Abstract Description
Carbon capture and storage projects in deep reservoirs have
significant monitoring obligations associated with regulatory needs and social licence to operate. Downhole methods are becoming increasingly attractive because of their low surface footprint and ease of stakeholder engagement. When several wells are available, monitoring from VSP-based seismic methods is possible using downholeDAS fibre optics, and even lower footprint seismic methods are possible using surface orbital vibrators combined with DAS. Crosswell pressure tomography (PT) monitoring is also possible using test water injections in completions in the reservoir interval and downhole pressure gauges. Monitoring confidence is enhanced when all monitoring data can be explained with a single model or range of models, which requires joint Bayesian inversion. However, simultaneous inversion of time-lapse seismic data and PT data is generally a difficult problem involving coupled multi-physics modelling. In the CCS context, highly buoyant and thin gas plumes make the problem susceptible to effective approximations that enable decoupling of the physics, and thereby a cascaded Bayesian inversion for both seismic amplitudes and crosswell pressures. We show inversions for the Otway stage 3 CCS demonstration project using these ideas.
significant monitoring obligations associated with regulatory needs and social licence to operate. Downhole methods are becoming increasingly attractive because of their low surface footprint and ease of stakeholder engagement. When several wells are available, monitoring from VSP-based seismic methods is possible using downholeDAS fibre optics, and even lower footprint seismic methods are possible using surface orbital vibrators combined with DAS. Crosswell pressure tomography (PT) monitoring is also possible using test water injections in completions in the reservoir interval and downhole pressure gauges. Monitoring confidence is enhanced when all monitoring data can be explained with a single model or range of models, which requires joint Bayesian inversion. However, simultaneous inversion of time-lapse seismic data and PT data is generally a difficult problem involving coupled multi-physics modelling. In the CCS context, highly buoyant and thin gas plumes make the problem susceptible to effective approximations that enable decoupling of the physics, and thereby a cascaded Bayesian inversion for both seismic amplitudes and crosswell pressures. We show inversions for the Otway stage 3 CCS demonstration project using these ideas.
Speakers
Authors
Authors
Dr James Gunning - CSIRO (Vic, Australia)
