History Matching for Geological Carbon Storage using Data-Space Inversion with Spatio-Temporal Data Parameterization

TL;DR

This paper introduces a deep-learning-based data-space inversion method for history matching in geological carbon storage, enabling efficient uncertainty reduction and posterior prediction of pressure and saturation fields using Bayesian data assimilation.

Contribution

It develops a novel spatio-temporal parameterization with adversarial autoencoders and convLSTM networks within a DSI framework, improving efficiency and accuracy over traditional methods.

Findings

Significant uncertainty reduction in pressure and saturation fields.

Efficient posterior predictions across multiple geological scenarios.

Effective use of deep learning for high-dimensional data parameterization.

Abstract

History matching based on monitoring data will enable uncertainty reduction, and thus improved aquifer management, in industrial-scale carbon storage operations. In traditional model-based data assimilation, geomodel parameters are modified to force agreement between flow simulation results and observations. In data-space inversion (DSI), history-matched quantities of interest, e.g., posterior pressure and saturation fields conditioned to observations, are inferred directly, without constructing posterior geomodels. This is accomplished efficiently using a set of O(1000) prior simulation results, data parameterization, and posterior sampling within a Bayesian setting. In this study, we develop and implement (in DSI) a deep-learning-based parameterization to represent spatio-temporal pressure and CO2 saturation fields at a set of time steps. The new parameterization uses an adversarial autoencoder (AAE) for dimension reduction and a convolutional long short-term memory (convLSTM) network to represent the spatial distribution and temporal evolution of the pressure and saturation fields. This parameterization is used with an ensemble smoother with multiple data assimilation (ESMDA) in the DSI framework to enable posterior predictions. A realistic 3D system characterized by prior geological realizations drawn from a range of geological scenarios is considered. A local grid refinement procedure is introduced to estimate the error covariance term that appears in the history matching formulation. Extensive history matching results are presented for various quantities, for multiple synthetic true models. Substantial uncertainty reduction in posterior pressure and saturation fields is achieved in all cases. The framework is applied to efficiently provide posterior predictions for a range of error covariance specifications. Such an assessment would be expensive using a model-based approach.