日本海甲烷羽流的定量回声探测

C. Aoyama, R. Matsumoto, A. Hiruta, O. Ishizaki, H. Machiyama, H. Numanami, M. Hiromatsu, G. Snyder
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引用次数: 7

摘要

R&T/V Umitaka-maru(Tokyo university of Marine Science and Technology)和R/V Natsushima(JAMSTEC)分别于2004年、2005年和2006年航行到日本海东缘直越盆地一个小脊上的甲烷泄漏区,利用定量回声测深仪和多波束SONER对海底天然气水合物和甲烷羽流的相关声学特征进行了调查[1]。详细的水深剖面显示,在水深910米至980米的山脊上,在3公里乘4公里的范围内,有许多土丘、坑洼和崩塌结构。我们利用定量回声探测仪和GPS定位数据绘制了甲烷羽流。我们还通过回波积分器测量了甲烷羽流和海底每100米范围和每一分钟的平均回波强度。我们从目前的回声探测仪和SONER调查中得到以下结果。1)测量了各甲烷羽流的平均体积后向散射强度(SV)。羽状体的最强SV为-33dB,高于鱼群的SV。2)各甲烷羽流的平均SV倾向于与水温和水压有关。3)在观测到甲烷羽流的区域,我们通过活塞取心回收了几块拳头大小的甲烷水合物。4)利用该方法对甲烷气泡上浮点进行了检测,发现水合物气泡上浮至300 m深度的温水处。我们揭示了海底锥形容器中的水合物气泡。结果表明,该声学方法对了解水下甲烷水合物的行为和监测甲烷渗漏面积是有效的。作为后续项目,我们计划1)原位测量水柱中甲烷水合物气泡和漂浮的甲烷水合物的SV, 2)对漂浮的甲烷气泡和甲烷水合物的数量进行试算,3)研究如何使用sea侧扫声纳对甲烷羽流的声学数据进行采样。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Acoustical surveys of Methane plumes using the quantitative echo sounder in Japan Sea
R&T/V Umitaka-maru(Tokyo Univ. of Marine Science and Technology) and R/V Natsushima(JAMSTEC) sailed to the methane seep area on a small ridge in the Naoetsu Basin, in the eastern margin of the Sea of Japan in 2004,2005 and 2006 to survey the ocean floor gas hydrate and related acoustic signatures of methane plumes by using a quantitative echo sounder and a multi beam SONER [1]. Detailed bathymetric profiles have revealed a number of mounds, pockmarks and collapse structures within 3 km times 4 km on the ridge at the water depth of 910 m to 980 m. We mapped minutely methane plumes by using a quantitative echo sounder with positioning data from GPS. We also measured averaged echo intensity from the methane plumes and sea bottoms both in every 100 m range and very one minute by the echo integrator. We obtained the following results from the present echo-sounder and SONER surveys. 1) We measured the averaged volume backscattering strength (SV) of each methane plume. The strongest SV, -33dB, of the plumes was stronger than SV of fish school. 2) Averaged SV of each methane plume tend to be related to the water temperature and the water pressure. 3) We recovered several fist-sized chunks of methane hydrate by piston coring at the area where we observed the methane plumes. 4) Using this method, we detected methane bubbles floating up points and revealed that the hydrate bubbles float upward until they reach warm waters at 300 m depth. 5) We revealed the hydrate bubbles in the conic container on the sea bottom. Because of results this acoustical method was effective to know the behaviors of the methane hydrate under water and to monitor the area of the methane seep. As a following up project, we are planning 1) to measure SV of methane hydrate bubbles and methane hydrate floating in water columns in situ, 2) to make a trial calculation of amount of floating methane bubbles and methane hydrates and 3) to study how to sample the acoustical data of methane plumes using the side scanning SONAR, called SeaBat.
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