贝叶斯全波形反演的物理结构变量推理

IF 3.9 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS
Xuebin Zhao, Andrew Curtis
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引用次数: 0

摘要

全波形反演(FWI)可根据地震波形数据创建地球地下结构的高分辨率模型。由于全波形反演问题的非线性和非唯一性,找到全局最佳拟合模型解并不一定是可取的,因为它们既能拟合数据中的噪声,也能拟合所需的信号。贝叶斯 FWI 计算所谓的后验概率分布函数,它描述了所有可能的模型解及其不确定性。在本文中,我们使用变分推理来解决贝叶斯 FWI 问题,并提出了一种称为物理结构变分推理的新方法。在一个简单的例子中,我们根据成像反演问题中的先验信息,将空间位置对之间的参数相关性包含在一个主波长范围内,并将其他相关性设为零。这使得该方法在内存要求和计算量方面都比其他变分法高效得多,但代价是所找到的解决方案在一定程度上失去了通用性。我们用二维声学 FWI 场景演示了所提出的方法,并将结果与使用其他方法得到的结果进行了比较。这验证了该方法可以生成有关后验分布的准确统计信息,同时大大提高了效率(在我们的 FWI 例子中,计算量减少了 1 个数量级)。我们进一步证明,尽管解决方案的通用性可能会降低,但后验不确定性可用于解决与估算地下储层和储存的 CO2${text{CO}}_{2}$ 体积相关的后验问题,并将偏差降至最低,从而创建一个基于 FWI 的高效决策工作流程。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Physically Structured Variational Inference for Bayesian Full Waveform Inversion

Physically Structured Variational Inference for Bayesian Full Waveform Inversion

Full waveform inversion (FWI) creates high resolution models of the Earth's subsurface structures from seismic waveform data. Due to the non-linearity and non-uniqueness of FWI problems, finding globally best-fitting model solutions is not necessarily desirable since they fit noise as well as the desired signal in data. Bayesian FWI calculates a so-called posterior probability distribution function, which describes all possible model solutions and their uncertainties. In this paper, we solve Bayesian FWI using variational inference, and propose a new methodology called physically structured variational inference, in which a physics-based structure is imposed on the variational distribution. In a simple example motivated by prior information from imaging inverse problems, we include parameter correlations between pairs of spatial locations within a dominant wavelength of each other, and set other correlations to zero. This makes the method far more efficient compared to other variational methods in terms of both memory requirements and computation, at the cost of some loss of generality in the solution found. We demonstrate the proposed method with a 2D acoustic FWI scenario, and compare the results with those obtained using other methods. This verifies that the method can produce accurate statistical information about the posterior distribution with hugely improved efficiency (in our FWI example, 1 order of magnitude reduction in computation). We further demonstrate that despite the possible reduction in generality of the solution, the posterior uncertainties can be used to solve post-inversion interrogation problems connected to estimating volumes of subsurface reservoirs and of stored CO 2 ${\text{CO}}_{2}$ , with minimal bias, creating a highly efficient FWI-based decision-making workflow.

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来源期刊
Journal of Geophysical Research: Solid Earth
Journal of Geophysical Research: Solid Earth Earth and Planetary Sciences-Geophysics
CiteScore
7.50
自引率
15.40%
发文量
559
期刊介绍: The Journal of Geophysical Research: Solid Earth serves as the premier publication for the breadth of solid Earth geophysics including (in alphabetical order): electromagnetic methods; exploration geophysics; geodesy and gravity; geodynamics, rheology, and plate kinematics; geomagnetism and paleomagnetism; hydrogeophysics; Instruments, techniques, and models; solid Earth interactions with the cryosphere, atmosphere, oceans, and climate; marine geology and geophysics; natural and anthropogenic hazards; near surface geophysics; petrology, geochemistry, and mineralogy; planet Earth physics and chemistry; rock mechanics and deformation; seismology; tectonophysics; and volcanology. JGR: Solid Earth has long distinguished itself as the venue for publication of Research Articles backed solidly by data and as well as presenting theoretical and numerical developments with broad applications. Research Articles published in JGR: Solid Earth have had long-term impacts in their fields. JGR: Solid Earth provides a venue for special issues and special themes based on conferences, workshops, and community initiatives. JGR: Solid Earth also publishes Commentaries on research and emerging trends in the field; these are commissioned by the editors, and suggestion are welcome.
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