Mrinal Sinha

and 3 more

Carbon capture and storage (CCS) is forecast to play a significant role towards CO2 emissions reduction. Cost-effective and simplified monitoring will be essential for rapid adoption and growth of CCS. Seismic imaging methods are regularly utilized to monitor low-velocity anomalies generated by injection of CO2 in the subsurface. In this study we generate active and passive synthetic seismic datasets at different stages of CO2 injection in the subsurface based on geologically constrained subsurface models of the Pelican storage site in the Gippsland Basin, Australia. We apply full waveform inversion (FWI) and wave-equation dispersion (WD) inversion to seafloor deployed distributed acoustic sensing (DAS) data to reconstruct the low-velocity anomalies. We model both strain (DAS) and displacement datasets for the active data component of the study and show that they result in similar reconstruction of the CO2 anomaly. FWI based time-lapse imaging of active data yields the most accurate results. However, this approach is expensive and also suffers from complex issues because of the near-onshore location of the storage site. Alternatively inverting passive data results in only minor differences, but can still effectively monitor changes in the subsurface, and assist in monitoring the CO2 plume at the reservoir depth. Furthermore, we demonstrate the capability of WD for inverting Scholte-waves derived from ambient noise for shallow detection of CO2 in the unlikely event of a leakage. Therefore, we propose a mixed mode monitoring strategy where passive data is utilised for routine monitoring while active surveys are deployed only when further investigation is required.
Permanent reservoir surveillance is an invaluable monitoring tool for CO2 storage projects, as it tracks spatial-temporal evolution of the gas plume. The frequent images of CO2 plumes will facilitate history-matching of the reservoir simulations and increase confidence of early leakage detection. However, continuous data acquisition and real-time interpretation require a new approach to data analysis. Here we propose a data-driven approach to forecasting future time-lapse seismic images based on the observed past images and test this approach on the Otway Stage 2C data. The core component of the predictor is a convolutional neural network, which considers subsequent plume maps as colour layers, similarly to standard red-green-blue blending. Based on the spatial distribution of these ‘colours’ we may predict the future contour of the seismically visible part of the plume. The neural networks absorb the physics of CO2 migration through training on reservoir simulations for a wide range of injection scenarios and subsurface models. Extensive testing shows that realistic plumes for Stage 2C are too complicated and the neural network should be pre-trained on simpler reservoir simulations that include only one or two geological features, such as: faults, spill-points. Such staged training enables a gradual descent of the neural network optimization to a global minimum. In an upshot, the proposed algorithms are proven accurate. The approach is practical, because each CO2 storage project requires extensive pre-injection reservoir simulations. Once the predictor has been trained, it forecasts plume evolution almost instantly and quickly adapts to changing dynamics of the CO2 migration.