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Geo-Acoustic Model and Acoustic Reflection Properties of Fluid Mud Layers in Estuaries

机译:河口流体泥层的地声模型和声反射特性

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A generalized geo-acoustic model of a fluid mud layer in estuaries of East China Sea has been derived from a large amount of field measurements of the bulk-density profiles of the layer, and of lab measurements of the acoustic velocities and attenuation coefficients of the fluid mud samples with different values of bulk-density for the frequencies of 100, 150, 500, and 1500 kHz. Based on the geo-acoustic model, the simulations of the acoustic reflection property of the fluid mud layer have been done by using the ray theory. The results confirm that the bulk-density profile of a fluid mud layer can be estimated and the effective water-depth for navigation in estuaries, which is defined by the criterion that the bulk-density of the fluid mud is less than 13 kN/m~3, can be determined by using echo sounding techniques.
机译:东海河口流体泥浆层的广义地球声学模型是通过大量实地测量该层的体积密度剖面以及实验室测量的声波速度和衰减系数得出的。在100、150、500和1500 kHz频率下具有不同堆积密度值的流体泥浆样本。基于地声模型,利用射线理论对流体泥浆层的声反射特性进行了模拟。结果证实,可以估算出流体泥浆层的堆积密度分布图,并可以通过在河口中航行的有效水深来估算,这是由流体泥浆的堆积密度小于13 kN / m的标准定义的〜3,可以通过使用回声探测技术来确定。

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