数据与物理联合驱动的叠前AVA弹性参数反演

IF 3 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Geophysics Pub Date : 2023-10-10 DOI:10.1190/geo2023-0135.1
Shuliang Wu, Yingying Wang, Qingping Li, Zhiliang He, Jianhua Geng
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引用次数: 0

摘要

纵波、横波速度和密度等弹性参数对地下定量解释和储层预测具有重要意义。目前叠前振幅与角度(AVA)反演方法已在工业上广泛应用于获取地下弹性参数。传统的AVA反演方法在理论上是基于线性化的物理模型,该模型描述了叠前地震反射系数与地下模型弹性参数之间的关系,称为物理模型驱动反演。然而,线性化的物理模型导致反演结果精度低,不确定性大。近年来,为了解决这一问题,开发了几种基于神经网络的叠前AVA反演方法,称为数据驱动反演。但是这些方法通常需要大量的标记数据来训练网络,并且这个过程没有明确的物理机制。因此,数据驱动的反演结果缺乏物理可解释性。为了解决这些问题,提出了一种数据和物理驱动的叠前AVA弹性参数联合反演方法。在半监督学习的框架下,利用二维卷积神经网络和递归神经网络建立相邻叠前AVA聚类与一维弹性参数在时域上的映射关系。将完整的Zoeppritz方程作为神经网络的物理模型约束,并使用测井数据和叠前AVA地震数据构建损失函数。该方法可以使用小标记数据进行训练网络,提高了反演过程的物理可解释性。提出了地震资料距离逆加权相关系数,对地震资料和测井资料的损失函数进行加权。综合和现场数据实例表明,数据驱动和物理驱动的叠前AVA弹性参数反演方法提高了反演精度和分辨率,并对反演结果的不确定性进行了估计。
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Joint Data- and Physics-driven Pre-stack AVA Elastic Parameters Inversion
Elastic parameters such as P- and S-wave velocity and density are of great significance for subsurface quantitative interpretation and reservoir prediction. Current pre-stack amplitude-versus-angle (AVA) inversion methods have been widely used in industry to obtain subsurface elastic parameters. Conventional AVA inversion methods are theoretically based on a linearized physical model formulating the relationship between pre-stack seismic reflection coefficients and subsurface model elastic parameters, called physical model-driven inversion. However, the linearized physical models lead to low accuracy and high uncertainty of inversion results. In recent years, several neural network-based pre-stack AVA inversion methods, called data-driven inversion, have been developed to address this issue. But these methods typically require a large amount of labeled data for training network, and the process does not have a clear physical mechanism. So the data-driven inversion results lack physical interpretability. To address these issues, a joint data- and physics-driven inversion of pre-stack AVA elastic parameters is proposed. Under the framework of semi-supervised learning, a two-dimensional convolutional neural network and a recurrent neural network are used to establish the mapping between several adjacent pre-stack AVA gathers and one-dimensional elastic parameters in time domain. The full Zoeppritz equation is used as a physical model constraint to the neural network, and loss functions are constructed using both well-logging data and pre-stack AVA seismic data. This approach can perform training network using small labeled data and increase physical interpretability of the inversion process. The inverse distance weighted correlation coefficient of seismic data is proposed to weight the loss function of seismic data and well-logging data. Synthetic and field data examples show that the joint data- and physics-driven pre-stack AVA elastic parameters inversion improves the accuracy and resolution, and provides an estimation of uncertainty of the inversion results.
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来源期刊
Geophysics
Geophysics 地学-地球化学与地球物理
CiteScore
6.90
自引率
18.20%
发文量
354
审稿时长
3 months
期刊介绍: Geophysics, published by the Society of Exploration Geophysicists since 1936, is an archival journal encompassing all aspects of research, exploration, and education in applied geophysics. Geophysics articles, generally more than 275 per year in six issues, cover the entire spectrum of geophysical methods, including seismology, potential fields, electromagnetics, and borehole measurements. Geophysics, a bimonthly, provides theoretical and mathematical tools needed to reproduce depicted work, encouraging further development and research. Geophysics papers, drawn from industry and academia, undergo a rigorous peer-review process to validate the described methods and conclusions and ensure the highest editorial and production quality. Geophysics editors strongly encourage the use of real data, including actual case histories, to highlight current technology and tutorials to stimulate ideas. Some issues feature a section of solicited papers on a particular subject of current interest. Recent special sections focused on seismic anisotropy, subsalt exploration and development, and microseismic monitoring. The PDF format of each Geophysics paper is the official version of record.
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