Obtaining a History of the Flux of Cosmic Rays using In Situ Cosmogenic $^{14}$C Trapped in Polar Ice

Carbon-14 ($^{14}$C) is produced in the atmosphere when neutrons from cosmic-ray air showers are captured by $^{14}$N nuclei. Atmospheric $^{14}$C becomes trapped in air bubbles in polar ice as compacted snow (firn) transforms into ice. $^{14}$C is also produced in situ in ice grains by penetrating...

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Main Authors: BenZvi, Segev, Petrenko, Vasilii V., Hmiel, Benjamin, Dyonisius, Michael, Smith, Andrew M., Yang, Bin, Hua, Quan
Format: Article in Journal/Newspaper
Language:unknown
Published: arXiv 2019
Subjects:
Online Access:https://dx.doi.org/10.48550/arxiv.1909.07994
https://arxiv.org/abs/1909.07994
id ftdatacite:10.48550/arxiv.1909.07994
record_format openpolar
spelling ftdatacite:10.48550/arxiv.1909.07994 2023-05-15T16:39:13+02:00 Obtaining a History of the Flux of Cosmic Rays using In Situ Cosmogenic $^{14}$C Trapped in Polar Ice BenZvi, Segev Petrenko, Vasilii V. Hmiel, Benjamin Dyonisius, Michael Smith, Andrew M. Yang, Bin Hua, Quan 2019 https://dx.doi.org/10.48550/arxiv.1909.07994 https://arxiv.org/abs/1909.07994 unknown arXiv arXiv.org perpetual, non-exclusive license http://arxiv.org/licenses/nonexclusive-distrib/1.0/ High Energy Astrophysical Phenomena astro-ph.HE Instrumentation and Methods for Astrophysics astro-ph.IM FOS Physical sciences Article CreativeWork article Preprint 2019 ftdatacite https://doi.org/10.48550/arxiv.1909.07994 2022-03-10T16:32:56Z Carbon-14 ($^{14}$C) is produced in the atmosphere when neutrons from cosmic-ray air showers are captured by $^{14}$N nuclei. Atmospheric $^{14}$C becomes trapped in air bubbles in polar ice as compacted snow (firn) transforms into ice. $^{14}$C is also produced in situ in ice grains by penetrating cosmic-ray neutrons and muons. Recent ice core measurements indicate that in the $^{14}$CO phase, the $^{14}$C is dominated by the in situ cosmogenic component at most ice coring sites. Thus, it should be possible to use ice-bound $^{14}$CO to reconstruct the historical flux of cosmic rays at Earth, without the transport and deposition uncertainties associated with $^{10}$Be or the carbon cycle uncertainties affecting atmospheric $^{14}$CO$_2$. The measurements will be sensitive to the cosmic-ray flux above the energy range most affected by solar modulation. We present estimates of the expected sensitivity of $^{14}$CO in ice cores to the historical flux of Galactic cosmic rays, based on recent studies of $^{14}$CO in polar ice. : Presented at the International Cosmic Ray Conference (ICRC2019) in Madison, WI, USA, July 2019. 8 pages, 2 figures Article in Journal/Newspaper ice core DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
topic High Energy Astrophysical Phenomena astro-ph.HE
Instrumentation and Methods for Astrophysics astro-ph.IM
FOS Physical sciences
spellingShingle High Energy Astrophysical Phenomena astro-ph.HE
Instrumentation and Methods for Astrophysics astro-ph.IM
FOS Physical sciences
BenZvi, Segev
Petrenko, Vasilii V.
Hmiel, Benjamin
Dyonisius, Michael
Smith, Andrew M.
Yang, Bin
Hua, Quan
Obtaining a History of the Flux of Cosmic Rays using In Situ Cosmogenic $^{14}$C Trapped in Polar Ice
topic_facet High Energy Astrophysical Phenomena astro-ph.HE
Instrumentation and Methods for Astrophysics astro-ph.IM
FOS Physical sciences
description Carbon-14 ($^{14}$C) is produced in the atmosphere when neutrons from cosmic-ray air showers are captured by $^{14}$N nuclei. Atmospheric $^{14}$C becomes trapped in air bubbles in polar ice as compacted snow (firn) transforms into ice. $^{14}$C is also produced in situ in ice grains by penetrating cosmic-ray neutrons and muons. Recent ice core measurements indicate that in the $^{14}$CO phase, the $^{14}$C is dominated by the in situ cosmogenic component at most ice coring sites. Thus, it should be possible to use ice-bound $^{14}$CO to reconstruct the historical flux of cosmic rays at Earth, without the transport and deposition uncertainties associated with $^{10}$Be or the carbon cycle uncertainties affecting atmospheric $^{14}$CO$_2$. The measurements will be sensitive to the cosmic-ray flux above the energy range most affected by solar modulation. We present estimates of the expected sensitivity of $^{14}$CO in ice cores to the historical flux of Galactic cosmic rays, based on recent studies of $^{14}$CO in polar ice. : Presented at the International Cosmic Ray Conference (ICRC2019) in Madison, WI, USA, July 2019. 8 pages, 2 figures
format Article in Journal/Newspaper
author BenZvi, Segev
Petrenko, Vasilii V.
Hmiel, Benjamin
Dyonisius, Michael
Smith, Andrew M.
Yang, Bin
Hua, Quan
author_facet BenZvi, Segev
Petrenko, Vasilii V.
Hmiel, Benjamin
Dyonisius, Michael
Smith, Andrew M.
Yang, Bin
Hua, Quan
author_sort BenZvi, Segev
title Obtaining a History of the Flux of Cosmic Rays using In Situ Cosmogenic $^{14}$C Trapped in Polar Ice
title_short Obtaining a History of the Flux of Cosmic Rays using In Situ Cosmogenic $^{14}$C Trapped in Polar Ice
title_full Obtaining a History of the Flux of Cosmic Rays using In Situ Cosmogenic $^{14}$C Trapped in Polar Ice
title_fullStr Obtaining a History of the Flux of Cosmic Rays using In Situ Cosmogenic $^{14}$C Trapped in Polar Ice
title_full_unstemmed Obtaining a History of the Flux of Cosmic Rays using In Situ Cosmogenic $^{14}$C Trapped in Polar Ice
title_sort obtaining a history of the flux of cosmic rays using in situ cosmogenic $^{14}$c trapped in polar ice
publisher arXiv
publishDate 2019
url https://dx.doi.org/10.48550/arxiv.1909.07994
https://arxiv.org/abs/1909.07994
genre ice core
genre_facet ice core
op_rights arXiv.org perpetual, non-exclusive license
http://arxiv.org/licenses/nonexclusive-distrib/1.0/
op_doi https://doi.org/10.48550/arxiv.1909.07994
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