Photo: www.equinor.com.
Europe
Subsurface Storage

How can we monitor North Sea carbon stores under wind farms and production platforms?

The UK North Sea is now a multi-energy basin, with carbon capture and storage (CCS), offshore wind, and oil and gas facilities increasingly competing for geographical and seafloor space

Repeat time-lapse seismic surveys can track CO2 plume migration, but where the seabed is obstructed by wind turbines or oil and gas platforms, access by ves­sels towing long multi-streamer arrays is impractical.

Research in the Centre for Energy Transition, part of the University of Aberdeen’s Interdisciplinary Institute, has sought solutions allowing wind and carbon storage pro­jects to co-exist. Sponsored by The Crown Estate (TCE) and Crown Estate Scotland (CES), Project Colocate fo­cused on areas of potential cross-sector overlap in the Out­er Moray Firth (OMF) and East Irish Sea (EIS), reviewing the operational and depth limitations of alternative mon­itoring technologies and the adaptation of Measurement, Monitoring and Verification (MMV) plans to specific store characteristics.

For example, gravity monitoring may offer partial as­surance in an area of wind farm and CCS overlap at More­cambe Net Zero (EIS; Sherwood Sandstone reservoir, 700-1,100 m), but exponential decay of signals with depth sees gravity as unsuitable for the deeper Cretaceous Captain and Cenozoic Mey sandstone reservoirs at 2,200-2,500 m in the Acorn and East Mey stores of the OMF. Similarly, microseismic surveys may identify and locate seal failures but cannot adequately image CO2 migration in typical reservoirs.

Amongst alternative seismic methods, single-source (‘spot’) seismic has allowed point calibrations for the South­ern North Sea Poseidon project, but recent modelling at Acorn shows that aquifer displacement following CO2 injec­tion should be imageable across the wider store, with repeat time-lapse 3D (4D) seismic coverage therefore preferred.

Smaller vessels towing short streamers are more manoeu­vrable but offer limited imaging below 1 km, while access to may still present collision risks. High-density Ocean Bottom Node (OBN) seismic is expensive, and sparse OBN lacks the short offsets needed for accurate shallow velocity fields. Prom­ising tests of fibre-optic seafloor arrays (DAS, Distributed Acoustic Sensing) at Norway’s Johan Sverdrup oilfield, now support future application to MMV, but the technology is as yet immature.

Effective investigation range of CCS MMV technologies, showing depth comparison of the OMF Acorn and East Mey CCS stores with Morecambe, Sleipner and Johan Sverdrup.

Adapting workflows tested by Equinor at Sleipner in Nor­way, our study proposes a hybrid solution with short stream­er seismic acquired prior to construction, complemented by initial baseline and later time-lapse sparse OBN.

Processing these datasets together through Full Waveform Inversion captures both long and short offsets. Re-using the short streamer data assures shallow velocities, with reservoir fluid changes at depth then imaged via merged repeat sparse OBN, which can be acquired with obstructions in place.

Project Colocate highlights the technical and commercial compromises arising from the co-location of CCS with offshore wind and oil and gas, concluding that coordinated multi-sec­tor licensing should avoid creating new co-location scenarios wherever possible. Nevertheless, a bespoke and hybrid MMV approach, combining short streamer data with time-lapse sparse OBN, may offer a solution for carbon stores where wind farms or other obstructions are already built or planned.

Previous article
It doesn’t need to be clay mineral diagenesis

Related Articles