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海底散射和反射数据的跨维联合反演。

Trans-dimensional joint inversion of seabed scattering and reflection data.

机构信息

School of Earth and Ocean Sciences, University of Victoria, Victoria, BC V8W 3P6, Canada.

出版信息

J Acoust Soc Am. 2013 Mar;133(3):1347-57. doi: 10.1121/1.4789930.

Abstract

This paper examines joint inversion of acoustic scattering and reflection data to resolve seabed interface roughness parameters (spectral strength, exponent, and cutoff) and geoacoustic profiles. Trans-dimensional (trans-D) Bayesian sampling is applied with both the number of sediment layers and the order (zeroth or first) of auto-regressive parameters in the error model treated as unknowns. A prior distribution that allows fluid sediment layers over an elastic basement in a trans-D inversion is derived and implemented. Three cases are considered: Scattering-only inversion, joint scattering and reflection inversion, and joint inversion with the trans-D auto-regressive error model. Including reflection data improves the resolution of scattering and geoacoustic parameters. The trans-D auto-regressive model further improves scattering resolution and correctly differentiates between strongly and weakly correlated residual errors.

摘要

本文研究了声波散射和反射数据的联合反演,以解决海底界面粗糙度参数(谱强度、指数和截止)和地声剖面问题。应用了跨维(trans-D)贝叶斯抽样,将沉积物层数和误差模型中自回归参数的阶(零阶或一阶)都视为未知。推导并实现了允许在跨维反演中在弹性基底上存在流体沉积物层的先验分布。考虑了三种情况:仅散射反演、散射和反射联合反演以及具有跨维自回归误差模型的联合反演。包含反射数据可提高散射和地声参数的分辨率。跨维自回归模型进一步提高了散射分辨率,并正确地区分了强相关和弱相关的残差。

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