2021
DOI: 10.1016/j.jngse.2021.104229
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Low-permeability reservoir sample wettability characterization at multiple scales: Pore-, micro- and macro-contact angles

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Cited by 24 publications
(15 citation statements)
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“…The contact angle and wetting area, two variables that directly determine wettability, are reasonably considered in this rock model because the factors influencing rock wettability (minerals, chemistry, pressure, temperature, etc. ), which ultimately act on the change of contact angle and wetting area, are fully considered …”
Section: Petrophysical Model and Numerical Simulation Schemementioning
confidence: 99%
See 1 more Smart Citation
“…The contact angle and wetting area, two variables that directly determine wettability, are reasonably considered in this rock model because the factors influencing rock wettability (minerals, chemistry, pressure, temperature, etc. ), which ultimately act on the change of contact angle and wetting area, are fully considered …”
Section: Petrophysical Model and Numerical Simulation Schemementioning
confidence: 99%
“…), which ultimately act on the change of contact angle and wetting area, are fully considered. 51 3.2. Construction of Fluid Distribution.…”
Section: Petrophysical Model and Numerical Simulation Schemementioning
confidence: 99%
“…Contact angle is a scale-dependent parameter, that is, macroscale contact angles measured on flat surfaces may differ significantly from micro- and nanoscale contact angles at in situ porous rocks, ,, because of line tension and local heterogeneity. , Thus, it is suggested to use advanced imaging techniques (such as microcomputed tomography , and nuclear magnetic resonance ) to further study wettability inside in situ porous rocks in the future. However, the resolution of the advanced imaging equipment is still not powerful enough to visualize a three-phase contact line clearly at nano-scale .…”
Section: Research Gaps and Future Outlookmentioning
confidence: 99%
“…More specifically, the soluble minerals in the rock are partially dissolved by the reaction with water, which has a certain effect on the SI of water, and the previous studies’ results show that the salinity of water also has a great influence on SI. In addition, clay minerals typically swell to a certain extent when in contact with water, complicating the pore structure of shale (e.g., blocking pores and throats) and sometimes reducing fluid migration rates. , For homogeneous porous media, the greater the tortuosity of the connected pore system, the longer the migration path of solute molecules through the same linear distance in the porous medium and the smaller the imbibition slope . Due to the strong heterogeneity and complex pore structure of shale with the coexistence of organic matter pores and inorganic pores, shale reservoirs often exhibit mixed wettability (Dalmatian wettability), which in turn affects the SI behavior. , The wettability and pore connectivity of shale reservoirs were previously evaluated by SI experiments. , However, the application of SI on the enrichment mechanism of hydrocarbons is quite limited. SI experiments, which can be treated as physical simulation experiments of fluid migration and accumulation in shale reservoirs to some extent, have the advantage of simple sample preparation, dynamic recording of changes in the imbibed fluid volume, and low costs.…”
Section: Introductionmentioning
confidence: 99%