Acoustic propagation experiments have been carried out in the Florida Straits with a multi-frequency broadband source that transmitted M-sequence pulses over a range of 10 km to a sparse-filled vertical line array. The sound source was cycled in octaves from 100 Hz to 3200 Hz, transmitting each octave for one hour. This paper presents results of matched field inversions of the acoustic field data to estimate geoacoustic model parameters for the experimental site. The inversion is very sensitive to the sediment sound speed at the sea floor. The estimated value of 1560 m/s is consistent with fine-grain calcareous sand material that is considered to represent ground truth for the site.
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机译:在佛罗里达州海峡中,具有多频宽带源的声学传播实验,该宽带源在稀疏垂直线阵列10km的范围内传递M序列脉冲。声源在octaves从100 Hz到3200 Hz循环,传输每个八度音程一小时。本文介绍了声场数据的匹配现场逆的结果,以估算实验部位的地理声学模型参数。反演对海底的沉积物声速非常敏感。估计值1560 m / s是与细粒钙质砂材料一致,被认为是该网站的基础事实。
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