用AI融合物理模型生成更真实的地震波,速度快成本低。
Integrating Fourier Neural Operators with Diffusion Models to improve Spectral Representation of Synthetic Earthquake Ground Motion Response
- 用神经算子加扩散模型生成地震波,结合物理规律与数据修正
- 频率偏差和拟合度提升,缓解了中频段能量衰减问题
- 适合地震工程模拟,尤其在无实测数据地区
核反应堆建筑需抵御强震带来的动态荷载,因此必须在多种真实地震场景(如最大可信地震)下评估其结构行为。然而,目标区域的地震目录和实测地震记录可能缺失,导致合成地震动日益重要。但现有方法面临物理机制不清晰、模型校准计算成本高昂等问题。本文提出一种基于AI的物理驱动方法:利用神经算子近似任意源-地质配置下的弹性动力学格林函数,并通过去噪扩散概率模型对生成的地震动时序进行修正。结果表明,该方法显著提升了合成地震动的频谱保真度,频率偏差和拟合度(GOF)均得到改善,有效缓解了神经算子生成序列中的中频段谱衰减现象。该方法在不同场地与震源条件下均可实现快速低成本推理。
原文摘要 · Abstract (English)
Nuclear reactor buildings must be designed to withstand the dynamic load induced by strong ground motion earthquakes. For this reason, their structural behavior must be assessed in multiple realistic ground shaking scenarios (e.g., the Maximum Credible Earthquake). However, earthquake catalogs and recorded seismograms may not always be available in the region of interest. Therefore, synthetic earthquake ground motion is progressively being employed, although with some due precautions: earthquake physics is sometimes not well enough understood to be accurately reproduced with numerical tools, and the underlying epistemic uncertainties lead to prohibitive computational costs related to model calibration. In this study, we propose an AI physics-based approach to generate synthetic ground motion, based on the combination of a neural operator that approximates the elastodynamics Green's operator in arbitrary source-geology setups, enhanced by a denoising diffusion probabilistic model. The diffusion model is trained to correct the ground motion time series generated by the neural operator. Our results show that such an approach promisingly enhances the realism of the generated synthetic seismograms, with frequency biases and Goodness-Of-Fit (GOF) scores being improved by the diffusion model. This indicates that the latter is capable to mitigate the mid-frequency spectral falloff observed in the time series generated by the neural operator. Our method showcases fast and cheap inference in different site and source conditions.
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