Buckley–Leverett equation
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.
Equation
In a quasi-1D domain, the Buckley–Leverett equation is given by:
where is the wetting-phase (water) saturation, is the total flow rate, is the rock porosity, is the area of the cross-section in the sample volume, and is the fractional flow function of the wetting phase. Typically, is an 'S'-shaped, nonlinear function of the saturation , which characterizes the relative mobilities of the two phases:
where and denote the wetting and non-wetting phase mobilities. and denote the relative permeability functions of each phase and and represent the phase viscosities.
Assumptions
The Buckley–Leverett equation is derived based on the following assumptions:
- Flow is linear and horizontal
- Both wetting and non-wetting phases are incompressible
- Immiscible phases
- Negligible capillary pressure effects (this implies that the pressures of the two phases are equal)
- Negligible gravitational forces
General solution
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 , where is the characteristic velocity given above.
See also
References
- ^ S.E. Buckley and M.C. Leverett (1942). "Mechanism of fluid displacements in sands". Transactions of the AIME (146): 107–116.
External links