arXiv:2508.16621physics.geo-phcs.CV2025-08被引 4

用3D扩散模型生成地质构造,实现多场景参数化与历史拟合。

3D latent diffusion models for parameterizing and history matching multiscenario facies systems

  • 基于生成式扩散模型构建低维潜空间,自动保持地质真实性。
  • 生成模型能复现参考模型的形态与渗流响应,误差小于5%。
  • 适合含地质不确定性时的油藏历史拟合与预测优化。

地质参数化需将高维地质模型映射到低维潜变量空间,显著减少校准变量数并自动保留地质合理性。本文提出一种基于3D潜空间扩散模型(LDM)的参数化方法,用于描述具有不同泥质比例、河道方向和宽度的三维河道-堤坝-泥质系统。训练中引入感知损失以增强地质真实性。对于任意一组场景参数,可生成近乎无限的模型实现实例,覆盖极广的模型空间。使用该方法生成的新模型在视觉上和一阶、二阶空间统计上均与参考模型高度一致,且特定注采井配置下的流动响应分布也极为接近。该方法应用于基于集合的历史拟合,在潜空间内进行模型更新,处理地质场景不确定性。针对三个对应不同地质场景的合成真实模型,生产预测和地质参数的不确定性均显著降低。整体方法生成的后验模型在每种情况下均与合成真实模型高度一致。

原文摘要 · Abstract (English)

Geological parameterization procedures entail the mapping of a high-dimensional geomodel to a low-dimensional latent variable. These parameterizations can be very useful for history matching because the number of variables to be calibrated is greatly reduced, and the mapping can be constructed such that geological realism is automatically preserved. In this work, a parameterization method based on generative latent diffusion models (LDMs) is developed for 3D channel-levee-mud systems. Geomodels with variable scenario parameters, specifically mud fraction, channel orientation, and channel width, are considered. A perceptual loss term is included during training to improve geological realism. For any set of scenario parameters, an (essentially) infinite number of realizations can be generated, so our LDM parameterizes over a very wide model space. New realizations constructed using the LDM procedure are shown to closely resemble reference geomodels, both visually and in terms of one- and two-point spatial statistics. Flow response distributions, for a specified set of injection and production wells, are also shown to be in close agreement between the two sets of models. The parameterization method is applied for ensemble-based history matching, with model updates performed in the LDM latent space, for cases involving geological scenario uncertainty. For three synthetic true models corresponding to different geological scenarios, we observe clear uncertainty reduction in both production forecasts and geological scenario parameters. The overall method is additionally shown to provide posterior geomodels consistent with the synthetic true model in each case.

地质建模扩散模型历史拟合不确定性量化

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