2022
DOI: 10.1021/acsomega.2c03717
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Study of Fractal and Multifractal Features of Pore Structure in Tight Sandstone Reservoirs of the Permian Lucaogou Formation, Jimsar Sag, Junggar Basin, Northwest China

Abstract: The primary factor impacting the tight sandstone reservoirs and fluid flow capacity represents the pore-throat structure. On the basis of petrophysical characteristics test, scanning electron microscopy (SEM), and casting thin-section examination of tight sandstone reservoir specimens from the Permian Lucaogou Formation in Jimsar Sag, Junggar Basin., the full-size pore-throat parameters and distribution characteristics were determined by constant-rate mercury injection (CRMI) analysis. Using fractal theory and… Show more

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Cited by 3 publications
(9 citation statements)
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“…This study employs the S-A model was used to decompose the composite anomalies of the PC1 and PC2 principal component combination, thereby obtaining the principal component background field and anomaly field in the study area (Figures and ). Among them, the background field obtained by S-A decomposition mainly reflects the background composition of elemental mass fractions; high-background areas may be favorable for polymetallic mineral exploration; variations in the background strength reflect the presence of elements in a favorable geological context for mineralization, and the anomaly field mainly reflects local anomalous mass molecules of elements and noise generated during data processing. , …”
Section: Results and Discussionmentioning
confidence: 99%
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“…This study employs the S-A model was used to decompose the composite anomalies of the PC1 and PC2 principal component combination, thereby obtaining the principal component background field and anomaly field in the study area (Figures and ). Among them, the background field obtained by S-A decomposition mainly reflects the background composition of elemental mass fractions; high-background areas may be favorable for polymetallic mineral exploration; variations in the background strength reflect the presence of elements in a favorable geological context for mineralization, and the anomaly field mainly reflects local anomalous mass molecules of elements and noise generated during data processing. , …”
Section: Results and Discussionmentioning
confidence: 99%
“…Among them, the background field obtained by S-A decomposition mainly reflects the background composition of elemental mass fractions; high-background areas may be favorable for polymetallic mineral exploration; variations in the background strength reflect the presence of elements in a favorable geological context for mineralization, and the anomaly field mainly reflects local anomalous mass molecules of elements and noise generated during data processing. 23 , 38 …”
Section: Results and Discussionmentioning
confidence: 99%
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“…Dynamic contact angle θ d is one of the important characteristics of the wetting behavior of liquid on a solid surface, which can be expressed as 64 Ä where θ e is the equilibrium contact angle, ζ is the friction coefficient of contact line, C pin is the pinning coefficient, and C is the smoothing parameter. Ca is the capillary number, which can be expressed as 64 = v Ca / cl (5) where v cl is the contact line velocity. The irreducible water saturation S wc is the fraction of irreducible water in a given pore space, and more details about irreducible water saturation S wc can be found in Appendix B.…”
mentioning
confidence: 99%