2019
DOI: 10.1142/s0218348x19400115
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Investigation of Fractal Characteristics and Methane Adsorption Capacity of the Upper Triassic Lacustrine Shale in the Sichuan Basin, Southwest China

Abstract: To better understand the nanopore characteristics and their effects on methane adsorption capacity of shales, we performed fractal analysis of nine shale samples collected from the fifth member of Upper Triassic Xujiahe Formation in the Sichuan Basin, southwest China. [Formula: see text] adsorption results show that shales have different adsorption characteristics at relative pressure of 0–0.5 and 0.5–1. Two fractal dimensions [Formula: see text] and [Formula: see text] were calculated using the Frenkel–Halsey… Show more

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Cited by 6 publications
(8 citation statements)
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“…Fractal concept was first proposed in 1975, by Mandelbrot [42], and widely used in porous media including shale [35,36,37,38,39,40,41,43,44,45]. Fractal theory is used to describe the roughness of pore surface and the complexity of pore structure for porous media.…”
Section: Resultsmentioning
confidence: 99%
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“…Fractal concept was first proposed in 1975, by Mandelbrot [42], and widely used in porous media including shale [35,36,37,38,39,40,41,43,44,45]. Fractal theory is used to describe the roughness of pore surface and the complexity of pore structure for porous media.…”
Section: Resultsmentioning
confidence: 99%
“…The commonly used parameter is fractal dimension D. The larger the fractal dimension, the rougher the pore surface or the more complex the pore structure. It is a well-accepted method to use gas adsorption for fractal dimension calculation [35,36,37,38,39,40,41,64]. According to Pfeifer’s theory [65], the fractal dimension can be calculated by the FHH equation:lnV=Kln[ln(P0P)]+C…”
Section: Resultsmentioning
confidence: 99%
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“…(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%
“…(3) Nanoscale average diameter: IUPAC refreshed the pore classification by size, defining nanopores as the pores with diameters to an upper limit of about 100 nm . Usually, the average pore diameter ( d ) is calculated from the cylindrical pore model ( d = 4 v / a ) with the specific pore surface area ( a ) and the specific pore volume ( v ) obtained in carbon dioxide or nitrogen adsorption experiments (see refs , , , , , , , , , , , , , ). The distribution indicates that the overwhelming majority of the average diameters lies in the range of 0–50 nm (Figure c), which conforms to the definition of nanopores.…”
Section: Introductionmentioning
confidence: 99%