DIFFUSION KINETICS OF PROTON-INDUCED 21NE, 3HE, AND 4HE IN QUARTZ

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dc.contributor.author Shuster D.L.
dc.contributor.author Farley K.A.
dc.date.accessioned 2023-11-26T02:22:38Z
dc.date.available 2023-11-26T02:22:38Z
dc.date.issued 2005
dc.identifier https://www.elibrary.ru/item.asp?id=14559564
dc.identifier.citation Geochimica et Cosmochimica Acta, 2005, 69, 9, 2349-2359
dc.identifier.issn 0016-7037
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/41984
dc.description.abstract A natural quartz sample free of mineral and fluid inclusions was irradiated with a 200 MeV proton beam to produce spallogenic 21Ne, 3He and 4He. Temperature-dependent diffusivities of these three nuclides were then determined simultaneously by high precision stepped-heating and noble gas mass spectrometry. The outward mobility of proton-induced nuclides reflects diffusion through the quartz lattice. In the studied range of 70 to 400°C the helium diffusion coefficients exceed those of neon by 5 7 orders of magnitude. The implied diffusion parameters Ea = 153.7 ± 1.5 (kJ/mol) and ln(Do/a2) = 15.9 ± 0.3 (ln(s-1)) and Ea = 84.5 ± 1.2 (kJ/mol) and ln(Do/a2) = 11.1 ± 0.3 (ln(s-1)) for proton-induced 21Ne and 3He, respectively, indicate that cosmogenic neon will be quantitatively retained in inclusion-free quartz at typical Earth surface temperatures whereas cosmogenic helium will not. However, the neon diffusion parameters also indicate that diffusive loss needs to be considered for small...
dc.title DIFFUSION KINETICS OF PROTON-INDUCED 21NE, 3HE, AND 4HE IN QUARTZ
dc.type Статья
dc.identifier.doi 10.1016/j.gca.2004.11.002


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