FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4313443205> ?p ?o ?g. }

• W4313443205 endingPage "129029" @default.
• W4313443205 startingPage "129029" @default.
• W4313443205 abstract "Investigating the porosity–permeability evolution in carbonate rocks during long-term infiltration is a challenging hydrodynamic problem in rock engineering (hydroelectric engineering, CO2 geological storage, and oil/gas development). In general, we consider the evolution of porosity and permeability to be positively correlated. However, the complex pore structures in carbonate rocks include multiscale pore-fracture structures, such as intergranular pores, dissolution pores, and even fractures. Although the permeability levels of carbonate rocks are similar, the evolution of the pore structure is highly variable. Here, we use the “rock seepage coupled nuclear magnetic resonance (NMR) online analysis and imaging system” platform to conduct a long-term penetration test in carbonate rocks under the coupling of stress and reactive fluid. The variation in the multiscale pore volume was quantitatively characterized by the inversion of the T2 spectrum. Subsequently, in combination with permeability measurement, the permeability-porosity evolution during long-term infiltration can be roughly divided into three stages. The experimental results show that the evolution of permeability exhibits noticeable stress sensitivity at the initial stage of the test (0–156 h). Since the compression of the pore volume is the dominant mechanism, the permeability decreases with porosity at this stage. A negative correlation between the evolution of porosity and permeability was observed during the subsequent stage of the test (156–400 h). This phenomenon may be attributed to mineral dissolution at this stage, causing the cementation to be exfoliated from the pore surface and to re-precipitate at the pore throat, locally blocking the seepage channels. As the test continued (400–720 h), mineral dissolution transitioned from micropores to mesopores and macropores, with a synergistic increase in porosity and permeability. These results revealed the competing mechanism of stress compression and mineral dissolution during long-term infiltration, providing an accurate prediction of the seepage properties in carbonate rocks." @default.
• W4313443205 created "2023-01-06" @default.
• W4313443205 creator A5001464751 @default.
• W4313443205 creator A5002500632 @default.
• W4313443205 creator A5032474866 @default.
• W4313443205 creator A5057117256 @default.
• W4313443205 creator A5057723713 @default.
• W4313443205 creator A5071951936 @default.
• W4313443205 date "2023-02-01" @default.
• W4313443205 modified "2023-10-14" @default.
• W4313443205 title "Effect of long-term infiltration on porosity-permeability evolution in carbonate rocks: An online NMR coupling penetration test" @default.
• W4313443205 cites W1600484415 @default.
• W4313443205 cites W1765115934 @default.
• W4313443205 cites W1968059710 @default.
• W4313443205 cites W2027425646 @default.
• W4313443205 cites W2040023566 @default.
• W4313443205 cites W2054163818 @default.
• W4313443205 cites W2057274687 @default.
• W4313443205 cites W2088667249 @default.
• W4313443205 cites W2092939090 @default.
• W4313443205 cites W2095140886 @default.
• W4313443205 cites W2174912353 @default.
• W4313443205 cites W2182938347 @default.
• W4313443205 cites W2338826487 @default.
• W4313443205 cites W2460886311 @default.
• W4313443205 cites W2803872995 @default.
• W4313443205 cites W2810442248 @default.
• W4313443205 cites W2899046881 @default.
• W4313443205 cites W2915997748 @default.
• W4313443205 cites W2947403272 @default.
• W4313443205 cites W2977413572 @default.
• W4313443205 cites W2991047371 @default.
• W4313443205 cites W2996562653 @default.
• W4313443205 cites W3107317270 @default.
• W4313443205 cites W3134978796 @default.
• W4313443205 cites W3163044996 @default.
• W4313443205 cites W3210047487 @default.
• W4313443205 cites W4206700446 @default.
• W4313443205 cites W4239748937 @default.
• W4313443205 cites W4282839281 @default.
• W4313443205 doi "https://doi.org/10.1016/j.jhydrol.2022.129029" @default.
• W4313443205 hasPublicationYear "2023" @default.
• W4313443205 type Work @default.
• W4313443205 citedByCount "2" @default.
• W4313443205 countsByYear W43134432052023 @default.
• W4313443205 crossrefType "journal-article" @default.
• W4313443205 hasAuthorship W4313443205A5001464751 @default.
• W4313443205 hasAuthorship W4313443205A5002500632 @default.
• W4313443205 hasAuthorship W4313443205A5032474866 @default.
• W4313443205 hasAuthorship W4313443205A5057117256 @default.
• W4313443205 hasAuthorship W4313443205A5057723713 @default.
• W4313443205 hasAuthorship W4313443205A5071951936 @default.
• W4313443205 hasConcept C120882062 @default.
• W4313443205 hasConcept C127313418 @default.
• W4313443205 hasConcept C147789679 @default.
• W4313443205 hasConcept C17409809 @default.
• W4313443205 hasConcept C185592680 @default.
• W4313443205 hasConcept C187320778 @default.
• W4313443205 hasConcept C191897082 @default.
• W4313443205 hasConcept C192562407 @default.
• W4313443205 hasConcept C19320362 @default.
• W4313443205 hasConcept C199289684 @default.
• W4313443205 hasConcept C2780659211 @default.
• W4313443205 hasConcept C41625074 @default.
• W4313443205 hasConcept C55493867 @default.
• W4313443205 hasConcept C6494504 @default.
• W4313443205 hasConcept C6648577 @default.
• W4313443205 hasConcept C88380143 @default.
• W4313443205 hasConceptScore W4313443205C120882062 @default.
• W4313443205 hasConceptScore W4313443205C127313418 @default.
• W4313443205 hasConceptScore W4313443205C147789679 @default.
• W4313443205 hasConceptScore W4313443205C17409809 @default.
• W4313443205 hasConceptScore W4313443205C185592680 @default.
• W4313443205 hasConceptScore W4313443205C187320778 @default.
• W4313443205 hasConceptScore W4313443205C191897082 @default.
• W4313443205 hasConceptScore W4313443205C192562407 @default.
• W4313443205 hasConceptScore W4313443205C19320362 @default.
• W4313443205 hasConceptScore W4313443205C199289684 @default.
• W4313443205 hasConceptScore W4313443205C2780659211 @default.
• W4313443205 hasConceptScore W4313443205C41625074 @default.
• W4313443205 hasConceptScore W4313443205C55493867 @default.
• W4313443205 hasConceptScore W4313443205C6494504 @default.
• W4313443205 hasConceptScore W4313443205C6648577 @default.
• W4313443205 hasConceptScore W4313443205C88380143 @default.
• W4313443205 hasFunder F4320321001 @default.
• W4313443205 hasFunder F4320325564 @default.
• W4313443205 hasFunder F4320336635 @default.
• W4313443205 hasLocation W43134432051 @default.
• W4313443205 hasOpenAccess W4313443205 @default.
• W4313443205 hasPrimaryLocation W43134432051 @default.
• W4313443205 hasRelatedWork W1966018702 @default.
• W4313443205 hasRelatedWork W2078704581 @default.
• W4313443205 hasRelatedWork W2359822476 @default.
• W4313443205 hasRelatedWork W2372412760 @default.
• W4313443205 hasRelatedWork W2387742759 @default.
• W4313443205 hasRelatedWork W2390326989 @default.
• W4313443205 hasRelatedWork W3170930060 @default.
• W4313443205 hasRelatedWork W4244074133 @default.

• next