日本地球惑星科学連合2018年大会

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[EE] 口頭発表

セッション記号 S (固体地球科学) » S-IT 地球内部科学・地球惑星テクトニクス

[S-IT25] Deep Carbon: Diamond formation and carbon speciation in Earth and planetary processes

2018年5月22日(火) 10:45 〜 12:15 A11 (東京ベイ幕張ホール)

コンビーナ:大谷 栄治(東北大学大学院理学研究科地学専攻)、Litasov Konstantin(V.S. Sobolev Institute of Geology and Mineralogy SB RAS)、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、共同)、Craig E Manning (University of California Los Angeles)、座長:鍵 裕之(東京大学)、大谷 栄治(東北大学)

12:00 〜 12:15

[SIT25-06] Behavior of nitrogen contained aromatic compound under high-pressure and high-temperature conditions under deep interior of the Earth.

*篠崎 彩子1三村 耕一2西田 民人2 (1.北海道大学、2.名古屋大学)

キーワード:沈み込み帯、窒素、高温高圧実験

Aromatic compounds are known to the most abundant organic materials in nature and sediments in the Earth’s surface and also in interstellar clouds and carbonaceous meteorites. Furthermore, aromatic compounds are found in inclusions from mantle xenoliths (Garanin et al., 2011; Tomilenko et al., 2016). Behavior of aromatic hydrocarbon molecules in the interior of the Earth has been investigated in experimental approaches. Temperature-induced oligomerization of polycyclic aromatic hydrocarbons was found at around 800 K at high pressure conditions (Chanyshev et al., 2015, Chanyshev et al., 2017). In this study, chemical reactivity and reaction pathway of a nitrogen-containing heteroaromatic compound under high-pressure and high-temperature were investigated experimentally.

For the high-pressure and temperature experiments, phthalazine (C8H6N2) was applied as a starting material. A piston-cylinder type high pressure apparatus was used for the experiments at 0.5-1.5 GPa and 374-573 K. After the experiments, the samples were recovered to ambient condition and then, analyzed using elemental analyzer, GC-FID, GC-MS, and MALDI-TOF/MS.

Decreasing of remained phthalazine and formation of various reaction products were observed >523 K at 0.5 GPa and >548 K at 1.5 GPa, indicating a chemical reaction of phthalazine. Significant decreasing of N/C ratio in the solid reaction products was observed with the chemical reaction, indicating selective distribution of nitrogen into volatile phase. MALDI-TOF/MS analysis showed that the various reaction products have heavier mass number than the phthalazine up to m/z=780, indicating that the reaction mechanism includes oligomerization of phthalazine. Precise analyses for molar weights and possible molecular structure of the reaction products were performed using GC-FID and GC-MS to reveal the reaction pathway of phthalazine and the effect of pressure. In the presentation, the behavior of nitrogen contained in aromatic compounds under deep interior of the Earth will be discussed from the experimental result.