日本地球惑星科学連合2019年大会

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セッション記号 M (領域外・複数領域) » M-IS ジョイント

[M-IS21] ガスハイドレートと地球環境・資源科学

2019年5月28日(火) 10:45 〜 12:15 A02 (東京ベイ幕張ホール)

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)、後藤 秀作(産業技術総合研究所地圏資源環境研究部門)、座長:石田 直人戸丸 仁

11:45 〜 12:00

[MIS21-05] Sampling of Methane Bubble Plumes and Solid Gas Hydrate on the Cascadia Margin, Pacific Northwest

*John E Lupton1Tamara Baumberger1Robert W. Embley1Susan G. Merle1Camilla Wilkinson1Conrad Young2 (1.NOAA Pacific Marine Environmental Laboratory, Newport, Oregon, USA、2.Young Engineering, Ramona, CA. USA)

キーワード:methane, hydrate, Cascadia Margin

The Cascadia Margin along California, Oregon, and Washington is host to hundreds of offshore methane seeps that produce bubble streams that ascend through the water column. In addition to the bubble streams, seismic reflection studies have detected the presence of extensive methane hydrate deposits beneath the seafloor. There are also a few sites along the Cascadia Margin where hydrate deposits are exposed and visible on the seafloor. During an expedition in 2016, our group used an ROV to collect uncontaminated samples of the bubble stream gas at several Cascadia Margin sites using special gas-tight bottles. Although we have successfully obtained samples of the bubble streams, the question remains as to whether the bubble streams are produced by the dissociation of hydrate, or instead represent free gas ascending through the sediment. We have developed a new sampler in which small samples of hydrate can be hermetically sealed into a small gas-tight volume in-situ while incorporating only a small amount of ambient seawater. The hydrate is then allowed to dissociate in the sample volume without exposure to air or other contaminates. During a return expedition to the Cascadia margin in June 2018 we successfully sampled solid methane hydrate at two sites using this new sampler and also collected additional samples of the free gas bubble streams. The paper will compare the results from these hydrate collections with the composition of the free gas.