Impact of model error on the measurement of flow properties needed to describe flow through porous media

被引:6
作者
Bentsen, RG
机构
[1] Sch. of Mining and Petrol. Eng., Dept. of Civ. and Environ. Eng., University of Alberta, Edmonton
来源
REVUE DE L INSTITUT FRANCAIS DU PETROLE | 1997年 / 52卷 / 03期
关键词
D O I
10.2516/ogst:1997042
中图分类号
TE [石油、天然气工业]; TK [能源与动力工程];
学科分类号
0807 ; 0820 ;
摘要
Indirect methods are commonly employed to determine the fundamental flow properties needed to describe flow through porous media. Consequently, if one or more of the postulates underlying the mathematical description of such indirect methods is invalid, significant model error can be introduced into the measured value of the flow property. In particular, this study shows that effective mobility curves that include the effect of viscous coupling between fluid phases differ significantly from those that exclude such coupling. Moreover, it is shown that the conventional effective mobilities that pertain to steady-state, cocurrent flow, steady-state, countercurrent flow and pure countercurrent imbibition differ significantly. Thus, it appears that traditional effective mobilities are not true parameters: rather, they are infinitely nonunique. In addition, it is shown that. while neglect of hydrodynamic forces introduces a small amount of model error into the pressure difference curve for cocurrent flow in unconsolidated porous media, such neglect introduces a large amount of model error into the pressure difference curve for countercurrent flow in such porous media. Moreover, such neglect makes it difficult to explain why the pressure gradients that pertain to steady-state, countercurrent flow are opposite in sign. It is shown also that improper handling of the inlet boundary condition can introduce significant model error into the analysis. This is because, if a short core is used with one of the unsteady-state methods for determining effective mobility, it may take many pore volumes of injection before the inlet saturation rises to its maximal value, which is in contradiction with the usual assumption that the inlet saturation rises immediately to its maximal value. Finally, it is pointed out that, because of differences in flow regime and scale, the effective mobilities measured in the laboratory may not be appropriate for inclusion in the data base for a reservoir-scale simulation.
引用
收藏
页码:299 / 315
页数:17
相关论文
共 31 条
[1]   CONDITIONS UNDER WHICH THE CAPILLARY TERM MAY BE NEGLECTED [J].
BENTSEN, RG .
JOURNAL OF CANADIAN PETROLEUM TECHNOLOGY, 1978, 17 (04) :25-30
[2]   EFFECT OF HYDRODYNAMIC-FORCES ON CAPILLARY-PRESSURE AND RELATIVE PERMEABILITY [J].
BENTSEN, RG .
TRANSPORT IN POROUS MEDIA, 1994, 17 (02) :121-132
[3]   EFFECT OF HYDRODYNAMIC-FORCES ON THE PRESSURE-DIFFERENCE EQUATION [J].
BENTSEN, RG .
TRANSPORT IN POROUS MEDIA, 1994, 17 (02) :133-144
[4]   AN INVESTIGATION INTO WHETHER THE NONDIAGONAL MOBILITY COEFFICIENTS WHICH ARISE IN COUPLED, 2-PHASE FLOW ARE EQUAL [J].
BENTSEN, RG .
TRANSPORT IN POROUS MEDIA, 1994, 14 (01) :23-32
[5]   A NEW APPROACH TO INSTABILITY THEORY IN POROUS-MEDIA [J].
BENTSEN, RG .
SOCIETY OF PETROLEUM ENGINEERS JOURNAL, 1985, 25 (05) :765-779
[6]   ON THE USE OF CONVENTIONAL COCURRENT AND COUNTERCURRENT EFFECTIVE PERMEABILITIES TO ESTIMATE THE 4 GENERALIZED PERMEABILITY COEFFICIENTS WHICH ARISE IN COUPLED, 2-PHASE FLOW [J].
BENTSEN, RG ;
MANAI, AA .
TRANSPORT IN POROUS MEDIA, 1993, 11 (03) :243-262
[7]  
BENTSEN RG, 1981, J CAN PETROL TECHNOL, V20, P93
[8]  
BENTSEN RG, 1991, AOSTRA J RES, V7, P169
[9]  
BENTSEN RG, 1989, AOSTRA J RES, V5, P61
[10]  
BENTSEN RG, 1990, AOSTRA J RES, V6, P155