Abstract
In this paper we consider porous media flow without capillary effects. We present a streamline method which includes gravity effects by operator splitting. The flow equations are treated by an IMPES method, where the pressure equation is solved by a (standard) finite element method. The saturation equation is solved by utilizing a front tracking method along streamlines of the pressure field. The effects of gravity are accounted for in a separate correction step. This is the first time streamlines are combined with gravity for three-dimensional (3D) simulations, and the method proves favourable compared to standard splitting methods based on fractional steps. By our splitting we can take advantage of very accurate and efficient 1D methods. The ideas have been implemented and tested in a full field simulator. In that context, both accuracy and CPU efficiency have tested favourably.
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Abbreviations
- S i :
-
saturation of phase i
- (Si) t :
-
partial derivative of S i, w.r.t. t, ∂Si/∂t
- x :
-
space coordinates
- γ :
-
gravity vector
- P i :
-
pressure within phase i
- ϱ i :
-
density of phase i
- μ iί :
-
dynamic viscosity of the phase i
- K :
-
absolute permeability of the rock
- k ί :
-
relative permeability of phase i
- λ ί :
-
mobility of phase i = Kk i/μi
- f ί :
-
fractional flow = λ i/(λn + λw)
- v ί :
-
Darcy velocity (specific discharge)
- v tot :
-
total Darcy velocity = v n + vw
- q ί :
-
mass rate of injection or production per unit of volume
- φ :
-
porosity of the rock
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Bratvedt, F., Gimse, T. & Tegnander, C. Streamline computations for porous media flow including gravity. Transp Porous Med 25, 63–78 (1996). https://doi.org/10.1007/BF00141262
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DOI: https://doi.org/10.1007/BF00141262