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Petroleum Geoscience; February 2007; v. 13; no. 1; p. 25-35; DOI: 10.1144/1354-079305-676
© 2007 Geological Society of London
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Original Article

Hierarchical approach for simulating fluid flow in normal fault zones

Silje Støren Berg1,2 and Erlend Øian1

1 Centre for Integrated Petroleum Research, University of Bergen, Allégt. 41, 5007 Bergen, Norway (e-mail: erlendo@mi.uib.no)
2 Present address: Statoil Research Center, Rotvoll, Arkitekt Ebbellsvei 10, 7005 Trondheim, Norway (e-mail: silbe@statoil.com)

Two-phase flow in faults is complex and difficult to predict. To analyse the effect of fault zones on fluid flow, this article presents a hierarchical geological/numerical framework aimed at simulating two-phase flow. The starting point is that fault zones consist of structures at several length scales, with each scale represented by suitable techniques within the same numerical model. A series of two-phase flow simulation experiments was conducted on four geological cases: one reference case with undeformed host rock and three cases with increasingly more complexity added to them. All the structures consist of lower permeability fault rocks in a high permeability host rock. The simulations were performed using an in-house flow simulator. The fault core (large scale) was modelled explicitly through local grid refinement, the subsidiary faults (intermediate scale) were represented in a discrete manner, while an upscaling procedure captured the effect of the deformation bands (fine scale). The simulation results show that each scale has a significant effect on the saturation, pressure drop and oil production, and that capillary pressure and anisotropic permeability are important parameters. The results emphasize the importance of the scale-dependent approach for analysing the effect of faults on two-phase flow.

KEYWORDS: Hierarchical modelling, numerical modelling, flow simulation, normal fault, fault seal




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