)
- Department of Geological Sciences, University of Michigan, Ann Arbor, Michigan 48109-1005 (United States)
- GSI Helmholtz Centre for Heavy Ion Research, Planckstr. 1, 64291 Darmstadt (Germany)
Fission tracks caused by the spontaneous fission of {sup 238}U in minerals, as revealed by chemical etching, are extensively used to determine the age and thermal history of Earth's crust. Details of the structure and annealing of tracks at the atomic scale have remained elusive, as the original track is destroyed during chemical etching. By combining transmission electron microscopy with in situ heating, we demonstrate that fission tracks in fluorapatite are actually porous tubes, instead of having an amorphous core, as generally assumed. Direct observation shows thermally induced track fragmentation in fluoapatite, in clear contrast to the amorphous tracks in zircon, which gradually ''fade'' without fragmentation. Rayleigh instability and the thermal emission of vacancies control the annealing of porous fission tracks in fluorapatite.
- OSTI ID:
- 21421452
- Journal Information:
- Physical Review. B, Condensed Matter and Materials Physics, Vol. 82, Issue 14; Other Information: DOI: 10.1103/PhysRevB.82.144109; (c) 2010 The American Physical Society; ISSN 1098-0121
- Country of Publication:
- United States
- Language:
- English
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Related Subjects
75 CONDENSED MATTER PHYSICS
SUPERCONDUCTIVITY AND SUPERFLUIDITY
ANNEALING
APATITES
EMISSION
FISSION FRAGMENTS
FISSION TRACKS
FLUORESCENCE
HEATING
INSTABILITY
NUCLEAR FRAGMENTS
POROUS MATERIALS
SPONTANEOUS FISSION
TRANSMISSION ELECTRON MICROSCOPY
URANIUM 238
ZIRCON
ACTINIDE NUCLEI
ALPHA DECAY RADIOISOTOPES
DECAY
ELECTRON MICROSCOPY
EVEN-EVEN NUCLEI
FISSION
HEAT TREATMENTS
HEAVY NUCLEI
ISOTOPES
LUMINESCENCE
MATERIALS
MICROSCOPY
MINERALS
NUCLEAR DECAY
NUCLEAR REACTIONS
NUCLEI
PARTICLE TRACKS
PHOSPHATE MINERALS
PHOTON EMISSION
RADIOISOTOPES
SILICATE MINERALS
SPONTANEOUS FISSION RADIOISOTOPES
URANIUM ISOTOPES
YEARS LIVING RADIOISOTOPES