Three-dimensional imaging of multiphase flow in porous media

被引:75
|
作者
Turner, ML
Knüfing, L
Arns, CH
Sakellariou, A
Senden, TJ
Sheppard, AP
Sok, RM
Limaye, A
Pinczewski, WV
Knackstedt, MA [1 ]
机构
[1] Australian Natl Univ, Res Sch Phys Sci & Engn, Dept Appl Math, Canberra, ACT 0200, Australia
[2] Australian Natl Univ, Dept Geol, CRCLEME, Canberra, ACT 0200, Australia
[3] VizLab, ANU Supercomp Facil, Canberra, ACT 0200, Australia
[4] Univ New S Wales, Sch Petr Engn, Sydney, NSW 2052, Australia
关键词
porous media; X-ray-CT; multiphase flow; morphology;
D O I
10.1016/j.physa.2004.03.059
中图分类号
O4 [物理学];
学科分类号
0702 ;
摘要
This paper reports progress in the 3D pore-scale micro-CT imaging of multiple fluid phases during drainage experiments in porous materials. Experiments performed on a sintered monodisperse bead pack and a Berea sandstone sample are described. It is observed that the residual (trapped) wetting phase in the sintered bead pack is present as pendular rings, bridges between adjacent grains and lenses within pore throats. Estimates of the residual wetting phase saturation are in accord with previous experiments and predictions on model bead packs. Relative permeabilities computed directly on the digitised images of the fluid phases are in good agreement with experimentally measured values for Berea sandstone. Two simple numerical methods for estimating two phase drainage saturation distributions directly from images are compared. Both methods give good agreement with the bead pack experiment. The match for Berea sandstone is poorer; differences may be due to variable wettability. (C) 2004 Elsevier B.V. All rights reserved.
引用
收藏
页码:166 / 172
页数:7
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