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arXiv 2510.17876physics.geo-phcs.LG
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利用隐式神经表示和科学机器学习进行三维重力数据反演

Three-dimensional inversion of gravity data using implicit neural representations and scientific machine learning

Geological Survey of Finland(芬兰地质调查局);Indian Institute of Technology Bombay(印度理工学院孟买分校)

Pankaj K Mishra, Sanni Laaksonen, Jochen Kamm, Anand Singh

AI总结:

本文提出一种基于隐式神经表示的三维重力反演方法,通过物理正演模型损失直接训练深度神经网络,实现连续密度场的反演,无需预定义网格或离散化,提升对地质结构的重建能力。

摘要:

重力数据反演是研究地下密度变化的重要方法,涉及矿产勘探、地热评估、碳储存、天然氢、地下水资源和构造演化。本文提出一种科学机器学习方法,利用隐式神经表示(INR)将地下密度表示为连续场。该方法通过物理正演模型损失直接训练深度神经网络,将空间坐标映射到连续密度场,无需预定义网格或离散化。空间编码增强了网络捕捉尖锐对比和短波长特征的能力,克服了传统坐标基网络因频谱偏倚导致的过度平滑问题。本文在合成示例中验证了该方法,包括平滑模型和倾斜块模型,以评估不同深度结构的恢复能力。INR框架在不使用显式正则化或深度加权的情况下重建了详细的结构和地质合理的边界,同时随着问题规模增大,减少了反演参数数量。这些结果展示了隐式表示在实现可扩展、灵活和可解释的大规模地球物理反演中的潜力。该框架可推广到其他地球物理方法及联合/多物理场反演。

英文摘要:

Inversion of gravity data is an important method for investigating subsurface density variations relevant to mineral exploration, geothermal assessment, carbon storage, natural hydrogen, groundwater resources, and tectonic evolution. Here we present a scientific machine-learning approach for three-dimensional gravity inversion that represents subsurface density as a continuous field using an implicit neural representation (INR). The method trains a deep neural network directly through a physics-based forward-model loss, mapping spatial coordinates to a continuous density field without predefined meshes or discretisation. Spatial encoding enhances the network's capacity to capture sharp contrasts and short-wavelength features that conventional coordinate-based networks tend to oversmooth due to spectral bias. We demonstrate the approach on synthetic examples including smooth models, representing realistic geological complexity, and a dipping block model to assess recovery of structures at different depths. The INR framework reconstructs detailed structure and geologically plausible boundaries without explicit regularisation or depth weighting, while reducing the number of inversion parameters as the problem size grows bigger. These results highlight the potential of implicit representations to enable scalable, flexible, and interpretable large-scale geophysical inversion. This framework could generalise to other geophysical methods and for joint/multiphysics inversion.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

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