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

机译:过去大气中冰芯和CO_2以及CH_4浓度的空气提取系统

摘要

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°42u27S, 44°20u27E) 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.
机译:已经开发了干法和熔体提取系统,分别确定极地冰芯中捕获的古代空气的CO_2和CH_4浓度。经证实,该日提取系统能够在2分钟内将1kg的岩心样品破碎成细粉,其空气提取效率估计为98%。用于CH_4测量的空气是通过在真空室内融化岩心样品而提取的。使用气相色谱法测定CO_2和CH_4的浓度。我们分析的总体精度优于CO_2的±1 ppmv和CH_4的±10 ppbv。在这项研究中使用了两个南极冰芯。在瑞穗站(70°42 u27S,44°20 u27E)钻出的冰芯显示,工业化前的CO_2和CH_4浓度(3300-200 yrs BP)分别为279-287 ppmv和690-750 ppbv,在过去的200年中,这两种浓度均迅速增加。还发现,在800至200年BP之间的CO_2浓度比工业化前剩余时间内的CO_2浓度高出将近7 ppmv,这可能是由于海洋和/或生物圈中的CO_2释放所致。在冰流末期附近(大和山脉附近)钻出的大和岩心分别显示出CO_2和CH_4的浓度分别为230-240 ppmv和530-580 ppbv,这显然低于冰川后的背景水平,这表明岩心是在冰河时期形成的。

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