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Titolo:
The degree and nature of radiation damage in zircon observed by Si-29 nuclear magnetic resonance
Autore:
Farnan, I; Salje, EKH;
Indirizzi:
Univ Cambridge, Dept Earth Sci, Cambridge CB2 3EQ, England Univ CambridgeCambridge England CB2 3EQ Sci, Cambridge CB2 3EQ, England
Titolo Testata:
JOURNAL OF APPLIED PHYSICS
fascicolo: 4, volume: 89, anno: 2001,
pagine: 2084 - 2090
SICI:
0021-8979(20010215)89:4<2084:TDANOR>2.0.ZU;2-7
Fonte:
ISI
Lingua:
ENG
Soggetto:
DISPLACEMENT CASCADES; AMORPHIZATION; TRANSITION; DYNAMICS; THORITE; METALS; STATE; PHASE; NMR;
Tipo documento:
Article
Natura:
Periodico
Settore Disciplinare:
Physical, Chemical & Earth Sciences
--discip_EC--
Citazioni:
26
Recensione:
Indirizzi per estratti:
Indirizzo: Farnan, I Univ Cambridge, Dept Earth Sci, Downing St, Cambridge CB2 3EQ, England Univ Cambridge Downing St Cambridge England CB2 3EQ EQ, England
Citazione:
I. Farnan e E.K.H. Salje, "The degree and nature of radiation damage in zircon observed by Si-29 nuclear magnetic resonance", J APPL PHYS, 89(4), 2001, pp. 2084-2090

Abstract

A quantitative analysis of Si-29 nuclear magnetic resonance spectra of radiation damaged, natural zircons showed that the local structure in crystalline and amorphous regions depend explicitly on radiation dose. Nonpercolating amorphous islands of high density "glass" within the crystalline matrix show a low interconnectivity of SiO4 tetrahedra. This structural state is quite different from that of the high dose, percolating regions of low density glass with more polymerised tetrahedra. A continuous nonlinear dose dependence between the high and low density glass states is reported. A continuous evolution of the local structure of the crystalline phase up to the percolation point is also reported. No phase separation into binary oxides wasobserved. The total number of permanently displaced atoms per alpha -recoil event is similar to 3800 atoms for low radiation doses and decreases to similar to 2000 atoms for 10 x 10(18) alpha events/g. No indication of partitioning of paramagnetic impurities between crystalline and amorphous regions was found for these natural zircons. The amorphous fractions of the metamict zircons were determined as a function of their accumulated radiation dose. These values coincide closely with those recently determined by x-ray diffraction studies. They are much greater than previously assumed based on density measurements. The dose dependence is consistent with the concept ofdirect impact amorphization in the atomic cascade following an alpha -recoil event. (C) 2001 American Institute of Physics.

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Documento generato il 04/04/20 alle ore 10:51:28