Abstract
Based on a core flooding experiment, a multiphase flow model considering the heterogeneity of porosity, permeability, capillary pressure, and relative permeability (i.e., the fully heterogeneous model) is proposed to analyze displacement in a natural sandstone core. Our results indicate (1) the fractal model approximately represents the porosity-permeability relationship of the core and combining it with the Leverett’s -function, it can be used to effectively describe the heterogeneity of capillary pressure; (2) although hypothetically assuming petro-physical properties at a few locations where obviously inhomogeneous structure and significant fluctuations of saturation are observed, the fully heterogeneous model is generally applicable to model two-phase flow in the sandstone core and can potentially reflect the saturation buildup; (3) the heterogeneity in capillary pressure plays an important role in generating local fluctuations of saturation profile and causing the heterogeneous saturation distribution, whereas the permeability heterogeneity can only result in slight fluctuations of saturation profile and has a small effect on the heterogeneous saturation distribution; and (4) an abrupt rise of saturation in the heterogeneous downstream region of the core cannot be fully reasonably interpreted by the heterogeneity of capillary pressure and permeability. The heterogeneity in the relative permeability can also possibly play an important role in causing such rise.
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Acknowledgments
Anonymous reviewers are acknowledged for their constructive comments. This work was financially supported by the National Science Foundation of China (No. 51376033 and 41004031) and the Fundamental Research Funds for the Central Universities (No. DUT15LAB18).
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© 2015 American Society of Civil Engineers.
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Received: Feb 18, 2015
Accepted: Sep 17, 2015
Published online: Nov 20, 2015
Published in print: Mar 1, 2016
Discussion open until: Apr 20, 2016
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