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首页> 外文期刊>Oceanic Engineering, IEEE Journal of >Bayesian Inversion of Interface-Wave Dispersion for Seabed Shear-Wave Speed Profiles
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Bayesian Inversion of Interface-Wave Dispersion for Seabed Shear-Wave Speed Profiles

机译:海底剪切波速度剖面的界面波频散的贝叶斯反演

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This paper applies Bayesian inversion to estimate seabed shear-wave speed profiles and their uncertainties from interface-wave dispersion data. A nonlinear formulation is developed to estimate the most probable profile together with marginal probability distributions and credibility intervals from the posterior probability density (PPD) using adaptive hybrid optimization and Metropolis–Hastings sampling (MHS). To address correlated data errors, a full error covariance matrix is estimated from residual analysis, and rigorous a posteriori statistical tests are applied to validate the covariance estimate and the assumption of a multivariate Gaussian error distribution. The most appropriate parameterization for the shear-wave speed profile is determined using the Bayesian information criterion (BIC), which provides the simplest model consistent with the resolving power of the data. Parameterizations considered vary in the number and type of layers, and include layers with uniform speed, and with linear and power-law shear-speed gradients. For the data considered here, a power-law parameterization is indicated, which is consistent with theoretical expectations for uniform, unconsolidated sediments under overburden pressure. The maximum depth to which the dispersion data constrain the shear-speed profile is investigated using an approximate analytic formula for power-law profiles and repeated inversions in which the maximum depth to an underlying half-space is systematically increased.
机译:本文采用贝叶斯反演方法从界面波频散数据估计海床切变波速度剖面及其不确定性。使用自适应混合优化和Metropolis-Hastings采样(MHS),开发了一种非线性公式来估计最可能的轮廓以及边际概率分布和可信度间隔,这些概率均来自后验概率密度(PPD)。为了解决相关的数据错误,从残差分析中估计出完整的误差协方差矩阵,并应用严格的后验统计检验来验证协方差估计和多元高斯误差分布的假设。使用贝叶斯信息标准(BIC)确定最适合剪切波速度剖面的参数,该标准提供了与数据的解析能力一致的最简单模型。所考虑的参数化在层的数量和类型上有所不同,并且包括具有均匀速度以及线性和幂律剪切速度梯度的层。对于此处考虑的数据,显示了幂律参数化,这与上覆压力下均匀,未固结沉积物的理论预期一致。使用幂律曲线的近似解析公式和重复反演来研究分散数据将剪切速度曲线约束到的最大深度,在该反演中,到底层半空间的最大深度会系统地增加。

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