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Mid-frequency geoacoustic inversion of source tow data from the ASIAEX east china sea experiment

机译:来自ASIAEX东海实验的震源数据中频地声反演

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During the 2001 ASIAEX East China Sea experiment, source tow data were collected by a 16-element, 75-m aperture vertical line array in 105 m deep water. Continuous wave tonals at 95, 195, 295, 395, 805, 850, and 905 Hz were transmitted from a J-15 transducer at a nominal depth of 47 m. An environmental model in the study area initially was derived by matched-field geoacoustic inversion using the low frequency data (195, 295, and 395 Hz). The quality of the inversion was checked by source localization over an interval of time while the source range varied from 1 to 3.5 km. In this study, the mid-frequency data (805, 850, and 905 Hz) are incorporated into the inversion procedure. The results indicate that the bestfit model found using the lower frequency band can be extended one-octave higher in the application of MFP source localization despite higher sidelobe levels. The quality of the refined model again is confirmed by time-continuous, source localization using the higher frequency data over the same time interval.
机译:在2001年ASIAEX东海实验中,源拖曳数据是通过在105 m深水中的16个元素,75 m孔径的垂直线阵列收集的。 95、195、295、395、805、850和905 Hz的连续波音调是从J-15传感器以47 m的标称深度传输的。研究区域的环境模型最初是使用低频数据(195、295和395 Hz)通过匹配场地声反演得出的。在一定的时间间隔内,通过震源定位检查反演的质量,而震源范围从1到3.5 km不等。在这项研究中,中频数据(805、850和905 Hz)被合并到反演程序中。结果表明,尽管旁瓣水平较高,但在MFP源定位的应用中,使用较低频段找到的最佳拟合模型可以扩展到八分之一。精炼模型的质量再次通过在相同时间间隔内使用更高频率的数据进行连续的源定位来确认。

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