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Model selection and Bayesian inference for high-resolutionseabed reflection inversion

机译:高分辨率海底反射反演的模型选择和贝叶斯推断

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This paper applies Bayesian inference, including model selection and posterior parameter inference,to inversion of seabed reflection data to resolve sediment structure at a spatial scale below the pulselength of the acoustic source. A practical approach to model selection is used, employing theBayesian information criterion to decide on the number of sediment layers needed to sufficiently fitthe data while satisfying parsimony to avoid overparametrization. Posterior parameter inference iscarried out using an efficient Metropolis—Hastings algorithm for high-dimensional models, andresults are presented as marginal-probability depth distributions for sound velocity, density, andattenuation. The approach is applied to plane-wave reflection-coefficient inversion of single-bouncedata collected on the Malta Plateau, Mediterranean Sea, which indicate complex fine structure closeto the water-sediment interface. This fine structure is resolved in the geoacoustic inversion results interms of four layers within the upper meter of sediments. The inversion results are in goodagreement with parameter estimates from a gravity core taken at the experiment site.
机译:本文将贝叶斯推断(包括模型选择和后验参数推断)应用于海床反射数据反演,以解析低于声源脉冲长度的空间尺度上的沉积物结构。使用一种实用的模型选择方法,采用贝叶斯信息准则来确定充分拟合数据所需的沉积物层数,同时满足简约性以避免过度参数化。使用高效的Metropolis-Hastings算法对高维模型进行后验参数推断,结果以声速,密度和衰减的边际概率深度分布表示。该方法适用于在马耳他马耳他高原收集的单反射数据的平面波反射系数反演,这表明靠近水-沉积物界面的复杂精细结构。这种精细的结构在沉积层上部一米内的四层地声反演结果中得到解决。反演结果与实验地点重力岩心的参数估计值吻合。

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