1992
DOI: 10.1557/proc-268-343
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Amorphization of PLZT Material by 1.5 MeV Krypton Ion Irradiation with In Situ TEM Observation

Abstract: PLZT 9/65/35 single crystals were irradiated with 1.5 MeV krypton ions at 25–450°C in the HVEM-Tandem Facility at Argonne National Laboratory. In-situ TEM was performed during irradiation in order to determine the critical amorphization dose. At room temperature, the material was completely amorphized after a dose of only 1.9×1014 ions/cm2, less than one fifth of the critical amorphization dose for silicon (1×1015 ions/cm2). The critical amorphization dose for the PLZT material increased with increasing irradi… Show more

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Cited by 9 publications
(7 citation statements)
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“…A lower ratio of S N /S E , calculated for low-mass ions like He, requires a rise of the number of displacements, necessary to amorphize clinoenstatite, indicating an in-situ annealing process due to the enhanced ratio between electronic and nuclear energy deposition. This result had been previously confirmed for olivines by Wang & Ewing (1992), who could not trigger an amorphization process by 400 keV He + ions.…”
Section: Resultssupporting
confidence: 72%
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“…A lower ratio of S N /S E , calculated for low-mass ions like He, requires a rise of the number of displacements, necessary to amorphize clinoenstatite, indicating an in-situ annealing process due to the enhanced ratio between electronic and nuclear energy deposition. This result had been previously confirmed for olivines by Wang & Ewing (1992), who could not trigger an amorphization process by 400 keV He + ions.…”
Section: Resultssupporting
confidence: 72%
“…Therefore we can conclude that the discussed annealing processes are not efficient enough to trigger recrystallization but may have repercussions on processing or evaporation of ice mantles around the grains. Wang & Ewing (1992) had proven that the critical dose necessary for amorphization of olivines rapidly increases with increasing magnesium content. The critical amorphization dose for fayalite is less than 1/4 of the critical dose of (Mg 0.88 Fe 0.12 ) 2 SiO 4 for 1.5 MeV Kr + ions at room temperature.…”
Section: Conclusion Of Astrophysical Relevancementioning
confidence: 99%
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“…The materials listed in this study can most easily be amorphized at room temperature 5 -under heavy ion irradiation at a faraction of a displacement per atom (dpa) [16,[22][23][24][25][26][27] except for UOZ. In most cases, radiation-induced nanophase formation has been found to be closely related to the process of radiation-induced solid-state amorphization.…”
Section: Resultsmentioning
confidence: 99%
“…Other property changes associated with this a-decay-induced transformation have been summarized in a recent review by Ewing et al [22]. Fission track annealing studies of natural apatites [17] and ion-beam irradiation studies of natural and synthetic apatites [21,23] suggest that simultaneous thermal recovery processes will minimize or even prevent amorphization in Pucontaining apatites under deep borehole conditions (temperature > 150-200°C). The chemical durability of natural apatites is well demonstrated by the 2 billion year old, 235U-enriched Oklo apatites [17].…”
Section: Waste Forms For Piutoniummentioning
confidence: 99%