Determination of deuterium concentration in melted ice samples by the chromium reduction method
We measured the isotope ratio of hydrogen (δD) in melted ice samples by reduction of the water sample with chromium powder. The reproducibility of the δD measurement is within 1.0‰. The δD of surface snow from coast to inland on the Antarctica ice sheet was measured. The measurement range was from -...
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National Institute of Polar Research
2003-07-01
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Series: | Antarctic Record |
Online Access: | http://doi.org/10.15094/00009260 |
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doaj-72b520f0e7264bbc8a9f6fd734603c042020-11-24T22:48:54ZengNational Institute of Polar ResearchAntarctic Record0085-72892432-079X2003-07-0147210111010.15094/00009260Determination of deuterium concentration in melted ice samples by the chromium reduction method Hideaki Motoyama0Shinji Morimoto1Okitsugu Watanabe2National Institute of Polar ResearchNational Institute of Polar ResearchNational Institute of Polar ResearchWe measured the isotope ratio of hydrogen (δD) in melted ice samples by reduction of the water sample with chromium powder. The reproducibility of the δD measurement is within 1.0‰. The δD of surface snow from coast to inland on the Antarctica ice sheet was measured. The measurement range was from -200‰ to -400‰. The δD of surface snow decreased gradually from coast to inland. Variations of δD agree with δ^<18>O fluctuations. The deuterium excess in the coastal region was small, less than 10‰. We established the method of determining δD in melted ice samples, which can be used to investigate the global environment system. http://doi.org/10.15094/00009260 |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Hideaki Motoyama Shinji Morimoto Okitsugu Watanabe |
spellingShingle |
Hideaki Motoyama Shinji Morimoto Okitsugu Watanabe Determination of deuterium concentration in melted ice samples by the chromium reduction method Antarctic Record |
author_facet |
Hideaki Motoyama Shinji Morimoto Okitsugu Watanabe |
author_sort |
Hideaki Motoyama |
title |
Determination of deuterium concentration in melted ice samples by the chromium reduction method |
title_short |
Determination of deuterium concentration in melted ice samples by the chromium reduction method |
title_full |
Determination of deuterium concentration in melted ice samples by the chromium reduction method |
title_fullStr |
Determination of deuterium concentration in melted ice samples by the chromium reduction method |
title_full_unstemmed |
Determination of deuterium concentration in melted ice samples by the chromium reduction method |
title_sort |
determination of deuterium concentration in melted ice samples by the chromium reduction method |
publisher |
National Institute of Polar Research |
series |
Antarctic Record |
issn |
0085-7289 2432-079X |
publishDate |
2003-07-01 |
description |
We measured the isotope ratio of hydrogen (δD) in melted ice samples by reduction of the water sample with chromium powder. The reproducibility of the δD measurement is within 1.0‰. The δD of surface snow from coast to inland on the Antarctica ice sheet was measured. The measurement range was from -200‰ to -400‰. The δD of surface snow decreased gradually from coast to inland. Variations of δD agree with δ^<18>O fluctuations. The deuterium excess in the coastal region was small, less than 10‰. We established the method of determining δD in melted ice samples, which can be used to investigate the global environment system. |
url |
http://doi.org/10.15094/00009260 |
work_keys_str_mv |
AT hideakimotoyama determinationofdeuteriumconcentrationinmeltedicesamplesbythechromiumreductionmethod AT shinjimorimoto determinationofdeuteriumconcentrationinmeltedicesamplesbythechromiumreductionmethod AT okitsuguwatanabe determinationofdeuteriumconcentrationinmeltedicesamplesbythechromiumreductionmethod |
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1725678196397965312 |