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中文核心期刊

单波束测深仪沉积层地声反演底质分类

Sediment classification with seafloor geoacoustic inversion using a single-beam echosounder

  • 摘要: 应用一种时域高频后向散射模型,对黄渤海41个站位的20 kHz单波束测深仪回波数据进行了沉积层地声参数反演底质分类研究。采用下山单行模拟退火算法(SIMPSA)对模型输出和接收回波的平均包络曲线进行最大似然匹配,估计海底沉积层的平均颗粒度。实验数据处理表明:对接收回波包络进行能量归一化处理有效地减小了由实验不确定性所导致的回波幅度异常起伏,将反演参数的方差降低至未加处理的50%;平均颗粒度的反演最优值与沉积层样本实验室测量值的一致性更高;将反演结果用于底质分类,正确识别率达到75.6%。

     

    Abstract: Bottom backscattered echoes of 41 sites located in the north of Yellow Sea and Bohai Sea were acquired by a vertically oriented echosounder working at 20 kHz.Based on a time domain incoherent intensity model of seafloor high frequency backscattering,the sediment classification with inversion of seafloor sediment geoacoustic parameters is investigated.By maximum likelihood matching between the averaged echo envelope and the model output with a global simulated annealing-downhill simplex optimization(SIMPSA),the sediment mean grain size is estimated.It is found that the fluctuation of the echo and the variance of the estimated parameters are effectively reduced once the echo envelope is normalized by the total echo energy before calculating the averaged envelope.And the estimated parameters are consistent with the ground truth.Simultaneously,the percentage of totally correct classification is 75.6%.

     

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