2020
DOI: 10.1155/2020/5295490
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Quantitative Characterization of Pore Connectivity and Movable Fluid Distribution of Tight Sandstones: A Case Study of the Upper Triassic Chang 7 Member, Yanchang Formation in Ordos Basin, China

Abstract: The pore connectivity and distribution of moveable fluids, which determines fluid movability and recoverable reserves, are critical for enhancing oil/gas recovery in tight sandstone reservoirs. In this paper, multiple techniques including high-pressure mercury intrusion porosimetry (MIP), nuclear magnetic resonance (NMR), scanning electron microscopy (SEM), and microcomputer tomography scanning (micro-CT) were used for the quantitative characterization of pore structure, pore connectivity, and movable fluid di… Show more

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Cited by 3 publications
(2 citation statements)
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“…NNR and Centrifugation. NMR techniques have been are already widely applied to study the distribution of fluids in tight sandstone reservoirs because of their efficiency, nondestructiveness, and accuracy [23,24]. The main principle is that fluids present in porous media generate detectable signals when subjected to an external magnetic field, and the intensity of the signal is proportional to the number of hydrogen nuclei in the sample [24].…”
Section: Experiments Methods and Proceduresmentioning
confidence: 99%
“…NNR and Centrifugation. NMR techniques have been are already widely applied to study the distribution of fluids in tight sandstone reservoirs because of their efficiency, nondestructiveness, and accuracy [23,24]. The main principle is that fluids present in porous media generate detectable signals when subjected to an external magnetic field, and the intensity of the signal is proportional to the number of hydrogen nuclei in the sample [24].…”
Section: Experiments Methods and Proceduresmentioning
confidence: 99%
“…Two T 2 cutoff values have been used to divide the T 2 spectrum into fully movable, partially movable, and fully immovable parts. , The movable fluid is mainly distributed in large pores and pores controlled by large pore throats, and the bound fluid is present in small pores and large pores controlled by small pore throats . Centrifugal force controls the theoretical minimum pore radius corresponding to the moving fluid. , However, the T 2 signal changes completely in the short relaxation range after the centrifugation of some samples. This phenomenon suggests that the short relaxation signal of the T 2 spectra of these samples may reflect macropore information to some extent. It might be possible to analyze the applicability of T 2 in terms of the lower limit of the centrifugal radius.…”
Section: Introductionmentioning
confidence: 99%