Determination of deuterium concentration in melted ice samples by the chromium reduction method

Antarctic Record

Volumn 47, Issue 2, 2003, Pages 101-110

  Motoyama, Hideaki ^a   Morimoto, Shinji ^a   Watanabe, Okitsugu ^a  

^a NATIONAL INSTITUTE OF POLAR RESEARCH   (Japan)

Author keywords

[No Author keywords available]

Indexed keywords

DEUTERIUM; ICE SHEET; ISOTOPIC COMPOSITION; MELTWATER; METHODOLOGY;

ANTARCTICA;

EID: 1242322072     PISSN: 00857289     EISSN: None     Source Type: Journal    
DOI: None     Document Type: Article

References (10)

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2. Friedman, I.I. (1953): Deutrium content of natural water and other materials. Geochim. Cosmochim. Acta, 15, 218-228.
3. Gehre, M., Hoefling, R., Kowski, P. and Strauch, G. (1996): Sample preparation device for quantitative hydrogen isotope analysis using chromium metal. Anal. Chem., 68, 4414-4417.
4. Gonfiantini, R., Stichler, W. and Rozanski, K. (1995): Standards and intercomparison materials distributed by the International Atomic Energy Agency for stable isotope measurements. Reference and Intercomparison Materials for Stable Isotopes of Light Elements, IAEA-TECDOC-825, International Atomic Energy Agency, 13-29.
5. Horita, J. (1988): Procedure for the hydrogen isotope analysis of water from concentrated brines. Chem. Geol.,: Isot. Geosci. Sect., 71, 85-88.
6. (1973): 53-61 (3). Chinese source.
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9. Watanabe, O., Kamiyama, K., Motoyama, H., Igarashi, M., Matoba, S., Shiraiwa, T., Yamada, T., Shoji, H., Kanamori, S., Kanamori, N., Nakawo, M., Ageta, Y., Koga, S. and Satow, K. (1997): Preliminary report on analyses of melted Dome Fuji core obtained in 1993. Proc. NIPR Symp. Polar Meteorol. Glaciol., 11, 14-23.
10. Watanabe, O., Fujii, Y., Kamiyama, K., Motoyama, H., Furukawa, T., Igarashi, M., Kohno, M., Kanamori, S., Kanamori, N., Agete, Y., Nakawo, M., Tanaka, H., Satow, K., Shoji, H., Kawamura, K., Matoba, S. and Shimada, W. (1999): Basic analyses of Dome Fuji deep ice core, Part 1: Stable oxygen and hydrogen isotope ratios, major chemical compositions and dust concentration. Polar Meteorol. Glaciol., 13, 83-89.