新英格兰泥区剪切和压缩地球声剖面的贝叶斯匹配场反演

IF 1.2 Q3 ACOUSTICS
Stan E Dosso, Preston S Wilson, David P Knobles, Julien Bonnel
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引用次数: 0

摘要

本文通过对匹配场声波数据的跨维贝叶斯反演,在20-2000 Hz的带宽范围内估计了新英格兰泥块的剪切和压缩海底地球声剖面。结果表明,在大部分上部泥浆层中,剪切波速度较低(~ 35 m/s),不确定性相对较小,在下伏过渡层和砂层中增加。纵波参数,包括衰减,也可以很好地估计,但横波衰减很难确定。对比含/不含剪切参数的反演和考虑参数间相关性表明,除了砂层中的压缩波衰减外,压缩参数的估计基本上不受剪切效应的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Bayesian matched-field inversion for shear and compressional geoacoustic profiles at the New England Mud Patcha).

This Letter estimates shear and compressional seabed geoacoustic profiles at the New England Mud Patch through trans-dimensional Bayesian inversion of matched-field acoustic data over a 20-2000 Hz bandwidth. Results indicate low shear-wave speeds (∼35 m/s) with relatively small uncertainties over most of the upper mud layer, increasing in underlying transition and sand layers. Compressional parameters, including attenuation, are also well estimated, but shear-wave attenuation is poorly determined. Comparison of inversions with/without shear parameters and consideration of inter-parameter correlations indicate that estimates of compressional parameters are not substantially influenced by shear effects, with the possible exception of compressional-wave attenuation in the sand layer.

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CiteScore
1.70
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