Matches in SemOpenAlex for { <https://semopenalex.org/work/W2034345208> ?p ?o ?g. }
- W2034345208 endingPage "72" @default.
- W2034345208 startingPage "56" @default.
- W2034345208 abstract "CO2 geo-sequestration process in deep saline aquifers has recently attracted attention as it addresses one of the current global issues of climate change. Suitable saline aquifers for CO2 storage are generally located very deep underground, where the aquifer’s pore fluid is highly saline. The strength of the reservoir rock mass is important to ensure safe sequestration, it is essential to check the aquifer rock mass strength in this highly saline environment. Although the Mohr–Coulomb failure criterion is widely used for many geotechnical engineering applications, its applicability to brine-saturated sedimentary rocks or saline aquifers has not been confirmed to date. This study therefore identifies the brine saturation effect on the stress–strain behaviour of saline aquifer reservoir rock (sandstone) under in-situ stress conditions, to check and if necessary modify the conventional Mohr–Coulomb failure criterion to capture the brine saturation effect on reservoir’s rock strength parameters. A series of tri-axial experiments was conducted on Hawkesbury sandstone samples, obtained from the Sydney basin, for a range of confining pressures (5–20 MPa) and brine saturation conditions (0%, 10%, 20% and 30% NaCl concentrations) at 25 °C constant temperature. According to the experimental results, the presence of NaCl in pore fluid causes the reservoir rock strength and shear parameters (friction angle and cohesion) to be increased in deep saline aquifers, and this effect increases with increasing brine concentration in the pore fluid. In addition, the presence of brine causes the dilatancy strength of saline aquifer rocks to be enhanced and the post-peak dilation (at which macroscopic shear faults may occur in the rock mass) of saline aquifer rock mass to be reduced. These enhance the micro-fracturing resistivity of the rock mass and increase the rock mass stability, both of which are favourable for the long-term integrity of the CO2 sequestration process in deep saline aquifers. In addition, the conventional linear Mohr–Coulomb failure criterion fails to simulate the measured stress–strain data of brine-saturated Hawkesbury sandstone. This can be precisely corrected using the modified failure criterion proposed in this study." @default.
- W2034345208 created "2016-06-24" @default.
- W2034345208 creator A5010619554 @default.
- W2034345208 creator A5023467994 @default.
- W2034345208 creator A5034564163 @default.
- W2034345208 creator A5049425101 @default.
- W2034345208 creator A5053961001 @default.
- W2034345208 date "2015-07-01" @default.
- W2034345208 modified "2023-09-25" @default.
- W2034345208 title "Non-linear stress–strain behaviour of reservoir rock under brine saturation: An experimental study" @default.
- W2034345208 cites W1563560881 @default.
- W2034345208 cites W1940002748 @default.
- W2034345208 cites W1965088949 @default.
- W2034345208 cites W1965655096 @default.
- W2034345208 cites W1969231330 @default.
- W2034345208 cites W1970301285 @default.
- W2034345208 cites W1982589147 @default.
- W2034345208 cites W2002050348 @default.
- W2034345208 cites W2003311804 @default.
- W2034345208 cites W2003947356 @default.
- W2034345208 cites W2007995374 @default.
- W2034345208 cites W2011896412 @default.
- W2034345208 cites W2025094360 @default.
- W2034345208 cites W2026203425 @default.
- W2034345208 cites W2030731130 @default.
- W2034345208 cites W2032009370 @default.
- W2034345208 cites W2037310459 @default.
- W2034345208 cites W2041567358 @default.
- W2034345208 cites W2042241092 @default.
- W2034345208 cites W2043865069 @default.
- W2034345208 cites W2044176438 @default.
- W2034345208 cites W2054667848 @default.
- W2034345208 cites W2057322819 @default.
- W2034345208 cites W2058059973 @default.
- W2034345208 cites W2063680241 @default.
- W2034345208 cites W2066120714 @default.
- W2034345208 cites W2067706890 @default.
- W2034345208 cites W2069320785 @default.
- W2034345208 cites W2076526095 @default.
- W2034345208 cites W2083055255 @default.
- W2034345208 cites W2086927025 @default.
- W2034345208 cites W2097471771 @default.
- W2034345208 cites W2111699946 @default.
- W2034345208 cites W2154053511 @default.
- W2034345208 cites W2166192443 @default.
- W2034345208 cites W4240111140 @default.
- W2034345208 cites W4242876594 @default.
- W2034345208 cites W61328401 @default.
- W2034345208 doi "https://doi.org/10.1016/j.measurement.2015.04.011" @default.
- W2034345208 hasPublicationYear "2015" @default.
- W2034345208 type Work @default.
- W2034345208 sameAs 2034345208 @default.
- W2034345208 citedByCount "21" @default.
- W2034345208 countsByYear W20343452082016 @default.
- W2034345208 countsByYear W20343452082017 @default.
- W2034345208 countsByYear W20343452082018 @default.
- W2034345208 countsByYear W20343452082019 @default.
- W2034345208 countsByYear W20343452082020 @default.
- W2034345208 countsByYear W20343452082021 @default.
- W2034345208 countsByYear W20343452082022 @default.
- W2034345208 countsByYear W20343452082023 @default.
- W2034345208 crossrefType "journal-article" @default.
- W2034345208 hasAuthorship W2034345208A5010619554 @default.
- W2034345208 hasAuthorship W2034345208A5023467994 @default.
- W2034345208 hasAuthorship W2034345208A5034564163 @default.
- W2034345208 hasAuthorship W2034345208A5049425101 @default.
- W2034345208 hasAuthorship W2034345208A5053961001 @default.
- W2034345208 hasConcept C114614502 @default.
- W2034345208 hasConcept C121332964 @default.
- W2034345208 hasConcept C127313418 @default.
- W2034345208 hasConcept C187320778 @default.
- W2034345208 hasConcept C2776957854 @default.
- W2034345208 hasConcept C33923547 @default.
- W2034345208 hasConcept C41242791 @default.
- W2034345208 hasConcept C75622301 @default.
- W2034345208 hasConcept C76177295 @default.
- W2034345208 hasConcept C78762247 @default.
- W2034345208 hasConcept C97355855 @default.
- W2034345208 hasConcept C9930424 @default.
- W2034345208 hasConceptScore W2034345208C114614502 @default.
- W2034345208 hasConceptScore W2034345208C121332964 @default.
- W2034345208 hasConceptScore W2034345208C127313418 @default.
- W2034345208 hasConceptScore W2034345208C187320778 @default.
- W2034345208 hasConceptScore W2034345208C2776957854 @default.
- W2034345208 hasConceptScore W2034345208C33923547 @default.
- W2034345208 hasConceptScore W2034345208C41242791 @default.
- W2034345208 hasConceptScore W2034345208C75622301 @default.
- W2034345208 hasConceptScore W2034345208C76177295 @default.
- W2034345208 hasConceptScore W2034345208C78762247 @default.
- W2034345208 hasConceptScore W2034345208C97355855 @default.
- W2034345208 hasConceptScore W2034345208C9930424 @default.
- W2034345208 hasLocation W20343452081 @default.
- W2034345208 hasOpenAccess W2034345208 @default.
- W2034345208 hasPrimaryLocation W20343452081 @default.
- W2034345208 hasRelatedWork W2002673683 @default.
- W2034345208 hasRelatedWork W2042920199 @default.
- W2034345208 hasRelatedWork W2077982178 @default.
- W2034345208 hasRelatedWork W2363350442 @default.