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Acoustic methane seepage quantification model design, experiments and deep-sea application

机译:声学甲烷渗流量化模型设计,实验和深海应用

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Detailed acoustic measurements of methane bubble distribution and plume dynamics were conducted during the Meteor M72/1 research survey in a deep marine hydrocarbon seep environment. This is located within the Dnepr paleodelta (North-West Black Sea) at a water depth of up to 2000m. Two sonar systems were employed; one is a PARASOUND echosounder (used for detection and localization of the seepage points at the seafloor) and the second is a horizontally looking sonar mounted on a remotely operated vehicle (ROV), used for gas flux quantification. The evolution of several bubble plumes was followed during their rise through the water column. It was detected that the dissolution of methane had a significant impact on the acoustic backscatter, especially in the region below the gas hydrate stability zone. Strong methane seepage flows were observed with volume fluxes ranging from 150 mm3/s to 600 mm3/s, measured from single outlets at the seafloor and rising up to 200 m bellow the water surface, thus demonstrating the rapid exchange of gases within the water column. A comparison with experimental data shows good agreement with predicted gas volume fluxes.
机译:在深海碳氢化合物渗透环境中的Meteor M72 / 1研究调查期间进行了详细的甲烷泡沫分布和羽流动力学的声学测量。这位于Dnepr Paleodelta(西北黑海)的水深,达到2000米的水深。使用了两个声纳系统;一个是解释的回路器(用于海底的渗水点的检测和定位),第二个是安装在用于气体通量量化的远程操作车辆(ROV)上的水平看声纳。在它们升高通过水柱期间,遵循几个泡沫羽毛的演变。检测到甲烷的溶解对声反向散射有显着影响,特别是在气水合物稳定区以下的区域中。用从海底的单个插座测量的体积助熔剂测量的体积助熔剂,从海底的单个插座测量,从海底上升到水面,展示了强甲烷渗流流量,从而展示了水柱内的气体迅速交换。与实验数据的比较显示了与预测的气体体积通量的良好一致性。

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