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Estimates of geoacoustic model parameters from inversions of horizontal and vertical line array data

机译:根据水平和垂直线阵列数据的反演估计地声模型参数

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This paper describes results from geoacoustic inversion of low-frequency acoustic data recorded at a receiving array divided into two sections, a sparse bottom laid horizontal array (HLA) and a vertical array (VLA) deployed in shallow water. The data are from an experiment conducted by the Norwegian Defence Research Establishment (FFI) in the Barents Sea, using broadband explosives (shot) sources. A two-layer range-independent geoacoustic model, consistent with seismic profiles from the area, described the environment. Inversion for geoacoustic model parameters was carried out using a fast implementation of the hybrid adaptive simplex simulated annealing (ASSA) inversion algorithm, with replica fields computed by the ORCA normal mode code. Low-frequency (40-128 Hz) data from six shot sources at ranges 3-9 km from the array were considered. Estimates of sediment and substrate p-wave velocities and sediment thickness were found to be consistent between independent inversions of data from the two sections of the array.
机译:本文描述了低频声学数据的地声反演的结果,该低频声学数据记录在分为两部分的稀疏底部铺设水平阵列(HLA)和部署在浅水中的垂直阵列(VLA)的接收阵列中。数据来自挪威国防研究机构(FFI)在巴伦支海进行的一项实验,使用宽带爆炸物(散弹)源。与该地区的地震剖面相一致的两层独立于范围的地声模型描述了环境。使用混合自适应单工模拟退火(ASSA)反演算法的快速实现来执行地声模型参数的反演,副本字段由ORCA正常模式代码计算。考虑了距离阵列3-9 km范围内六个发射源的低频(40-128 Hz)数据。发现沉积物和基质的p波速度以及沉积物厚度的估计值在来自阵列两部分的独立数据反演之间是一致的。

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