日本地球惑星科学連合2018年大会

講演情報

[JJ] Eveningポスター発表

セッション記号 M (領域外・複数領域) » M-IS ジョイント

[M-IS17] ガスハイドレートと地球環境・資源科学

2018年5月22日(火) 17:15 〜 18:30 ポスター会場 (幕張メッセ国際展示場 7ホール)

コンビーナ:戸丸 仁(千葉大学理学部地球科学科)、八久保 晶弘(北見工業大学)、谷 篤史(神戸大学 大学院人間発達環境学研究科、共同)、後藤 秀作(産業技術総合研究所地圏資源環境研究部門)

[MIS17-P14] Geochemical characteristics of hydrocarbons and ions within gas chimney structures in the Tsushima Basin and the Oki Trough, eastern margin of the Japan Sea

*井口 彩1戸丸 仁1茂手木 竜也2石田 直人2松本 良3 (1.千葉大学大学院融合理工学府、2.鳥取大学大学院工学研究科、3.明治大学ガスハイドレート研究所)

キーワード:ガスチムニー、炭化水素ガス、日本海

Shallow gas hydrate often develops on gas chimney structures associated with mound/pockmarks in the eastern margin of the Japan Sea, however, the distribution and reaction of gas and ion dissolved in pore water inside the chimney is not well understood. We retrieved sediment cores from the well-developed gas chimneys with mound in the southeastern margin of Tsushima Basin and western and eastern Oki Trough to characterize the geochemical compositions of gas and ion, and compare their variations with regional geology including subsurface/thermal structures.
Concentrations of sulfate dissolved in pore waters rapidly decrease with depth to the sulfate-methane interface (SMI). Contrarily, concentrations of methane increase downward from the depth of the SMI. Methane/ethane ratios are low (<100) above the SMI, however, those rapidly increase below the SMI particularly on the mound sites with gas chimney structure. This is because methane was oxidized anaerobically by the sulfate at the depth of SMI and methane was generated by methanogenic bacteria below the SMI. The thermogenic methane generated at greater depth is also dominant at the gas chimney site where the geothermal gradient is generally high, the distribution of deep-sourced materials are significant near the seafloor in these locations.