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浅海地声参数宽带匹配场反演的实验研究 被引量:9

Experimental Research for Geoacoustic Inversion Using Broadband Matched Field in Shallow Water
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摘要 根据不同浅海环境参数在不同的频段对匹配场功率具有不同贡献的特点 ,提出了宽带匹配场反演的多步优化策略 ,并与直接全参数反演进行了实测数据的性能对比。采用多步反演策略对亚洲海实验 ( ASIAEX2 0 0 1 )数据进行处理 ,按照不同海区水文条件的差异 ,分别进行了水平不变和水平变化的环境参数反演 ,得到了东中国海 Inversion by MFP (Matched Field Processing) can be considered as a complex non linear optimization problem. The accuracy with which a parameter can be inverted effectively depends mainly on the extent of its influence on the acoustic field. Sensitive parameters can be estimated accurately and quickly as compared with less sensitive parameters. In order to get satisfactory inversion results of environmental parameters from ASIAEX2001 (Asian Seas International Acoustics Experiment) in the ECS (East China Sea) in June 2001, we studied the sensitivity of the inverted parameters including geometric and geoacoustic parameters at different frequencies. Fig.3 (a) gives the sensitivity indices of five geometric parameters--1.range, 2.water depth, 3.source depth, 4.receiver depth, 5.array tilt--at four typical frequencies--40Hz, 210Hz, 470Hz, 670 Hz. Fig.3 (b) gives sensitivity indices of 4 sediment parameters --1.thickness, 2.attenuation, 3.density, 4.sound speed--at the same four typical frequencies. Fig.3(c) gives sensitivity indices of 3 bottom parameters --1.sound speed, 2.attenuation, 3.density--also at the same four typical frequencies. Taking into consideration the fact that different parameters have different sensitivitiy indices on MFI (Matched Field Inversion) power, we propose a new approach named MS MFI (Multi Step MFI). The MS MFI scheme presented in Fig.4 is, in our opinion, ideal for complex geoacoustic models involving large number of unknowns. We divide the total parameter space into a few subspaces and perform inversion in each subspace. Firstly, in inverting the more sensitive parameters, we use high frequency data. Secondly, in inverting the less sensitive parameters, we use one or two high and several low frequency data. Finally, in inverting the least sensitive parameters, we use low frequency data. If necessary, we execute these three steps iteratively until we get suitable values. Subsection 1.2 gives four advantages for MS MFI as compared with DAP MFI (Direct All Parameters MFI). Using multi
机构地区 西北工业大学
出处 《西北工业大学学报》 EI CAS CSCD 北大核心 2003年第5期611-615,共5页 Journal of Northwestern Polytechnical University
基金 国家自然科学基金 (6 0 0 72 0 2 5 ) 西北工业大学"英才培养计划"基金资助
关键词 宽带匹配场反演 亚洲海实验 多步反演策略 MFP (Matched Field Processing), ASIAEX (Asian Seas International Acoustic Experiments), DAP MFI (Direct All Parameters Matched Field Inversion), MS MFI (Multi Step Matched Field Inversion)
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参考文献9

  • 1杨坤德,马远良,杨益新,张忠兵.匹配场反演结果的后验概率分析[J].西北工业大学学报,2002,20(4):637-641. 被引量:4
  • 2卢博 黄韶健 张福生.东海大陆架某海区海底沉积物及其声学物理性质[A]..陕西省2002年声学学术会议论文集[C].,2002.42~45. 被引量:1
  • 3Potty G R, Miller J H. Tomographic Inversion for Sediment Parameters in Shallow Water. J Acoust Soc Am, 2000,108(3) : 973~986. 被引量:1
  • 4Yang Kunde, Ma Yuanliang. Shallow Water Broadband Matched Field Inversion with Multi-Step Strategy. The 3rd Intgrnational Workshop on Acoustical Engineering and Technology, Harbin, China, 2002. 被引量:1
  • 5Lynch J. ASIAEX East China Sea Cruise Report. Hawaii, ASIAEX2000 Workshop, 2000. 被引量:1
  • 6Porter M. The KRAKEN Normal Mode Program. Saclantcen Mem. , SM-245, 1991. 被引量:1
  • 7Dahl P H. ASIAEX East China Sea Cruise Report on the Activities of the R/V Melville. ASIAEX2001 Report, 2001. 被引量:1
  • 8Miller J H. Geoacoustic Measurements in the East China Sea. ASIAEX Workshop, Chengdu, China, 2002. 被引量:1
  • 9Hamilton E L. Geoacoustic Modeling of the Sea Floor. J Acoust Soc Am, 1980, 68(5): 1313~1340. 被引量:1

二级参考文献5

  • 1[1]Potty G P, Miller J H. Tomographic Inversion for Sediment Parameters in Shallow Water. J Acoust Soc Am, 2000, 108(3): 973~986 被引量:1
  • 2[2]Gerstoft P. Inversion of Seismoacoustic Data Using Genetic Algorithms and a Posteriori Probability Distribution. J Acoust Soc Am, 1994, 95(2): 770~782 被引量:1
  • 3[3]Gerstoft P. Ocean Acoustic Inversion with Estimation of a Posteriori Probability Distribution. J Acoust Soc Am, 1998, 104(2): 808~819 被引量:1
  • 4[4]Lynch J. ASIAEX 2000 East China Sea Cruise Report. Hawaii, ASIAEX2000 Workshop, 2000 被引量:1
  • 5[5]Hamilton E L. Geoacoustic Modeling of the Sea Floor. J Acoust Soc Am, 1980, 68(5): 1313~1340 被引量:1

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