Episodic fluid venting from sedimentary basins fuelled by pressurised mudstones
Subsurface sandstone reservoirs sealed by overlying, low-permeability layers provide capacity for long-term sequestration of anthropogenic waste. Leakage can occur if reservoir pressures rise sufficiently to fracture the seal. Such pressures can be generated within the reservoir by vigorous injectio...
| Main Authors: | , , , , |
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| Format: | Journal article |
| Language: | English |
| Published: |
National Academy of Sciences
2024
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| _version_ | 1797112831677562880 |
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| author | Kearney, LM Katz, RF Macminn, CW Kirkham, C Cartwright, J |
| author_facet | Kearney, LM Katz, RF Macminn, CW Kirkham, C Cartwright, J |
| author_sort | Kearney, LM |
| collection | OXFORD |
| description | Subsurface sandstone reservoirs sealed by overlying, low-permeability layers provide capacity for long-term sequestration of anthropogenic waste. Leakage can occur if reservoir pressures rise sufficiently to fracture the seal. Such pressures can be generated within the reservoir by vigorous injection of waste or, over thousands of years, by natural processes. In either case, the precise role of intercalated mudstones in the long-term evolution of reservoir pressure remains unclear; these layers have variously been viewed as seals, as pressure sinks, or as pressure sources. Here, we use the geological record of episodic fluid venting in the Levant Basin to provide striking evidence for the pressure-source hypothesis. We use a Bayesian framework to combine recently published venting data, which record critical subsurface pressures since ∼2 Ma, with a stochastic model of pressure evolution to infer a pressure-recharge rate of ∼30 MPa/Myr. To explain this large rate, we quantify and compare a range of candidate mechanisms. We find that poroelastic pressure diffusion from mudstones provides the most plausible explanation for these observations, amplifying the ∼3 MPa/Myr recharge caused primarily by tectonic compression. Since pressurized mudstones are ubiquitous in sedimentary basins, pressure diffusion from mudstones is likely to promote seal failure globally. |
| first_indexed | 2024-03-07T08:29:28Z |
| format | Journal article |
| id | oxford-uuid:9eb006fa-4695-47dd-9940-ba114b3941f9 |
| institution | University of Oxford |
| language | English |
| last_indexed | 2024-03-07T08:29:28Z |
| publishDate | 2024 |
| publisher | National Academy of Sciences |
| record_format | dspace |
| spelling | oxford-uuid:9eb006fa-4695-47dd-9940-ba114b3941f92024-03-04T14:42:58ZEpisodic fluid venting from sedimentary basins fuelled by pressurised mudstonesJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:9eb006fa-4695-47dd-9940-ba114b3941f9EnglishSymplectic ElementsNational Academy of Sciences2024Kearney, LMKatz, RFMacminn, CWKirkham, CCartwright, JSubsurface sandstone reservoirs sealed by overlying, low-permeability layers provide capacity for long-term sequestration of anthropogenic waste. Leakage can occur if reservoir pressures rise sufficiently to fracture the seal. Such pressures can be generated within the reservoir by vigorous injection of waste or, over thousands of years, by natural processes. In either case, the precise role of intercalated mudstones in the long-term evolution of reservoir pressure remains unclear; these layers have variously been viewed as seals, as pressure sinks, or as pressure sources. Here, we use the geological record of episodic fluid venting in the Levant Basin to provide striking evidence for the pressure-source hypothesis. We use a Bayesian framework to combine recently published venting data, which record critical subsurface pressures since ∼2 Ma, with a stochastic model of pressure evolution to infer a pressure-recharge rate of ∼30 MPa/Myr. To explain this large rate, we quantify and compare a range of candidate mechanisms. We find that poroelastic pressure diffusion from mudstones provides the most plausible explanation for these observations, amplifying the ∼3 MPa/Myr recharge caused primarily by tectonic compression. Since pressurized mudstones are ubiquitous in sedimentary basins, pressure diffusion from mudstones is likely to promote seal failure globally. |
| spellingShingle | Kearney, LM Katz, RF Macminn, CW Kirkham, C Cartwright, J Episodic fluid venting from sedimentary basins fuelled by pressurised mudstones |
| title | Episodic fluid venting from sedimentary basins fuelled by pressurised mudstones |
| title_full | Episodic fluid venting from sedimentary basins fuelled by pressurised mudstones |
| title_fullStr | Episodic fluid venting from sedimentary basins fuelled by pressurised mudstones |
| title_full_unstemmed | Episodic fluid venting from sedimentary basins fuelled by pressurised mudstones |
| title_short | Episodic fluid venting from sedimentary basins fuelled by pressurised mudstones |
| title_sort | episodic fluid venting from sedimentary basins fuelled by pressurised mudstones |
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