Early solar irradiation as a source of the inner solar system chromium isotopic heterogeneity
Autor: | Klaus Mezger, Y. Kadlag, Ingo Leya, Harry Becker, Jason Hirtz |
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Rok vydání: | 2021 |
Předmět: |
Solar System
Materials science 520 Astronomy Radiochemistry 500 Naturwissenschaften und Mathematik::520 Astronomie::520 Astronomie und zugeordnete Wissenschaften chemistry.chemical_element chromium isotopic heterogeneity solar irradiation 620 Engineering Chromium Geophysics chemistry Space and Planetary Science inner solar system Irradiation |
Zdroj: | Kadlag, Yogita; Hirtz, Jason; Becker, Harry; Leya, Ingo; Mezger, Klaus (2021). Early solar irradiation as a source of the inner solar system chromium isotopic heterogeneity. Meteoritics & planetary science, 56(11), pp. 2083-2102. Meteoritical Society at the University of Arkansas, Dept. of Chemistry and Biochemistry 10.1111/maps.13756 |
ISSN: | 1945-5100 1086-9379 |
DOI: | 10.1111/maps.13756 |
Popis: | Different solar system objects display variable abundances of neutron-rich isotopes such as 54Cr, 50Ti, and 48Ca, which are commonly attributed to a heterogeneous distribution of presolar grains in different domains of the solar system. Here, we show that the heterogeneity of 54Cr/52Cr and the correlation of 54Cr/52Cr with Fe/Cr in metal fractions of EH3 chondrites and in inner solar system bodies can be attributed to variable irradiation of dust grains by solar energetic particles and variable mixing of irradiated material in the different domains of the inner solar nebula. The isotope variations in inner solar system objects can be generated by ~300 y long local irradiation of mm- to cm-sized solids with average solar energetic particle fluxes of ~105 times the modern value. The relative homogeneity of 53Cr/52Cr in inner solar system objects can be a consequence of the production of 53Mn by the early irradiation of dust, evaporation, and nebula-wide homogenization of Mn due to high temperatures, followed by Mn/Cr fractionation within the first few million years of the solar system. The 54Cr/52Cr of the Earth can be produced by irradiated pebbles and |
Databáze: | OpenAIRE |
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