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南黄海砂质海底反向声散射测量(6-24 kHz)
引用本文:阚光明,刘保华,杨志国,于盛齐,戚乐华,于凯本,裴彦良.南黄海砂质海底反向声散射测量(6-24 kHz)[J].海洋学报(英文版),2019,38(5):99-108.
作者姓名:阚光明  刘保华  杨志国  于盛齐  戚乐华  于凯本  裴彦良
作者单位:海洋沉积与环境地质国家海洋局重点实验室, 国家海洋局第一海洋研究所, 青岛 266061, 中国;青岛海洋科学与技术试点国家实验室, 海洋地质过程与环境功能实验室, 青岛 266237, 中国,青岛海洋科学与技术试点国家实验室, 海洋地质过程与环境功能实验室, 青岛 266237, 中国;国家深海基地管理中心, 国家海洋局, 青岛 266237, 中国,青岛海洋科学与技术试点国家实验室, 海洋地质过程与环境功能实验室, 青岛 266237, 中国;国家深海基地管理中心, 国家海洋局, 青岛 266237, 中国,青岛海洋科学与技术试点国家实验室, 海洋地质过程与环境功能实验室, 青岛 266237, 中国;国家深海基地管理中心, 国家海洋局, 青岛 266237, 中国,海洋沉积与环境地质国家海洋局重点实验室, 国家海洋局第一海洋研究所, 青岛 266061, 中国;中国海洋大学海洋地球科学学院, 青岛 266100, 中国,青岛海洋科学与技术试点国家实验室, 海洋地质过程与环境功能实验室, 青岛 266237, 中国;国家深海基地管理中心, 国家海洋局, 青岛 266237, 中国,海洋沉积与环境地质国家海洋局重点实验室, 国家海洋局第一海洋研究所, 青岛 266061, 中国;青岛海洋科学与技术试点国家实验室, 海洋地质过程与环境功能实验室, 青岛 266237, 中国
基金项目:The Opening Fund of Pilot National Laboratory for Marine Science and Technology (Qingdao) under contract No. QNLM2016ORP0209; the National Natural Science Foundation of China under contract Nos 41330965, 41676055 and 41527809; the Taishan Scholar Project Funding under contract No. tspd20161007.
摘    要:在南黄海某一典型的砂质海底区域,采用全向性声源和全向性接收水听器开展了频率范围为6-24 kHz的海底反向声散射测量。测量结果表明,在避免海面散射干扰并满足远场条件的情况下,本次实验获得了掠射角范围为18~80°的海底反向声散射强度,其数值为-41.1~24.4 dB。在有效掠射角范围内,声散射强度总体上随掠射角的增大呈现出增大趋势,但对于不同的频率,其变化趋势有所不同,反映出不同的散射机理。在20°、40°和60°掠射角处,在6-24 kHz的频率范围内反向声散射强度总体上呈现出正相关的频率依赖性,其线性相关斜率分别为0.2229 dB/kHz、0.5130 dB/kHz、0.1746 dB/kHz。在最大掠射角80°处,反向声散射强度未呈现出明显的频率相关性。

关 键 词:反向声散射强度  砂质海底  南黄海  掠射角依赖性  频率依赖性
收稿时间:2018/8/6 0:00:00

Acoustic backscattering measurement from sandy seafloor at 6–24 kHz in the South Yellow Sea
KAN Guangming,LIU Baohu,YANG Zhiguo,YU Shengqi,QI Lehu,YU Kaiben and PEI Yanliang.Acoustic backscattering measurement from sandy seafloor at 6–24 kHz in the South Yellow Sea[J].Acta Oceanologica Sinica,2019,38(5):99-108.
Authors:KAN Guangming  LIU Baohu  YANG Zhiguo  YU Shengqi  QI Lehu  YU Kaiben and PEI Yanliang
Affiliation:Key Laboratory of Marine Sedimentology and Environmental Geology, First Institute of Oceanography, Ministry of Natural Resources, Qingdao 266061, China;Laboratory for Marine Geology and Environment, Pilot National Laboratory for Marine Science and Technology (Qingdao), Qingdao 266237, China,Laboratory for Marine Geology and Environment, Pilot National Laboratory for Marine Science and Technology (Qingdao), Qingdao 266237, China;National Deep Sea Center, Ministry of Natural Resources, Qingdao 266237, China,Laboratory for Marine Geology and Environment, Pilot National Laboratory for Marine Science and Technology (Qingdao), Qingdao 266237, China;National Deep Sea Center, Ministry of Natural Resources, Qingdao 266237, China,Laboratory for Marine Geology and Environment, Pilot National Laboratory for Marine Science and Technology (Qingdao), Qingdao 266237, China;National Deep Sea Center, Ministry of Natural Resources, Qingdao 266237, China,Key Laboratory of Marine Sedimentology and Environmental Geology, First Institute of Oceanography, Ministry of Natural Resources, Qingdao 266061, China;College of Marine Geosciences, Ocean University of China, Qingdao 266100, China,Laboratory for Marine Geology and Environment, Pilot National Laboratory for Marine Science and Technology (Qingdao), Qingdao 266237, China;National Deep Sea Center, Ministry of Natural Resources, Qingdao 266237, China and Key Laboratory of Marine Sedimentology and Environmental Geology, First Institute of Oceanography, Ministry of Natural Resources, Qingdao 266061, China;Laboratory for Marine Geology and Environment, Pilot National Laboratory for Marine Science and Technology (Qingdao), Qingdao 266237, China
Abstract:The acoustic bottom backscattering strength was measured at the frequency range of 6-24 kHz on a typical sandy bottom in the South Yellow Sea by using omnidirectional sources and omnidirectional receiving hydrophones. In the experiment, by avoiding disturbances due to scattering off the sea surface and satisfying the far-field condition, we obtained values of acoustic bottom backscattering strength ranging from -41.1 to -24.4 dB within a grazing angle range of 18°-80°. In the effective range of grazing angles, the acoustic scattering strength generally increases with an increase in the grazing angles, but trends of the variation were distinct in different ranges of frequency, which reflect different scattering mechanisms. The frequency dependence of bottom backscattering strength is generally characterized by a positive correlation in the entire frequency range of 6-24 kHz at the grazing angles of 20°, 40° and 60° with the linear regression slopes of 0.222 9 dB/kHz, 0.513 0 dB/kHzand 0.174 6 dB/kHz, respectively. At the largest grazing angle of 80°, the acoustic backscattering strength exhibits no evident frequency dependence.
Keywords:acoustic backscattering strength  sandy bottom  South Yellow Sea  gazing angle dependence  frequency dependence
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