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Yongchen Song

Professor
Supervisor of Doctorate Candidates
Supervisor of Master's Candidates


Gender:Male
Alma Mater:大连理工大学
Degree:Doctoral Degree
School/Department:能源与动力学院
Discipline:Energy and Environmental Engineering
Business Address:能动大楼810
Contact Information:songyc@dlut.edu.cn
E-Mail:songyc@dlut.edu.cn
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Current position: Home >> Scientific Research >> Paper Publications

Numerical Analysis of CO2 and Water Displacement in Natural Rock Cores Based on a Fully Heterogeneous Model

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Indexed by:期刊论文

Date of Publication:2016-03-01

Journal:JOURNAL OF HYDROLOGIC ENGINEERING

Included Journals:SCIE

Volume:21

Issue:3

ISSN No.:1084-0699

Key Words:Core flooding experiment; Numerical modeling; Multiphase flow; Capillary pressure; Permeability; Relative permeability

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 CO2/water 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 J-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 CO2 saturation are observed, the fully heterogeneous model is generally applicable to model CO2/brine two-phase flow in the sandstone core and can potentially reflect the CO2 saturation buildup; (3)the heterogeneity in capillary pressure plays an important role in generating local fluctuations of CO2 saturation profile and causing the heterogeneous CO2 saturation distribution, whereas the permeability heterogeneity can only result in slight fluctuations of CO2 saturation profile and has a small effect on the heterogeneous saturation distribution; and (4)an abrupt rise of CO2 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.