AIR EXTRACTION SYSTEMS FOR ICE CORE AND CO_2 AND CH_4 CONCENTRATIONS IN THE PAST ATMOSPHERE

• Main Authors: ナカザワ タカキヨ, マチダ トシノブ, エスミ ケンジ, タナカ マサユキ, フジイ ヨシユキ, アオキ シュンジ, ワタナベ オキツグ, Takakiyo NAKAZAWA, Toshinobu MACHIDA, Kenji ESUMI, Masayuki TANAKA, Yoshiyuki FUJII, Shuhji AOKI, Okitsugu WATANABE
• Format: Report
• Language: English
• Published: ABSTRACT 1992
• Subjects: Antarctic; Mizuho; Yamato; Mizuho Station; Antarc*; ice core; Polar meteorology and glaciology; Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology
• Online Access: https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3716; http://id.nii.ac.jp/1291/00003716/; https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3716&item_no=1&attribute_id=18&file_no=1

Dry and melt extraction systems have been developed to determine respectively the CO_2 and CH_4 concentrations of ancient air trapped in the polar ice core. The day extraction system was confirmed to be capable of crushing a core sample of 1kg to fine powder within 2 min, and its air extraction efficiency was estimated to be 98%. The air for the CH_4 measurements was extracted by melting core samples in an evacuated chamber. The CO_2 and CH_4 concentrations were determined using gas chromatography. The overall precision of our analyses is better than ±1 ppmv for CO_2 and ±10 ppbv for CH_4. Two Antarctic ice cores were used in this study. The ice core drilled at Mizuho Station (70°42'S, 44°20'E) showed that pre-industrial levels of the CO_2 and CH_4 concentrations (3300-200 yrs BP) were 279-287 ppmv and 690-750 ppbv, respectively and both concentrations increased rapidly for the last 200 years. It was also found that the CO_2 concentrations between 800 and 200 yrs BP were higher by almost 7 ppmv than those in remaining pre-industrial time, due probably to CO_2 release from the oceans and/or the biosphere. The Yamato core drilled near the end of ice flow (near the Yamato Mountains) showed concentrations of 230-240 ppmv and 530-580 ppbv for CO_2 and CH_4,respectively, which are apparently lower than post-glacial background levels, implying that the core was formed in the glacial period.