IDENTIFICATION OF ANNUAL LAYERS BY CHEMICAL ANALYSES WITH A 10M DC CORE

P(論文) For dating an ice core, identification of annual layers is of great importance. Dating is usually examined by detecting seasonal cycles of concentration of chemical components along the core. Chemical analyses have been carried out with a 10m-long shallow core of Dome Camp (77.0°S, 35.0°E) sam...

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Main Authors: ナカムラ, カズキ, アゲタ, ユタカ, ナカワ, マサヨシ, アズマ, クミコ, NAKAMURA, Kazuki, AGETA, Yutaka, NAKAWO, Masayoshi, AZUMA, Kumiko
Language:English
Published: National Institute of Polar Research 1994
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/record/3860/files/KJ00000767968.pdf
https://doi.org/10.15094/00003860
https://nipr.repo.nii.ac.jp/records/3860
_version_ 1829306229160148992
author ナカムラ, カズキ
アゲタ, ユタカ
ナカワ, マサヨシ
アズマ, クミコ
NAKAMURA, Kazuki
AGETA, Yutaka
NAKAWO, Masayoshi
AZUMA, Kumiko
author_facet ナカムラ, カズキ
アゲタ, ユタカ
ナカワ, マサヨシ
アズマ, クミコ
NAKAMURA, Kazuki
AGETA, Yutaka
NAKAWO, Masayoshi
AZUMA, Kumiko
author_sort ナカムラ, カズキ
collection National Institute of Polar Research Repository, Japan
description P(論文) For dating an ice core, identification of annual layers is of great importance. Dating is usually examined by detecting seasonal cycles of concentration of chemical components along the core. Chemical analyses have been carried out with a 10m-long shallow core of Dome Camp (77.0°S, 35.0°E) sampled by JARE-26 in December 1985,to see the potential use of this method for a deep ice core to be retrieved in the near future near the camp, East Antarctica. We have analyzed, with an ion chromatograph, Cl^-, NO_3^- and SO_4^<2-> concentrations for small "disk" samples cut horizontally at every 1cm interval in depth so that 8 or 9 successive samples will cover an annual layer, because the accumulation rate has been estimated to be 9.2cm/year (snow) as an average for the last few decades at Dome Camp. Periodic variations were found in the concentration profiles of both Cl^- and SO_4^<2->. The period of the latter was found to be close to 9cm. Hence SO_4^<2-> could be a good indicator of annual layers for core samples near the dome, although care has to be taken for volcanic events which would have an enormous effect on SO_4^<2-> concentration. The period of the variation of Cl^- concentration, however, was much longer than the thickness of an annual layer. The concentration of NO_3^- was found to have decreased rapidly with depth, which seems to indicate a discernible loss of NO_3^- during the growth of snow crystals in the surface layer at shallow depths. departmental bulletin paper
genre Antarc*
Antarctica
East Antarctica
ice core
Polar meteorology and glaciology
Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology
genre_facet Antarc*
Antarctica
East Antarctica
ice core
Polar meteorology and glaciology
Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology
geographic East Antarctica
geographic_facet East Antarctica
id ftnipr:oai:nipr.repo.nii.ac.jp:00003860
institution Open Polar
language English
op_collection_id ftnipr
op_doi https://doi.org/10.15094/00003860
op_relation Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology
8
203
AA10756213
https://nipr.repo.nii.ac.jp/record/3860/files/KJ00000767968.pdf
https://doi.org/10.15094/00003860
https://nipr.repo.nii.ac.jp/records/3860
publishDate 1994
publisher National Institute of Polar Research
record_format openpolar
spelling ftnipr:oai:nipr.repo.nii.ac.jp:00003860 2025-04-13T14:07:19+00:00 IDENTIFICATION OF ANNUAL LAYERS BY CHEMICAL ANALYSES WITH A 10M DC CORE ナカムラ, カズキ アゲタ, ユタカ ナカワ, マサヨシ アズマ, クミコ NAKAMURA, Kazuki AGETA, Yutaka NAKAWO, Masayoshi AZUMA, Kumiko 1994-11 application/pdf https://nipr.repo.nii.ac.jp/record/3860/files/KJ00000767968.pdf https://doi.org/10.15094/00003860 https://nipr.repo.nii.ac.jp/records/3860 eng eng National Institute of Polar Research Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology 8 203 AA10756213 https://nipr.repo.nii.ac.jp/record/3860/files/KJ00000767968.pdf https://doi.org/10.15094/00003860 https://nipr.repo.nii.ac.jp/records/3860 1994 ftnipr https://doi.org/10.15094/00003860 2025-03-19T10:19:57Z P(論文) For dating an ice core, identification of annual layers is of great importance. Dating is usually examined by detecting seasonal cycles of concentration of chemical components along the core. Chemical analyses have been carried out with a 10m-long shallow core of Dome Camp (77.0°S, 35.0°E) sampled by JARE-26 in December 1985,to see the potential use of this method for a deep ice core to be retrieved in the near future near the camp, East Antarctica. We have analyzed, with an ion chromatograph, Cl^-, NO_3^- and SO_4^<2-> concentrations for small "disk" samples cut horizontally at every 1cm interval in depth so that 8 or 9 successive samples will cover an annual layer, because the accumulation rate has been estimated to be 9.2cm/year (snow) as an average for the last few decades at Dome Camp. Periodic variations were found in the concentration profiles of both Cl^- and SO_4^<2->. The period of the latter was found to be close to 9cm. Hence SO_4^<2-> could be a good indicator of annual layers for core samples near the dome, although care has to be taken for volcanic events which would have an enormous effect on SO_4^<2-> concentration. The period of the variation of Cl^- concentration, however, was much longer than the thickness of an annual layer. The concentration of NO_3^- was found to have decreased rapidly with depth, which seems to indicate a discernible loss of NO_3^- during the growth of snow crystals in the surface layer at shallow depths. departmental bulletin paper Other/Unknown Material Antarc* Antarctica East Antarctica ice core Polar meteorology and glaciology Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology National Institute of Polar Research Repository, Japan East Antarctica
spellingShingle ナカムラ, カズキ
アゲタ, ユタカ
ナカワ, マサヨシ
アズマ, クミコ
NAKAMURA, Kazuki
AGETA, Yutaka
NAKAWO, Masayoshi
AZUMA, Kumiko
IDENTIFICATION OF ANNUAL LAYERS BY CHEMICAL ANALYSES WITH A 10M DC CORE
title IDENTIFICATION OF ANNUAL LAYERS BY CHEMICAL ANALYSES WITH A 10M DC CORE
title_full IDENTIFICATION OF ANNUAL LAYERS BY CHEMICAL ANALYSES WITH A 10M DC CORE
title_fullStr IDENTIFICATION OF ANNUAL LAYERS BY CHEMICAL ANALYSES WITH A 10M DC CORE
title_full_unstemmed IDENTIFICATION OF ANNUAL LAYERS BY CHEMICAL ANALYSES WITH A 10M DC CORE
title_short IDENTIFICATION OF ANNUAL LAYERS BY CHEMICAL ANALYSES WITH A 10M DC CORE
title_sort identification of annual layers by chemical analyses with a 10m dc core
url https://nipr.repo.nii.ac.jp/record/3860/files/KJ00000767968.pdf
https://doi.org/10.15094/00003860
https://nipr.repo.nii.ac.jp/records/3860