Exploring ice core drilling chips from a cold Alpine glacier for cosmogenic radionuclide (Be-10) analysis

Ice cores offer unique multi-proxy paleoclimate records, but provide only very limited sample material, which has to be carefully distributed for various proxy analyses. Beryllium-10, for example, is analysed in polar ice cores to investigate past changes of the geomagnetic field, solar activity, an...

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Published in:Results in Physics
Main Authors: Zipf L, Merchel S, Bohleber P, Rugel G, Scharf A
Other Authors: Zipf, L, Merchel, S, Bohleber, P, Rugel, G, Scharf, A
Format: Article in Journal/Newspaper
Language:unknown
Published: 2016
Subjects:
Online Access:https://hdl.handle.net/10278/5014732
https://doi.org/10.1016/j.rinp.2016.01.002
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spelling ftuniveneziairis:oai:iris.unive.it:10278/5014732 2024-04-21T08:04:43+00:00 Exploring ice core drilling chips from a cold Alpine glacier for cosmogenic radionuclide (Be-10) analysis Zipf L Merchel S Bohleber P Rugel G Scharf A Zipf, L Merchel, S Bohleber, P Rugel, G Scharf, A 2016 https://hdl.handle.net/10278/5014732 https://doi.org/10.1016/j.rinp.2016.01.002 unknown info:eu-repo/semantics/altIdentifier/wos/WOS:000389770300023 volume:6 firstpage:78 lastpage:79 numberofpages:2 journal:RESULTS IN PHYSICS https://hdl.handle.net/10278/5014732 doi:10.1016/j.rinp.2016.01.002 info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-84960877132 Settore GEO/08 - Geochimica e Vulcanologia Settore GEO/10 - Geofisica della Terra Solida info:eu-repo/semantics/article 2016 ftuniveneziairis https://doi.org/10.1016/j.rinp.2016.01.002 2024-03-28T01:22:06Z Ice cores offer unique multi-proxy paleoclimate records, but provide only very limited sample material, which has to be carefully distributed for various proxy analyses. Beryllium-10, for example, is analysed in polar ice cores to investigate past changes of the geomagnetic field, solar activity, and the aerosol cycle, as well as to more accurately date the material. This paper explores the suitability of a drilling by-product, the so-called drilling chips, for 10Be-analysis. An ice core recently drilled at a cold Alpine glacier is used to directly compare 10Be-data from ice core samples with corresponding drilling chips. Both sample types have been spiked with 9Be-carrier and identically treated to chemically isolate beryllium. The resulting BeO has been investigated by accelerator mass spectrometry (AMS) for 10Be/9Be-ratios to calculate 10Be-concentrations in the ice. As a promising first result, four out of five sample-combinations (ice core and drilling chips) agree within 2-sigma uncertainty range. However, further studies are needed in order to fully demonstrate the potential of drilling chips for 10Be-analysis in alpine and shallow polar ice cores. Article in Journal/Newspaper ice core Università Ca’ Foscari Venezia: ARCA (Archivio Istituzionale della Ricerca) Results in Physics 6 78 79
institution Open Polar
collection Università Ca’ Foscari Venezia: ARCA (Archivio Istituzionale della Ricerca)
op_collection_id ftuniveneziairis
language unknown
topic Settore GEO/08 - Geochimica e Vulcanologia
Settore GEO/10 - Geofisica della Terra Solida
spellingShingle Settore GEO/08 - Geochimica e Vulcanologia
Settore GEO/10 - Geofisica della Terra Solida
Zipf L
Merchel S
Bohleber P
Rugel G
Scharf A
Exploring ice core drilling chips from a cold Alpine glacier for cosmogenic radionuclide (Be-10) analysis
topic_facet Settore GEO/08 - Geochimica e Vulcanologia
Settore GEO/10 - Geofisica della Terra Solida
description Ice cores offer unique multi-proxy paleoclimate records, but provide only very limited sample material, which has to be carefully distributed for various proxy analyses. Beryllium-10, for example, is analysed in polar ice cores to investigate past changes of the geomagnetic field, solar activity, and the aerosol cycle, as well as to more accurately date the material. This paper explores the suitability of a drilling by-product, the so-called drilling chips, for 10Be-analysis. An ice core recently drilled at a cold Alpine glacier is used to directly compare 10Be-data from ice core samples with corresponding drilling chips. Both sample types have been spiked with 9Be-carrier and identically treated to chemically isolate beryllium. The resulting BeO has been investigated by accelerator mass spectrometry (AMS) for 10Be/9Be-ratios to calculate 10Be-concentrations in the ice. As a promising first result, four out of five sample-combinations (ice core and drilling chips) agree within 2-sigma uncertainty range. However, further studies are needed in order to fully demonstrate the potential of drilling chips for 10Be-analysis in alpine and shallow polar ice cores.
author2 Zipf, L
Merchel, S
Bohleber, P
Rugel, G
Scharf, A
format Article in Journal/Newspaper
author Zipf L
Merchel S
Bohleber P
Rugel G
Scharf A
author_facet Zipf L
Merchel S
Bohleber P
Rugel G
Scharf A
author_sort Zipf L
title Exploring ice core drilling chips from a cold Alpine glacier for cosmogenic radionuclide (Be-10) analysis
title_short Exploring ice core drilling chips from a cold Alpine glacier for cosmogenic radionuclide (Be-10) analysis
title_full Exploring ice core drilling chips from a cold Alpine glacier for cosmogenic radionuclide (Be-10) analysis
title_fullStr Exploring ice core drilling chips from a cold Alpine glacier for cosmogenic radionuclide (Be-10) analysis
title_full_unstemmed Exploring ice core drilling chips from a cold Alpine glacier for cosmogenic radionuclide (Be-10) analysis
title_sort exploring ice core drilling chips from a cold alpine glacier for cosmogenic radionuclide (be-10) analysis
publishDate 2016
url https://hdl.handle.net/10278/5014732
https://doi.org/10.1016/j.rinp.2016.01.002
genre ice core
genre_facet ice core
op_relation info:eu-repo/semantics/altIdentifier/wos/WOS:000389770300023
volume:6
firstpage:78
lastpage:79
numberofpages:2
journal:RESULTS IN PHYSICS
https://hdl.handle.net/10278/5014732
doi:10.1016/j.rinp.2016.01.002
info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-84960877132
op_doi https://doi.org/10.1016/j.rinp.2016.01.002
container_title Results in Physics
container_volume 6
container_start_page 78
op_container_end_page 79
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