Unsecured legacy wells pose significant risks to carbon capture and storage(CCS)as they present potential leakage pathways for stored CO_(2) to return to the atmosphere.In the UK,legacy wells must be assessed for a ca...Unsecured legacy wells pose significant risks to carbon capture and storage(CCS)as they present potential leakage pathways for stored CO_(2) to return to the atmosphere.In the UK,legacy wells must be assessed for a carbon storage permit to be granted and high-risk wells require costly remediation.We use a well risk assessment scheme to evaluate the risk of wells in the Southern North Sea.We then combine our well risk assessment with investigation using the analytical tool CO2BLOCK,which relies on a gravity current model to estimate pressure and plume migration distances.We evaluate the Viking,Camelot and Poseidon projects,which plan to inject CO_(2) into the depleted reservoirs of Southern North Sea gas fields.Carbon dioxide plumes are typically several kilometers wide,and it should be possible to avoid plume migration to high-risk legacy wells.In contrast,pressure fields produced by CO_(2) injection are tens of kilometers wide and low magnitude pressure increases frequently extend beyond the bounds of storage licence areas.The pressure fields encounter hundreds of wells and in the cases of the Camelot and Poseidon projects,interact with each other.展开更多
基金supported by the Natural Environment Research Council[grant number NE/S007415/1]Shell as iCASE sponsors。
文摘Unsecured legacy wells pose significant risks to carbon capture and storage(CCS)as they present potential leakage pathways for stored CO_(2) to return to the atmosphere.In the UK,legacy wells must be assessed for a carbon storage permit to be granted and high-risk wells require costly remediation.We use a well risk assessment scheme to evaluate the risk of wells in the Southern North Sea.We then combine our well risk assessment with investigation using the analytical tool CO2BLOCK,which relies on a gravity current model to estimate pressure and plume migration distances.We evaluate the Viking,Camelot and Poseidon projects,which plan to inject CO_(2) into the depleted reservoirs of Southern North Sea gas fields.Carbon dioxide plumes are typically several kilometers wide,and it should be possible to avoid plume migration to high-risk legacy wells.In contrast,pressure fields produced by CO_(2) injection are tens of kilometers wide and low magnitude pressure increases frequently extend beyond the bounds of storage licence areas.The pressure fields encounter hundreds of wells and in the cases of the Camelot and Poseidon projects,interact with each other.
