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Phase III - Department of Mines and Petroleum

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The GJV have focussed their priorities on the detection <strong>of</strong> early failure modes in the deep subsurface (in<br />

<strong>and</strong> around the target reservoir). This is a sensible approach <strong>and</strong> to some extent, depending on the efficacy<br />

<strong>of</strong> the deep monitoring tools, reduces the requirement for exhaustive shallow or surface monitoring<br />

deployments.<br />

More specifically, the monitoring strategy is guided by the requirements <strong>of</strong> the Uncertainty Management<br />

Plan. Provided this is valid, <strong>and</strong> the highside/lowside outcomes are properly taken into account, then the<br />

overall monitoring plan is largely robust. The major containment risks appear to have been satisfactorily<br />

identified <strong>and</strong> the strategy <strong>of</strong> time-lapse 3D/2D surface seismic, observation wells <strong>and</strong> soil gas<br />

measurements is, in principle, well suited to deal with these risks.<br />

Figure 12 Output from the International Energy Association Greenhouse Gas R&D Programme (IEAGHG) monitoring<br />

selection tool for a simplified Barrow Isl<strong>and</strong> (onshore) scenario with ‘basic’ filter. The tools that would normally be<br />

considered essential are highlighted in red.<br />

Time-lapse surface seismic is identified as the key monitoring tool. Its capability is, however, constrained<br />

by the very variable seismic data quality so far obtained across Barrow Isl<strong>and</strong> <strong>and</strong> the stringent l<strong>and</strong>-use<br />

restrictions imposed on surface activities. A major project risk therefore is the significant possibility that<br />

3D surface seismic may not be able to satisfactorily image the CO 2 plume everywhere. The GJV have<br />

evaluated the main seismic quality parameters <strong>and</strong> a limited seismic pilot study has been carried out to<br />

further optimise the baseline 3D survey <strong>and</strong> assess repeatability. This is commendable but spatial coverage<br />

<strong>of</strong> such a test is limited. It is recommended that the report on the seismic pilot study <strong>and</strong> final specification<br />

for the 3D seismic survey be reviewed in the <strong>Phase</strong> IV assessment.<br />

The GJV has followed a thorough process in identifying the most suitable technologies <strong>and</strong> completion<br />

geometries for monitoring saturation <strong>and</strong> pressure changes in both CO 2 injection wells <strong>and</strong> observation<br />

(surveillance) wells. Clear, well defined objectives for each monitoring variable (pressure, temperature,<br />

saturation, fluid sampling, etc.) have been documented. These objectives have been reflected in the<br />

Uncertainty Management Plan with initial “signposts” or indicators <strong>of</strong> lowside <strong>and</strong> highside project<br />

outcomes identified. These signposts are based on early simulation results <strong>and</strong> will need to be revisited in<br />

light <strong>of</strong> the most recent project study findings (i.e., dynamic simulation model, geomechanics, geochemical<br />

<strong>and</strong> injectivity reports) to ensure they remain reasonable indicators for the implementation <strong>of</strong> mitigation<br />

plans. The monitoring <strong>of</strong> saturation <strong>and</strong> pressure changes in the observation <strong>and</strong> injection wells will help<br />

calibrate the seismic data <strong>and</strong> the integration <strong>of</strong> the seismic <strong>and</strong> well logging datasets will clearly be<br />

beneficial.<br />

xxxv

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