Galactic cosmic ray effects on iron and nickel isotopes in iron meteorites

We present model calculations for cosmogenic production rates in order to quantify the potential effects of spallation and neutron capture reactions on Fe and Ni isotopes in iron meteorites. We aim to determine whether the magnitude of any cosmogenic effects on the isotopic ratios of Fe and/or Ni ma...

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Main Authors: Cook, David L., Leya, Ingo, Schonbachler, Maria
Other Authors: Earth Observatory of Singapore
Format: Article
Language:English
Published: 2021
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Online Access:https://hdl.handle.net/10356/146394
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spelling sg-ntu-dr.10356-1463942021-02-20T20:10:58Z Galactic cosmic ray effects on iron and nickel isotopes in iron meteorites Cook, David L. Leya, Ingo Schonbachler, Maria Earth Observatory of Singapore Science::Astronomy Chondrule Meteoroids We present model calculations for cosmogenic production rates in order to quantify the potential effects of spallation and neutron capture reactions on Fe and Ni isotopes in iron meteorites. We aim to determine whether the magnitude of any cosmogenic effects on the isotopic ratios of Fe and/or Ni may hinder the search for nucleosynthetic variations in these elements or in the application of the 60Fe‐60Ni chronometer. The model shows that neutron capture reactions are the dominant source of shifts in Fe and Ni isotopic ratios and that spallation reactions are mostly negligible. The effects on 60Ni are sensitive to the Co/Ni ratio in the metal. The total galactic cosmic ray (GCR) effects on 60Ni and 64Ni can be minimized through the choice of normalizing isotopes (61Ni/58Ni versus 62Ni/58Ni). In nearly all cases, the GCR effects (neutron capture and/or spallation) on Fe and Ni isotopic ratios are smaller than the current analytical resolution of the isotopic measurements. The model predictions are compared to the Fe and Ni isotopic compositions measured in a suite of six group IAB irons with a range of cosmic ray exposure histories. The experimental data are in good agreement with the model results. The minimal effects of GCRs on Fe and Ni isotopes should not hamper the search for nucleosynthetic variations in these two elements or the application of the 60Fe‐60Ni chronometer in iron meteorites or chondrites. Published version 2021-02-16T01:44:56Z 2021-02-16T01:44:56Z 2020 Journal Article Cook, D. L., Leya, I., & Schonbachler, M. (2020). Galactic cosmic ray effects on iron and nickel isotopes in iron meteorites. Meteoritics & Planetary Science, 55(12), 2758-2771. doi:10.1111/maps.13446 1945-5100 https://hdl.handle.net/10356/146394 10.1111/maps.13446 12 55 2758 2771 en Meteoritics & Planetary Science © 2020 The Authors. Meteoritics & Planetary Science published by Wiley Periodicals, Inc. on behalf of The Meteoritical Society (MET).This is an open access article under the terms of the Creative Commons Attribution License, which permits use,distribution and reproduction in any medium, provided the original work is properly cited. application/pdf
institution Nanyang Technological University
building NTU Library
continent Asia
country Singapore
Singapore
content_provider NTU Library
collection DR-NTU
language English
topic Science::Astronomy
Chondrule
Meteoroids
spellingShingle Science::Astronomy
Chondrule
Meteoroids
Cook, David L.
Leya, Ingo
Schonbachler, Maria
Galactic cosmic ray effects on iron and nickel isotopes in iron meteorites
description We present model calculations for cosmogenic production rates in order to quantify the potential effects of spallation and neutron capture reactions on Fe and Ni isotopes in iron meteorites. We aim to determine whether the magnitude of any cosmogenic effects on the isotopic ratios of Fe and/or Ni may hinder the search for nucleosynthetic variations in these elements or in the application of the 60Fe‐60Ni chronometer. The model shows that neutron capture reactions are the dominant source of shifts in Fe and Ni isotopic ratios and that spallation reactions are mostly negligible. The effects on 60Ni are sensitive to the Co/Ni ratio in the metal. The total galactic cosmic ray (GCR) effects on 60Ni and 64Ni can be minimized through the choice of normalizing isotopes (61Ni/58Ni versus 62Ni/58Ni). In nearly all cases, the GCR effects (neutron capture and/or spallation) on Fe and Ni isotopic ratios are smaller than the current analytical resolution of the isotopic measurements. The model predictions are compared to the Fe and Ni isotopic compositions measured in a suite of six group IAB irons with a range of cosmic ray exposure histories. The experimental data are in good agreement with the model results. The minimal effects of GCRs on Fe and Ni isotopes should not hamper the search for nucleosynthetic variations in these two elements or the application of the 60Fe‐60Ni chronometer in iron meteorites or chondrites.
author2 Earth Observatory of Singapore
author_facet Earth Observatory of Singapore
Cook, David L.
Leya, Ingo
Schonbachler, Maria
format Article
author Cook, David L.
Leya, Ingo
Schonbachler, Maria
author_sort Cook, David L.
title Galactic cosmic ray effects on iron and nickel isotopes in iron meteorites
title_short Galactic cosmic ray effects on iron and nickel isotopes in iron meteorites
title_full Galactic cosmic ray effects on iron and nickel isotopes in iron meteorites
title_fullStr Galactic cosmic ray effects on iron and nickel isotopes in iron meteorites
title_full_unstemmed Galactic cosmic ray effects on iron and nickel isotopes in iron meteorites
title_sort galactic cosmic ray effects on iron and nickel isotopes in iron meteorites
publishDate 2021
url https://hdl.handle.net/10356/146394
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