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    基于一维到二维膨胀卷积核的半监督地震波阻抗反演

    Semi-supervised seismic impedance inversion based on 1D-to-2D dilated convolution kernels

    • 摘要: 深度学习方法被广泛应用于地震反演领域,半监督框架有效克服了反演过程中井数据有限的瓶颈。常规一维半监督反演方法逐道对地震数据进行处理,忽略了相邻地震道之间的空间关系,需添加初始模型补充低频信息,二维半监督方法需要大量标注的地震数据进行训练,数据获取成本高,标注质量难以保证。为充分利用有限的测井数据,并减少对大规模标注数据集的依赖,提出了一种基于一维到二维膨胀卷积核的半监督地震波阻抗反演框架。首先利用测井数据与地震数据预训练一维卷积神经网络,学习波阻抗的时域特征表示;随后通过物理约束的卷积核膨胀,将其扩展为二维卷积核,实现跨维度特征迁移,并在目标区少量二维标注数据上进行监督微调,以融合井位信息与无标注地震数据。为保证迁移的物理合理性与稳定性,设计了空间感知的权重分布和渐进式训练策略。合成数据实验与实际工区应用结果表明,该方法在保持井点一致性的同时,能够获得较高的反演精度和良好的空间连续性,在少井条件下表现出较好的稳定性与工程应用潜力。

       

      Abstract: Deep learning methods have been extensively applied in seismic inversion, and semi-supervised frameworks effectively overcome the bottleneck of limited log data. Conventional 1D semi-supervised inversion approaches process seismic data trace by trace, neglecting spatial correlations between adjacent traces and often requiring an initial model to compensate for missing low-frequency information. In contrast, 2D methods rely on large amounts of labeled seismic data for training, which is restricted by the high cost of data acquisition and the difficulty of ensuring labeling quality. To make full use of limited log data and reduce dependence on large-scale labeled datasets, this study proposes a semi-supervised seismic impedance inversion framework based on 1D-to-2D dilated convolution kernels. The method first pre-trains a 1D convolutional neural network using log and seismic data to learn temporal feature representations of impedance. Subsequently, through physics-constrained kernel dilation, the network is expanded into a 2D form to enable cross-dimensional feature transfer. Supervised fine-tuning is then performed on sparse 2D labeled data from the target area to integrate well-log information with unlabeled seismic data. To ensure the physical plausibility and stability of the transfer, this study designs a spatially aware weight distribution and a progressive training strategy. Experimental results on synthetic and field data demonstrate that the proposed method maintains consistency at well sites and achieves high inversion accuracy and good spatial continuity. It exhibits strong stability and engineering application potential with limited log data.

       

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