2019
DOI: 10.3390/en12071207
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Organic Matter Pore Characterization of the Wufeng-Longmaxi Shales from the Fuling Gas Field, Sichuan Basin: Evidence from Organic Matter Isolation and Low-Pressure CO2 and N2 Adsorption

Abstract: Organic matter (OM) pores are significant for shale gas accumulation and flow mechanisms. The pores of Wufeng-Longmaxi (W-L) shale in the Sichuan Basin, China have been extensively characterized, however, the proportion of OM pores in this shale have not been adequately discussed. In this study, the contribution of OM pores to the total pore volume of W-L shale was quantitatively studied through the analysis of OM isolation, field emission scanning electron microscopy (FE-SEM) and low-pressure CO2 and N2 adsor… Show more

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Cited by 13 publications
(6 citation statements)
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“…Although shale oil reservoirs have small natural fractures, they are characterized in the order of the nanodarcy formations. The International Union of Pure and Applied Chemistry (IUPAC) classifies pores on a nanometric scale as macropores (>50 nm), mesopores (2–50 nm), and micropores (2 nm) …”
Section: Background Of the Shale/tight Oil Reservoirmentioning
confidence: 99%
“…Although shale oil reservoirs have small natural fractures, they are characterized in the order of the nanodarcy formations. The International Union of Pure and Applied Chemistry (IUPAC) classifies pores on a nanometric scale as macropores (>50 nm), mesopores (2–50 nm), and micropores (2 nm) …”
Section: Background Of the Shale/tight Oil Reservoirmentioning
confidence: 99%
“…The multipoint BET surface area showed a positive trend with average pore size and a strong positive relationship with total pore volume R 2 = 0.83, Fig. 13d), indicating that the shale beds with smaller average pore size have more abundant macropores and mesopores (Chen et al, 2016;Li et al, 2019). The scatter plot between multipoint BET surface area and fixed carbon content shows an average negative correlation (R 2 = 0.55, Fig 13e), signifying that the organic matter does not support gas storage (Hazra et al, 2018b), whereas the BET plot shows a weak positive trend with the ash content that comparatively favors adsorption of gas (Fig.…”
Section: Discussionmentioning
confidence: 94%
“…In particular, some of the clay minerals with mixed OM pores exhibited long strip shapes (Figure d). The interP pores in the shale samples were mainly distributed between the quartzes, feldspars, clay minerals, or calcites (Figure e–g); were triangular and polygonal in shape; and were in contact with each other, forming an effective pore network . The sizes of the interP pores were relatively large, ranging from the nanoscale to microscale.…”
Section: Resultsmentioning
confidence: 99%
“…The interP pores in the shale samples were mainly distributed between the quartzes, feldspars, clay minerals, or calcites (Figure 5e−g); were triangular and polygonal in shape; and were in contact with each other, forming an effective pore network. 32 The sizes of the interP pores were relatively large, ranging from the nanoscale to microscale. The intraP pores were mainly developed within quartzes (Figure 5h) and calcites (Figure 5i), which were relevant to the dissolution in the shales.…”
Section: Mineral Compositions and Organicmentioning
confidence: 99%