SPE Journal
Volume 14,
Number 3,
September 2009,
pp. 532-542
Summary
The geometric distribution of immiscible fluid phases in fractures is not
readily accessible experimentally, so aperture-scale simulations of drainage
and imbibition in realistic fractures can provide valuable insight. We
implement a level set method for computing the location within a fracture of
the interface between two fluids controlled by capillary forces. The movement
of the interface in response to changes in capillary pressure is approximated
as quasistatic displacement. Fluid interfaces are thus constant mean curvature
surfaces, satisfying the Young-Laplace equation. We apply a progressive
quasistatic (PQS) algorithm to determine when spontaneous pore-level events
occur during fluid displacement. The algorithm captures reversible and
irreversible behavior. We illustrate the approach in two types of rough-walled
fractures. One type is a 3D crack between irregular, impermeable surfaces; the
other type is a gap between irregular 2D and 3D grain packs. We focus on the
disconnected (defending) fluid volumes and (advancing) fluid main pathway as
the geometric properties of the fracture are varied, notably aperture and the
number of contact points between the upper and lower fracture surfaces. The
curvature of the fluid/fluid interface in the plane of the fracture is often
ignored by invasion percolation simulation techniques, yet it is known to
influence strongly the fluid cluster properties. Our simulations establish the
exact position and shape of the interface in realistic fracture geometries,
from which fluid volumes, contact areas, and interface curvatures can be
obtained. This establishes a new, mechanistic basis for predicting relative
permeabilities in fractures and for evaluating transfer functions in
dual-porosity flow models.
© 2009. Society of Petroleum Engineers
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History
- Original manuscript received:
27 July 2007
- Meeting paper published:
11 November 2007
- Revised manuscript received:
18 November 2008
- Manuscript approved:
18 November 2008
- Published online:
27 July 2009
- Version of record:
28 September 2009