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 can be interpreted as a way of incorporating the microscopic effects due to capillary pressure in two-phase flow into Darcy's law.

In a 1D sample (control volume), let $S(x,t)$ be the water saturation, then the Buckley–Leverett equation is

$\frac{\partial S}{\partial t} = U(S)\frac{\partial S}{\partial x}$

where

$U(S) = \frac{Q}{\phi A} \frac{\mathrm{d} f}{\mathrm{d} S}.$

$f$ is the fractional flow rate, $Q$ is the total flow, $\phi$ is porosity and $A$ is area of the cross-section in the sample volume.

Assumptions for validity

The Buckley–Leverett equation is derived for a 1D sample given

• mass conservation
• capillary pressure $p_c(S)$ is a function of water saturation $S$ only
• $\mathrm{d}p_c/\mathrm{d}S = 0$ causing the pressure gradients of the two phases to be equal.
• Flow is Linear
• Flow is Steady-State
• Formation is one Layer

General solution

The solution of the Buckley–Leverett equation has the form $S(x,t) = S(x+U(S)t)$ which means that $U(S)$ is the front velocity of the fluids at saturation $S$.

See also

• Capillary pressure
• Permeability (fluid)
• Relative permeability
• Darcy's law

References

1. S.E. Buckley and M.C. Leverett (1942). "Mechanism of fluid displacements in sands" (PDF). Transactions of the AIME (146): 107–116.

External links

• Buckley-Leverett Equation and Uses in Porous Media