Accretion rate of extraterrestrial 41Ca in Antarctic snow samples

Interplanetary Dust Particles (IDPs) are small grains, generally less than a few hundred micrometers in size. Their main source is the Asteroid Belt, located at 3 AU from the Sun, between Mars and Jupiter. During their flight from the Asteroid Belt to the Earth they are irradiated by galactic and so...

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Published in:Nuclear Instruments and Methods in Physics Research Section B: Beam Interactions with Materials and Atoms
Main Authors: Gómez Guzmán, J. M., Bishop, S., Faestermann, T., Famulok, N., Fimiani, Leticia, Hain, K., Jahn, S., Korschinek, G., Ludwig, P., Rodrigues Ferreira Maltez, Dario Pablo
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier Science
Subjects:
AMS
Online Access:http://hdl.handle.net/11336/98530
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spelling ftconicet:oai:ri.conicet.gov.ar:11336/98530 2023-10-09T21:47:14+02:00 Accretion rate of extraterrestrial 41Ca in Antarctic snow samples Gómez Guzmán, J. M. Bishop, S. Faestermann, T. Famulok, N. Fimiani, Leticia Hain, K. Jahn, S. Korschinek, G. Ludwig, P. Rodrigues Ferreira Maltez, Dario Pablo application/pdf http://hdl.handle.net/11336/98530 eng eng Elsevier Science info:eu-repo/semantics/altIdentifier/doi/10.1016/j.nimb.2015.05.016 info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S0168583X15004875 http://hdl.handle.net/11336/98530 Gómez Guzmán, J. M.; Bishop, S.; Faestermann, T.; Famulok, N.; Fimiani, Leticia; et al.; Accretion rate of extraterrestrial 41Ca in Antarctic snow samples; Elsevier Science; Beam Interactions with Materials and Atoms; 361; 10-2015; 620-626 0168-583X CONICET Digital CONICET info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ 41CA AMS INTERPLANETARY DUST https://purl.org/becyt/ford/1.3 https://purl.org/becyt/ford/1 info:eu-repo/semantics/article info:ar-repo/semantics/artículo info:eu-repo/semantics/publishedVersion ftconicet https://doi.org/10.1016/j.nimb.2015.05.016 2023-09-24T19:16:50Z Interplanetary Dust Particles (IDPs) are small grains, generally less than a few hundred micrometers in size. Their main source is the Asteroid Belt, located at 3 AU from the Sun, between Mars and Jupiter. During their flight from the Asteroid Belt to the Earth they are irradiated by galactic and solar cosmic rays (GCR and SCR), thus radionuclides are formed, like 41Ca and 53Mn. Therefore, 41Ca (T1/2 = 1.03 × 105 yr) can be used as a key tracer to determine the accretion rate of IDPs onto the Earth because there are no significant terrestrial sources for this radionuclide. The first step of this study consisted to calculate the production rate of 41Ca in IDPs accreted by the Earth during their travel from the Asteroid Belt. This production rate, used in accordance with the 41Ca/40Ca ratios that will be measured in snow samples from the Antarctica will be used to calculate the amount of extraterrestrial material accreted by the Earth per year. There challenges for this project are, at first, the much longer time for the flight needed by the IDPs to travel from the Asteroid Belt to the Earth in comparison with the 41Ca half-life yields an early saturation for the 41Ca/40Ca ratio, and second, the importance of selecting the correct sampling site to avoid a high influx of natural 40Ca, preventing dilution of the 41Ca/40Ca ratio, the quantity measured by AMS. Fil: Gómez Guzmán, J. M. Technische Universitat München; Alemania Fil: Bishop, S. Technische Universitat München; Alemania Fil: Faestermann, T. Technische Universitat München; Alemania Fil: Famulok, N. Technische Universitat München; Alemania Fil: Fimiani, Leticia. Technische Universitat München; Alemania Fil: Hain, K. Technische Universitat München; Alemania Fil: Jahn, S. Technische Universitat München; Alemania Fil: Korschinek, G. Technische Universitat München; Alemania Fil: Ludwig, P. Technische Universitat München; Alemania Fil: Rodrigues Ferreira Maltez, Dario Pablo. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. ... Article in Journal/Newspaper Antarc* Antarctic Antarctica CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) Antarctic Argentina Pablo ENVELOPE(-63.717,-63.717,-64.283,-64.283) Jupiter ENVELOPE(101.133,101.133,-66.117,-66.117) Ferreira ENVELOPE(-62.050,-62.050,-64.600,-64.600) Guzmán ENVELOPE(-62.850,-62.850,-64.817,-64.817) Nuclear Instruments and Methods in Physics Research Section B: Beam Interactions with Materials and Atoms 361 620 626
institution Open Polar
collection CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas)
op_collection_id ftconicet
language English
topic 41CA
AMS
INTERPLANETARY DUST
https://purl.org/becyt/ford/1.3
https://purl.org/becyt/ford/1
spellingShingle 41CA
AMS
INTERPLANETARY DUST
https://purl.org/becyt/ford/1.3
https://purl.org/becyt/ford/1
Gómez Guzmán, J. M.
Bishop, S.
Faestermann, T.
Famulok, N.
Fimiani, Leticia
Hain, K.
Jahn, S.
Korschinek, G.
Ludwig, P.
Rodrigues Ferreira Maltez, Dario Pablo
Accretion rate of extraterrestrial 41Ca in Antarctic snow samples
topic_facet 41CA
AMS
INTERPLANETARY DUST
https://purl.org/becyt/ford/1.3
https://purl.org/becyt/ford/1
description Interplanetary Dust Particles (IDPs) are small grains, generally less than a few hundred micrometers in size. Their main source is the Asteroid Belt, located at 3 AU from the Sun, between Mars and Jupiter. During their flight from the Asteroid Belt to the Earth they are irradiated by galactic and solar cosmic rays (GCR and SCR), thus radionuclides are formed, like 41Ca and 53Mn. Therefore, 41Ca (T1/2 = 1.03 × 105 yr) can be used as a key tracer to determine the accretion rate of IDPs onto the Earth because there are no significant terrestrial sources for this radionuclide. The first step of this study consisted to calculate the production rate of 41Ca in IDPs accreted by the Earth during their travel from the Asteroid Belt. This production rate, used in accordance with the 41Ca/40Ca ratios that will be measured in snow samples from the Antarctica will be used to calculate the amount of extraterrestrial material accreted by the Earth per year. There challenges for this project are, at first, the much longer time for the flight needed by the IDPs to travel from the Asteroid Belt to the Earth in comparison with the 41Ca half-life yields an early saturation for the 41Ca/40Ca ratio, and second, the importance of selecting the correct sampling site to avoid a high influx of natural 40Ca, preventing dilution of the 41Ca/40Ca ratio, the quantity measured by AMS. Fil: Gómez Guzmán, J. M. Technische Universitat München; Alemania Fil: Bishop, S. Technische Universitat München; Alemania Fil: Faestermann, T. Technische Universitat München; Alemania Fil: Famulok, N. Technische Universitat München; Alemania Fil: Fimiani, Leticia. Technische Universitat München; Alemania Fil: Hain, K. Technische Universitat München; Alemania Fil: Jahn, S. Technische Universitat München; Alemania Fil: Korschinek, G. Technische Universitat München; Alemania Fil: Ludwig, P. Technische Universitat München; Alemania Fil: Rodrigues Ferreira Maltez, Dario Pablo. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. ...
format Article in Journal/Newspaper
author Gómez Guzmán, J. M.
Bishop, S.
Faestermann, T.
Famulok, N.
Fimiani, Leticia
Hain, K.
Jahn, S.
Korschinek, G.
Ludwig, P.
Rodrigues Ferreira Maltez, Dario Pablo
author_facet Gómez Guzmán, J. M.
Bishop, S.
Faestermann, T.
Famulok, N.
Fimiani, Leticia
Hain, K.
Jahn, S.
Korschinek, G.
Ludwig, P.
Rodrigues Ferreira Maltez, Dario Pablo
author_sort Gómez Guzmán, J. M.
title Accretion rate of extraterrestrial 41Ca in Antarctic snow samples
title_short Accretion rate of extraterrestrial 41Ca in Antarctic snow samples
title_full Accretion rate of extraterrestrial 41Ca in Antarctic snow samples
title_fullStr Accretion rate of extraterrestrial 41Ca in Antarctic snow samples
title_full_unstemmed Accretion rate of extraterrestrial 41Ca in Antarctic snow samples
title_sort accretion rate of extraterrestrial 41ca in antarctic snow samples
publisher Elsevier Science
url http://hdl.handle.net/11336/98530
long_lat ENVELOPE(-63.717,-63.717,-64.283,-64.283)
ENVELOPE(101.133,101.133,-66.117,-66.117)
ENVELOPE(-62.050,-62.050,-64.600,-64.600)
ENVELOPE(-62.850,-62.850,-64.817,-64.817)
geographic Antarctic
Argentina
Pablo
Jupiter
Ferreira
Guzmán
geographic_facet Antarctic
Argentina
Pablo
Jupiter
Ferreira
Guzmán
genre Antarc*
Antarctic
Antarctica
genre_facet Antarc*
Antarctic
Antarctica
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1016/j.nimb.2015.05.016
info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S0168583X15004875
http://hdl.handle.net/11336/98530
Gómez Guzmán, J. M.; Bishop, S.; Faestermann, T.; Famulok, N.; Fimiani, Leticia; et al.; Accretion rate of extraterrestrial 41Ca in Antarctic snow samples; Elsevier Science; Beam Interactions with Materials and Atoms; 361; 10-2015; 620-626
0168-583X
CONICET Digital
CONICET
op_rights info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
op_doi https://doi.org/10.1016/j.nimb.2015.05.016
container_title Nuclear Instruments and Methods in Physics Research Section B: Beam Interactions with Materials and Atoms
container_volume 361
container_start_page 620
op_container_end_page 626
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