The elusive (60)Fe in the solar nebula
No (60)Ni or (61)Ni anomalies have been detected in troilite inclusions from Muonionalusta, a 4565.3 +/- 0.1 Ma old IVA iron meteorite, to the level of the analytical precision of 10 ppm. Because Muonionalusta troilite is very old, has a high Fe/Ni ratio, and is free of (61)Ni anomalies, it is the i...
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creator | Moynier, Frédéric Blichert-Toft, Janne Wang, Kun Herzog, Gregory F. Albarède, Francis |
description | No (60)Ni or (61)Ni anomalies have been detected in troilite inclusions from Muonionalusta, a 4565.3 +/- 0.1 Ma old IVA iron meteorite, to the level of the analytical precision of 10 ppm. Because Muonionalusta troilite is very old, has a high Fe/Ni ratio, and is free of (61)Ni anomalies, it is the ideal material in which to search for potential excesses of (60)Ni produced by the decay of (60)Fe (t(1/2) = 2.62 Ma). The (60)Ni/(58)Ni and Fe/Ni ratios (up to 1680) measured here imply an upper limit for the initial (60)Fe/(56)Fe for the Muonionalusta troilite of 3 x 10(-9). Assuming that (60)Fe was homogeneously distributed across the nebula, this result suggests that the solar system initial (60)Fe/(56)Fe ratio was less than 5 x 10(-9), which is lower than previously measured by at least a factor of 50 |
doi_str_mv | 10.1088/0004-637X/741/2/71 |
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Because Muonionalusta troilite is very old, has a high Fe/Ni ratio, and is free of (61)Ni anomalies, it is the ideal material in which to search for potential excesses of (60)Ni produced by the decay of (60)Fe (t(1/2) = 2.62 Ma). The (60)Ni/(58)Ni and Fe/Ni ratios (up to 1680) measured here imply an upper limit for the initial (60)Fe/(56)Fe for the Muonionalusta troilite of 3 x 10(-9). Assuming that (60)Fe was homogeneously distributed across the nebula, this result suggests that the solar system initial (60)Fe/(56)Fe ratio was less than 5 x 10(-9), which is lower than previously measured by at least a factor of 50</description><identifier>ISSN: 0004-637X</identifier><identifier>EISSN: 1538-4357</identifier><identifier>DOI: 10.1088/0004-637X/741/2/71</identifier><language>eng</language><publisher>American Astronomical Society</publisher><ispartof>The Astrophysical journal, 2011-11, Vol.741 (2)</ispartof><rights>Distributed under a Creative Commons Attribution 4.0 International License</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><orcidid>0000-0003-4321-5581 ; 0000-0003-1994-1428 ; 0000-0002-4932-4079</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>230,314,780,784,885,27924,27925</link.rule.ids><backlink>$$Uhttps://insu.hal.science/insu-00674581$$DView record in HAL$$Hfree_for_read</backlink></links><search><creatorcontrib>Moynier, Frédéric</creatorcontrib><creatorcontrib>Blichert-Toft, Janne</creatorcontrib><creatorcontrib>Wang, Kun</creatorcontrib><creatorcontrib>Herzog, Gregory F.</creatorcontrib><creatorcontrib>Albarède, Francis</creatorcontrib><title>The elusive (60)Fe in the solar nebula</title><title>The Astrophysical journal</title><description>No (60)Ni or (61)Ni anomalies have been detected in troilite inclusions from Muonionalusta, a 4565.3 +/- 0.1 Ma old IVA iron meteorite, to the level of the analytical precision of 10 ppm. Because Muonionalusta troilite is very old, has a high Fe/Ni ratio, and is free of (61)Ni anomalies, it is the ideal material in which to search for potential excesses of (60)Ni produced by the decay of (60)Fe (t(1/2) = 2.62 Ma). The (60)Ni/(58)Ni and Fe/Ni ratios (up to 1680) measured here imply an upper limit for the initial (60)Fe/(56)Fe for the Muonionalusta troilite of 3 x 10(-9). 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Because Muonionalusta troilite is very old, has a high Fe/Ni ratio, and is free of (61)Ni anomalies, it is the ideal material in which to search for potential excesses of (60)Ni produced by the decay of (60)Fe (t(1/2) = 2.62 Ma). The (60)Ni/(58)Ni and Fe/Ni ratios (up to 1680) measured here imply an upper limit for the initial (60)Fe/(56)Fe for the Muonionalusta troilite of 3 x 10(-9). Assuming that (60)Fe was homogeneously distributed across the nebula, this result suggests that the solar system initial (60)Fe/(56)Fe ratio was less than 5 x 10(-9), which is lower than previously measured by at least a factor of 50</abstract><pub>American Astronomical Society</pub><doi>10.1088/0004-637X/741/2/71</doi><orcidid>https://orcid.org/0000-0003-4321-5581</orcidid><orcidid>https://orcid.org/0000-0003-1994-1428</orcidid><orcidid>https://orcid.org/0000-0002-4932-4079</orcidid></addata></record> |
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title | The elusive (60)Fe in the solar nebula |
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