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In [[fluid dynamics]], the '''Buckley–Leverett equation''' is a [[conservation law|conservation equation]] used to model [[two-phase flow]] in [[porous media]].<ref>{{cite journal|author=S.E. Buckley and M.C. Leverett|title=Mechanism of fluid displacements in sands|url=http://www.aimehq.org/library/books/Petroleum%20Technology,%201941,%20Vol.%20IV/T.P.%201337.pdf|journal=Transactions of the AIME|issue=146|pages=107–116|year=1942}}</ref> 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 [[fluid dynamics]], the '''Buckley–Leverett equation''' is a [[conservation law|conservation equation]] used to model [[two-phase flow]] in [[porous media]]<ref>{{cite journal|author=S.E. Buckley and M.C. Leverett|title=Mechanism of fluid displacements in sands|url=https://www.onepetro.org/journal-paper/SPE-942107-G|journal=Transactions of the AIME|issue=146|pages=107–116|year=1942}}</ref>. 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.


In a 1D sample ([[control volume]]), let <math>S(x,t)</math> be the [[water saturation]], then the Buckley–Leverett equation is
In a 1D sample ([[control volume]]), let <math>S(x,t)</math> be the [[water saturation]], then the Buckley–Leverett equation is
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<math>f</math> is the fractional flow rate, <math>Q</math> is the total flow, <math>\phi</math> is [[porosity]] and <math>A</math> is area of the cross-section in the sample volume.
<math>f</math> is the fractional flow rate, <math>Q</math> is the total flow, <math>\phi</math> is [[porosity]] and <math>A</math> is area of the cross-section in the sample volume.


==Assumptions for validity==
==Assumptions==
The Buckley–Leverett equation is derived for a 1D sample given
The Buckley–Leverett equation is derived based on the following assumptions:
* Flow is linear and horizontal
* [[Conservation of mass|mass conservation]]
* Both wetting and non-wetting phases are incompressible
* [[capillary pressure]] <math>p_c(S)</math> is a function of [[water saturation]] <math>S</math> only
* Immiscible phases
* <math>\mathrm{d}p_c/\mathrm{d}S = 0</math> causing the [[pressure gradients]] of the two phases to be equal.
* Negligible capillary pressure effects (this implies that the pressures of the two phases are equal)
* Flow is Linear
* Negligible gravitational forces
* Flow is Steady-State
* Formation is one Layer


==General solution==
==General solution==

Revision as of 05:21, 3 March 2017

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.

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

where

is the fractional flow rate, is the total flow, is porosity and is area of the cross-section in the sample volume.

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 solution of the Buckley–Leverett equation has the form which means that is the front velocity of the fluids at saturation .

See also

References

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