2016
DOI: 10.1016/j.advwatres.2016.07.017
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C1-Continuous relative permeability and hybrid upwind discretization of three phase flow in porous media

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Cited by 26 publications
(16 citation statements)
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“…An interpolation method is usually used to compute k ro from two-phase oil-gas k rog (s o ) and oil-water k row (s o ) data, see for example the works by Stone (1973) and Baker (1988). As discussed in Lee and Efendiev (2016), the method choice can affect the nonlinear convergence of the underlying discretization scheme.…”
Section: Resultsmentioning
confidence: 99%
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“…An interpolation method is usually used to compute k ro from two-phase oil-gas k rog (s o ) and oil-water k row (s o ) data, see for example the works by Stone (1973) and Baker (1988). As discussed in Lee and Efendiev (2016), the method choice can affect the nonlinear convergence of the underlying discretization scheme.…”
Section: Resultsmentioning
confidence: 99%
“…which is the default setting of the commercial simulator Eclipse (Schlumberger 2013). This choice ensures positive values and continuous derivatives provided that k row , k rog fulfill the same criterion (Baker 1988;Lee and Efendiev 2016). We consider simple relative permeabilities given by Corey functions for a pair of wetting and non-wetting fluids,…”
Section: Resultsmentioning
confidence: 99%
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“…In practice, reservoir simulators often suffer from serious difficulties in obtaining converged numerical solutions for the preselected timestep size. This is because even though FIM is unconditionally stable, the nonlinear Newton-based solver will not be unconditionally convergent (Lee and Efendiev 2016). When convergence failures are encountered, the most commonly used remedy is to restart the nonlinear solver with a smaller timestep size (Younis et al 2010).…”
Section: Introductionmentioning
confidence: 99%
“…Lee et al (2015) proposed a continuously differentiable numerical flux scheme called Hybrid Upwinding (HU) to address the discontinuous behavior due to flow reversal. In HU, the upwinding of the viscous term of the numerical flux is based on the sign of the total velocity, whereas the directionality of the gravitational term is determined by phase densities, such that the heaviest fluid goes down and the lightest fluid goes up (Lee and Efendiev 2016). extended the work of Lee et al (2015) to an arbitrary number of fluid phases.…”
Section: Introductionmentioning
confidence: 99%