We formulate a hierarchy of models relevant for studying coupled
well-reservoir flows. The starting point is an integral equation
representing unsteady single-phase 3-D porous media flow and the
1-D isothermal Euler equations representing unsteady well flow.
This system of conservation laws is coupled to the integral
equation through natural coupling conditions accounting for the
flow between well and surrounding reservoir. By imposing
simplifying assumptions we obtain various hyperbolic-parabolic and
hyperbolic-elliptic systems. In particular, by assuming that the
fluid is incompressible we obtain a hyperbolic-elliptic system
for which we present existence and uniqueness results. Numerical
examples demonstrate formation of steep gradients resulting from a
balance between a local nonlinear convective term and a non-local
diffusive term. This balance is governed by various well,
reservoir, and fluid parameters involved in the non-local
diffusion term, and reflects the interaction between well and
reservoir.
Citation: Steinar Evje, Kenneth H. Karlsen. Hyperbolic-elliptic models for well-reservoir flow[J]. Networks and Heterogeneous Media, 2006, 1(4): 639-673. doi: 10.3934/nhm.2006.1.639
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Abstract
We formulate a hierarchy of models relevant for studying coupled
well-reservoir flows. The starting point is an integral equation
representing unsteady single-phase 3-D porous media flow and the
1-D isothermal Euler equations representing unsteady well flow.
This system of conservation laws is coupled to the integral
equation through natural coupling conditions accounting for the
flow between well and surrounding reservoir. By imposing
simplifying assumptions we obtain various hyperbolic-parabolic and
hyperbolic-elliptic systems. In particular, by assuming that the
fluid is incompressible we obtain a hyperbolic-elliptic system
for which we present existence and uniqueness results. Numerical
examples demonstrate formation of steep gradients resulting from a
balance between a local nonlinear convective term and a non-local
diffusive term. This balance is governed by various well,
reservoir, and fluid parameters involved in the non-local
diffusion term, and reflects the interaction between well and
reservoir.
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2.
Helmer A. Friis, Steinar Evje,
Asymptotic behavior of a compressible two-phase model with well–formation interaction,
2013,
254,
00220396,
3957,
10.1016/j.jde.2013.02.001
3.
Steinar Evje,
Global weak solutions for a compressible gas-liquid model with well-formation interaction,
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