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首页> 外文期刊>IEEE Journal of Oceanic Engineering >A Shallow-Water Reverberation Model Based on Perturbation Theory
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A Shallow-Water Reverberation Model Based on Perturbation Theory

机译:基于摄动理论的浅水混响模型

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摘要

ara> A shallow-water reverberation model is developed based on Bass perturbation theory. The key component for shallow-water reverberation modeling, the modal backscattering matrix (MBSM), has been investigated and the explicit analytic expressions of the MBSM both for the scattering due to interface roughness and due to sediment volume inhomogeneities are derived. For rough interface scattering, it is shown that the angular dependence and the frequency dependence of the MBSM can be separated: the angular dependence is given by $sin^{2}(theta_{m} {rm P}/2)sin^{2} (theta_{n}{rm P}/2)$, where $theta_{m}$ is the modal grazing angle and ${rm P}$ is a bottom parameter related to the bottom reflection phase shift, and the frequency dependence is given by $k_{0}^{4 - n}$, where $n$ depends on the power spectrum of the roughness, for instance, $n = 3$ for Goff–Jordan spectrum. The difference between the scattering due to sediment volume inhomogeneities and the scattering due to rough interface is that there is an extra factor contributed by the vertical correlation and the exponential attenuation of the modal function weighting on the vertical direction in the sediment medium. This extra factor has some important impacts: 1) there will be, in general, a coupled angular-frequency behavior, 2) the angular pattern will decrease more rapidly at small grazing angle area, and 3) the angular pattern is no longer separable. It is shown that only for a “thin” layer (or low frequency), the scattering due to volume inhomogeneities will have a similar behavior a- - s the scattering due to rough interface. The significant feature of the angular pattern for both kinds of scattering is a marked departure from Lambert's law at small grazing angle area. The explicit analytic expression of the MBSM, and the differences between the two kinds of bottom scattering, given in this paper, provide the opportunity for a comprehensive model-data comparison and a better understanding of the scattering mechanism.
机译:ara>基于低音扰动理论,建立了浅水混响模型。研究了浅水混响建模的关键成分,模态后向散射矩阵(MBSM),并推导出了MBSM对由于界面粗糙度和沉积物体积不均匀性引起的散射的明确解析表达式。对于粗糙的界面散射,表明可以将MBSM的角度依赖性和频率依赖性分开:角度依赖性由<公式公式类型=“ inline”> $ sin ^ {2 }(theta_ {m} {rm P} / 2)sin ^ {2}(theta_ {n} {rm P} / 2)$ ,其中 < tex Notation =“ TeX”> $ theta_ {m} $ 是模态掠角, $ {rm P} $ < / tex> 是与底部反射相移有关的底部参数,并且频率依赖性由 $ k_ {0} ^ {4 -n} $ ,其中 $ n $ 取决于粗糙度的功率谱,例如,对于Goff–Jordan光谱, $ n = 3 $ 。由沉积物体积不均匀性引起的散射与由粗糙界面引起的散射之间的差异在于,在沉积介质中,垂直相关性和模态函数加权在垂直方向上的指数衰减有一个额外的因素。这个额外的因素有一些重要的影响:1)通常会有一个耦合的角频率行为; 2)在较小的掠角区域,角度模式会更快地减小; 3)角度模式不再可分离。结果表明,仅对于“薄”层(或低频),由于体积不均匀引起的散射将具有类似的行为,即由于粗糙界面而引起的散射。两种散射的角度模式的显着特征是在小掠角区域明显偏离了朗伯定律。本文给出了MBSM的显式解析表达式以及两种底部散射之间的差异,为全面的模型数据比较和更好地理解散射机理提供了机会。

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