A MECHANISTIC POPULATION BALANCE MODEL FOR TRANSIENT AND STEADY-STATE FOAM FLOW IN BOISE SANDSTONE

被引:175
作者
KOVSCEK, AR
PATZEK, TW
RADKE, CJ
机构
[1] UNIV CALIF BERKELEY,LAWRENCE BERKELEY LAB,DIV EARTH SCI,BERKELEY,CA 94720
[2] UNIV CALIF BERKELEY,LAWRENCE BERKELEY LAB,DEPT CHEM ENGN,BERKELEY,CA 94720
[3] UNIV CALIF BERKELEY,LAWRENCE BERKELEY LAB,DEPT MAT SCI & MINERAL ENGN,BERKELEY,CA 94720
关键词
D O I
10.1016/0009-2509(95)00199-F
中图分类号
TQ [化学工业];
学科分类号
0817 ;
摘要
Foam in porous media is discontinuous on a length scale that overlaps with pore dimensions. This foam-bubble microstructure determines the flow behavior of foam in porous media and, in turn, the flow of gas and liquid. Modeling of foam displacement has been frustrated because empirical extensions of the conventional continuum and Newtonian description of fluids in porous media do not reflect the coupling of foam-bubble microstructure and foam theology. We report a mechanistic model for foam displacement in porous media that incorporates pore-level mechanisms of foam generation, coalescence, and transport in the transient Bow of aqueous foams. A mean-size foam-bubble conservation equation, along with the traditional reservoir/groundwater simulation equations, provides the foundation for our mechanistic foam-displacement simulations. Since foam mobility depends heavily upon its texture, the bubble population balance is both useful and necessary, as the role of foam texture must be incorporated into any model which seeks to predict foam flow accurately. Our model employs capillary-pressure-dependent kinetic expressions for lamellae generation and coalescence, and incorporates trapping of lamellae. Additionally, the effects of surfactant chemical transport are included. All model parameters have clear physical meaning and, consequently, are independent of Bow conditions. Thus, for the first time, scale up of foam-flow behavior from laboratory to field dimensions appears possible. The simulation model is verified by comparison with experiment. In situ, transient, and steady aqueous-phase liquid contents are garnered in a 1.3 mu m(2) Boise sandstone using scanning gamma-ray densitometry. Backpressures exceed 5 MPa, and foam quality ranges from 0.80 to 0.99. Total superficial velocities range from as little as 0.42 to 2.20 m/d. Sequential pressure taps measure Row resistance. Excellent agreement is found between experiment and theory. Further, we find that the bubble population balance is the only current means of describing all Row modes of foam self-consistently.
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收藏
页码:3783 / 3799
页数:17
相关论文
共 36 条
[1]   THE INFLUENCE OF DISJOINING PRESSURE ON FOAM STABILITY AND FLOW IN POROUS-MEDIA [J].
ARONSON, AS ;
BERGERON, V ;
FAGAN, ME ;
RADKE, CJ .
COLLOIDS AND SURFACES A-PHYSICOCHEMICAL AND ENGINEERING ASPECTS, 1994, 83 (02) :109-120
[2]  
Aziz K., 1979, PETROLEUM RESERVOIR
[3]  
Bear J., 1972, DYNAMICS FLUIDS PORO
[4]   GENERALIZED ENTERING COEFFICIENTS - A CRITERION FOR FOAM STABILITY AGAINST OIL IN POROUS-MEDIA [J].
BERGERON, V ;
FAGAN, ME ;
RADKE, CJ .
LANGMUIR, 1993, 9 (07) :1704-1713
[5]  
Bernard G.G., 1965, SOC PET ENG J, P295
[6]   THE MOTION OF LONG BUBBLES IN TUBES [J].
BRETHERTON, FP .
JOURNAL OF FLUID MECHANICS, 1961, 10 (02) :166-188
[7]  
CHAMBERS KT, 1991, INTERFACIAL PHENOMEN, P191
[8]  
Corey A. T., 1954, PROD MON, V19, P38
[9]  
de Vries A.S., 1990, SPE RESERVOIR ENG, V5, P185, DOI [10.2118/18075-pa, DOI 10.2118/18075-PA]
[10]  
Ettinger R.A., 1992, SPE RESERVOIR ENG, V7, P83, DOI [DOI 10.2118/19688-PA, 10.2118/19688-PA]