2018
DOI: 10.1016/s1876-3804(18)30046-6
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Model construction of micro-pores in shale: A case study of Silurian Longmaxi Formation shale in Dianqianbei area, SW China

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Cited by 80 publications
(37 citation statements)
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“…The adsorption/desorption isotherms presented in Figure 2 represent a type IV isotherm with a small H3 hysteresis loop observed in the p / p 0 range of 0.8–1.0. It indicates that samples belong to the mesopore group with groove pores structures [ 45 ]. The inset figure in Figure 2 shows the pore size curve, determined from the adsorption branch of the isotherm.…”
Section: Resultsmentioning
confidence: 99%
“…The adsorption/desorption isotherms presented in Figure 2 represent a type IV isotherm with a small H3 hysteresis loop observed in the p / p 0 range of 0.8–1.0. It indicates that samples belong to the mesopore group with groove pores structures [ 45 ]. The inset figure in Figure 2 shows the pore size curve, determined from the adsorption branch of the isotherm.…”
Section: Resultsmentioning
confidence: 99%
“…As a multi-stage superimposed basin developed on the Upper Yangtze platform, the Dianqianbei Depression is adjacent to the southern margin of the Sichuan Basin in the north, the Dianqian uplift in the south (Fig. 1), and the Diandongbei Depression in the west (Chen et al 2018c). The depression is featured by strong tectonics in the south and west, and it is tectonically a typical slotted east-west extended fold belt composed of wide anticlines and closed synclines (Liang et al 2011;He et al 2019).…”
Section: Geological Settingmentioning
confidence: 99%
“…(1) Atomic-scale geometrically heterogeneous surfaces: statistical self-similarity, a typical geometric feature of surface heterogeneity that can hardly be described by Euclidean geometry, is a ubiquitous characteristic of most materials in nature . Thanks to the fractal theory advanced by Mandelbrot, , the surface fractal dimension functions as an applicable measure of surface geometric heterogeneity. The fractal pore morphology has been examined by mercury intrusion porosimetry (MIP), the fractal Frenkel–Halsey–Hill (FHH) adsorption isotherm equation based on nitrogen adsorption, , nuclear magnetic resonance, ,, small-angle and ultrasmall-angle neutron scattering, , ...…”
Section: Introductionmentioning
confidence: 99%
“…These findings indicate marked surface geometric heterogeneity at the atomic scale. (2) Slitlike shape: the pore shape can be determined from the shape of the hysteresis loop of the nitrogen adsorption and desorption isotherms (see refs , , , , , , , , , , , , , , , , ) according to the classification by the International Union of Pure and Applied Chemistry (IUPAC) or by the field emission scanning electron microscope (see refs , , , , , , , , , , , , , , , , , , , , , , ) and MIP. ,,, The summary statistics reveal that slit pores constitute the largest...…”
Section: Introductionmentioning
confidence: 99%
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