負イオン質量分析法による超高感度同位体分析とその地球化学・環境科学への応用

  • 鈴木 勝彦
    東京大学大学院総合文化研究科広域科学専攻広域システム科学系 (現)京都大学大学院理学研究科附属地球熱学研究施設

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タイトル別名
  • Highly sensitive analysis of isotope abundances through negative thermal ionization mass spectrometry and its application to geochemistry and environmental chemistry
  • 地球化学の新方法 負イオン質量分析法による超高感度同位体分析とその地球化学・環境科学への応用
  • チキュウ カガク ノ シン ホウホウ フイオン シツリョウ ブンセキホウ ニ ヨル チョウコウカンド ドウイタイ ブンセキ ト ソノ チキュウ カガク カンキョウ カガク エ ノ オウヨウ

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抄録

Negative thermal ionization mass spectrometry (N-TIMS) has been recently developed as a precise and accurate method in mass spectrometry to determine isotope ratios of some elements, which cannot be measured by positive thermal ionization mass spectrometry (P-TIMS) easily. In N-TIMS, isotopic compositions of elements, such as halogens, chalcogens, boron and platinum group elements with high ionization potentials, are determined as negative atomic ions M-, oxide ions MOx- (x=1-4) or fluoride ions MFx- (x=4). Recent interesting developments in geochemistry is the determinations of rhenium-osmium systematics, redetermination of the relative atomic masses of elements by more precise and more accurate isotope ratio measurements, the determination of isotope variations in geological and cosmic samples and the analysis of trace and ultra-trace amounts of elements in the environment. In this paper, after theory and characteristics of N-TIMS are mentioned, some recent applications of N-TIMS is summarized in the field of geochemistry and environmental chemistry. Among recent topics, (1) application to rhenium-osmium systematics, (2) precise boron isotope analysis and its application to environmental chemistry, and (3) precise iron isotope analysis and its application to biological and medical use are described. Problems involved in N-TIMS are also discussed.

収録刊行物

  • 地球化学

    地球化学 33 (2), 67-102, 1999

    一般社団法人日本地球化学会

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