用扩散模型解决碳捕集地下流体建模难题,显著提升稀疏数据下的精度与效率。
Function-Space Decoupled Diffusion for Forward and Inverse Modeling in Carbon Capture and Storage
- 分域扩散框架分离参数与动态场建模,先学地质先验再用神经算子引导物理一致性
- 仅25%观测数据下误差仅7.7%,较传统方法提升11倍,突破数据稀疏瓶颈
- 首次验证扩散逆解法有效性,生成结果物理合理且采样效率提升4倍
准确刻画地下流体对碳捕集与封存(CCS)至关重要,但受制于观测稀疏导致的逆问题不适定性。本文提出函数空间解耦扩散后验采样(Fun-DDPS)框架,结合函数空间扩散模型与可微神经算子代理模型,实现前向与逆向建模。该方法使用单通道扩散模型学习地质参数先验(geomodel),再通过局部神经算子(LNO)代理模型提供跨场动力学条件的物理一致性引导。这种解耦设计使扩散先验能稳健恢复参数空间缺失信息,而代理模型则高效提供梯度引导用于数据同化。在合成的CCS建模数据集上验证:(1)仅25%观测时,Fun-DDPS相对误差为7.7%,远低于标准代理模型的86.9%(提升11倍),证明其在极端数据稀疏下的鲁棒性;(2)首次严格对比扩散基逆解器与渐近精确拒绝采样(RS)后验。Fun-DDPS与联合状态基线(Fun-DPS)均达到小于0.06的Jensen-Shannon散度,且前者生成结果无高频伪影,样本效率较拒绝采样提高4倍。
原文摘要 · Abstract (English)
Accurate characterization of subsurface flow is critical for Carbon Capture and Storage (CCS) but remains challenged by the ill-posed nature of inverse problems with sparse observations. We present Function-space Decoupled Diffusion Posterior Sampling (Fun-DDPS), a generative framework that combines function-space diffusion models with differentiable neural operator surrogates for both forward and inverse modeling. Our approach learns a prior distribution over geological parameters (geomodel) using a single-channel diffusion model, then leverages a Local Neural Operator (LNO) surrogate to provide physics-consistent guidance for cross-field conditioning on the dynamics field. This decoupling allows the diffusion prior to robustly recover missing information in parameter space, while the surrogate provides efficient gradient-based guidance for data assimilation. We demonstrate Fun-DDPS on synthetic CCS modeling datasets, achieving two key results: (1) For forward modeling with only 25% observations, Fun-DDPS achieves 7.7% relative error compared to 86.9% for standard surrogates (an 11x improvement), proving its capability to handle extreme data sparsity where deterministic methods fail. (2) We provide the first rigorous validation of diffusion-based inverse solvers against asymptotically exact Rejection Sampling (RS) posteriors. Both Fun-DDPS and the joint-state baseline (Fun-DPS) achieve Jensen-Shannon divergence less than 0.06 against the ground truth. Crucially, Fun-DDPS produces physically consistent realizations free from the high-frequency artifacts observed in joint-state baselines, achieving this with 4x improved sample efficiency compared to rejection sampling.
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