日本地球惑星科学連合2015年大会

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セッション記号 M (領域外・複数領域) » M-TT 計測技術・研究手法

[M-TT44] 地球化学の最前線: 未来の地球化学を展望して

2015年5月26日(火) 18:15 〜 19:30 コンベンションホール (2F)

コンビーナ:*平田 岳史(京都大学大学院理学研究科地球惑星科学専攻)、高橋 嘉夫(東京大学大学院理学系研究科地球惑星科学専攻)、角皆 潤(名古屋大学大学院環境学研究科)、小畑 元(東京大学大気海洋研究所海洋化学部門海洋無機化学分野)、橘 省吾(北海道大学大学院理学研究院自然史科学専攻地球惑星システム科学分野)、鈴木 勝彦(独立行政法人海洋研究開発機構・地球内部ダイナミクス領域)、下田 玄(産業技術総合研究所地質調査総合センター)、鍵 裕之(東京大学大学院理学系研究科附属地殻化学実験施設)、横山 祐典(東京大学 大気海洋研究所 海洋底科学部門/地球表層圏変動研究センター)、横山 哲也(東京工業大学大学院理工学研究科地球惑星科学専攻)

18:15 〜 19:30

[MTT44-P03] 年代サイトメトリー推進のためのICP質量分析計の開発

*平田 岳史1服部 健太郎1坂田 周平1折橋 裕二2 (1.国立大学法人京都大学、2.国立大学法人東京大学地震研究所)

Age distribution (age cytometry) is one of the most principal and versatile information to decode the geological events underlying the Earth evolution. To take full advantage of the age cytometry, both the high analytical throughput and the better precision in the age determination is severely desired. Combination of laser ablation sampling technique and the high-sensitivity ICP-mass spectrometer (LA-ICPMS) enables us to measure precise U-Pb ages directly from the small area in the solid samples. Recently, both the precision and reliability of the U-Pb age data was dramatically improved by both the newly developed ion counting technique using the attenuator device and the correction technique for the initial disequilibrium for the U-Th-Pb decay series (Sakata et al., 2014). Moreover, magnetic sector-based mass spectrometry equipped with the multiple-ion counting system results in much higher analytical precision in the Pb/U and Pb/Th isotope ratio measurements. With the multiple-ion counting system, the analysis time for the U-Pb age determination could be dramatically shortened down to 1 - 5 sec, which was almost 1/4 - 1/10 levels over the conventional U-Pb age determinations using the single collector ICPMS instruments. This suggests that both the higher analytical throughput and the better precision in the Pb/U ratio measurements could be achieved. The problem associated with the multi-ion counting technique would be a time-dependent changes in the gain and the background (dark noise) of the multipliers. This is one of the large sources of analytical error in the U-Th-Pb age determinations. To overcome this, multiple-ion counting system using Daly ion collectors was employed in our MC-ICPMS system.

Several unique features could be achieved by the Daly ion counter, such as (a) wider dynamic range of the ion counting up to <10 Mcps, (b) smaller time-changes in gain and background level of the collector, and (c) better peak parallelism (peak flatness) over the conventional multipliers. Only the problem associated with the Daly counter is that the width of the Daly collector would be significantly larger than the mass dispersion for the heavier elements. In this study, two pairs of ion deflectors were used to obtain wider mass dispersion for the ion beams. With the multiple ion counting using the Daly ion counters, better precision and smaller contribution of the time-dependent changes in the gain and background counts could be achieved.

In this presentation, new ion collector system was applied to the MC-ICPMS system, and the preliminary results on the Pb/U and Pb/Th isotope ratio measurements and age determinations on zircon samples will be described.