日本地球惑星科学連合2016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-TT28] 地球化学の最前線:未来の地球化学を展望して

2016年5月22日(日) 10:45 〜 12:15 A04 (アパホテル&リゾート 東京ベイ幕張)

コンビーナ:*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)、角野 浩史(東京大学大学院総合文化研究科広域科学専攻相関基礎科学系)、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)、平田 岳史(京都大学大学院理学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)、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)、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(国立研究開発法人海洋研究開発機構・海底資源研究開発センター)、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 高解像度環境解析研究センター)、座長:角野 浩史(東京大学大学院総合文化研究科広域科学専攻相関基礎科学系)、横山 哲也小畑 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)

11:45 〜 12:00

[MTT28-11] FTICR-MS解析の土壌有機物への適用

*池谷 康祐1,3Sleighter Rachel2Hatcher Patrick2渡邉 彰3 (1.農業環境技術研究所、2.オールドドミニオン大学、3.名古屋大学)

キーワード:土壌有機物、質量分析

Fourier transform ion cyclotron resonance mass spectrometry (FTICR-MS) has an ultrahigh resolution which makes it possible that respective organic molecules detected are accurately assigned to a molecular formula. Soil organic matter plays important roles associated with crop productivity and carbon sequestration. However, the chemical structure is still unknown. We applied this technique to some humic and fulvic acids that were chemically extracted and separated from some typical soils in Japan.
Materials and methods
Humic acids (HAs) were prepared from ten Japanese soils to cover varying degrees of humification and fulvic acids (FAs) were prepared from four Japanese and one Chinese soils according to NAGOYA method or IHSS method. The degree of humification of HAs was evaluated with the absorbance at 600 nm per mg C mL-1 (A600/C) and the ratio of absorbances at 400 and 600 nm on a logarithmic scale [log(A400/A600)]. Based on these two variables, HAs were classified into four types: Rp < P < B < A, with the degree of humificaiton increasing in this order. The FTICR-MS was performed according to Sleighter and Hatcher (2008). The molecular formulas assigned were examined using the van Krevelen diagram, double bond equivalent (DBE), and Kendrick mass defect (KMD) analysis that focusing on condensed aromatic structure.
Results
1) The number of molecular formulas in the condensed aromatic region increased from Type Rp (124-374) HAs to Type A HAs (751-1008). The sum of the peak magnitudes of the condensed aromatic components increased with increasing degree of humification.
2) The largest DBE values tended to be larger in the order: Type A (33) > Type B (30) > Type P (27) > Type Rp (25) HAs.
3) The KMD analysis indicated that potential structures of condensed aromatic components having 2-10 rings could occur in the soil HAs. The largest number of the rings increased in the order: Types Rp and P (7) < Type B (9) < Type A (10) HAs.
4) The KMD analysis indicated that potential structures of condensed aromatic components having up to 7 rings could occur in the five FAs.