In fluid dynamics, the Buckley–Leverett equation is a conservation equation used to model two-phase flow in porous media.
[1] The Buckley–Leverett equation or the Buckley–Leverett displacement describes an immiscible displacement process, such as the displacement of oil by water, in a one-dimensional or quasi-one-dimensional reservoir.
This equation can be derived from the mass conservation equations of two-phase flow, under the assumptions listed below.
is the wetting-phase (water) saturation,
is the total flow rate,
is the area of the cross-section in the sample volume, and
is the fractional flow function of the wetting phase.
is an S-shaped, nonlinear function of the saturation
, which characterizes the relative mobilities of the two phases: where
denote the wetting and non-wetting phase mobilities.
denote the relative permeability functions of each phase and
represent the phase viscosities.
The Buckley–Leverett equation is derived based on the following assumptions: The characteristic velocity of the Buckley–Leverett equation is given by: The hyperbolic nature of the equation implies that the solution of the Buckley–Leverett equation has the form
The non-convexity of the fractional flow function
also gives rise to the well known Buckley-Leverett profile, which consists of a shock wave immediately followed by a rarefaction wave.
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