Fundamentals of Fluid Flow in Porous Media
Multi-phase Saturated Rock Properties:
Phase Trapping: Bypassing
According to the Pc equation, at the same condition non-wetting phase tends to invade the larger pores because of the lower capillary pressure. This tendency leads to special trapping mechanism named bypassing. The main trapping mechanism in drainage is bypassing although during the imbibition process non-wetting phase could be trapped by bypassing mechanism but it is not the major trapping mechanism.
A reservoir rock consists of a complex network of branching and reuniting pore elements of differing sizes and geometry. Any successful analysis of the displacement process should eventually recognize this complex network. However one can begin by understanding the processes which take place in the simpler elements of the network. The mechanisms of drainage displacement and imbibition displacement are best illustrated by visualization of flow experiments in transparent capillary networks etched on glass plates. The simplest type of pore system used in such displacement studies is the pore doublet (Figure 2‑69).
Figure 2-69: Pore Doublet Model
Smaller throat is invaded first during the imbibition because of higher capillary pressure and larger throat is swept first during the drainage process.
(a) Drainage Process, No Trapping
(b) Drainage Process, Bypassing in Smaller Throat
(c) Imbibition Process, Bypassing in Larger Throat
(d) Imbibition Process, Snap-Off
(e) Imbibition Process, Snap-Off in Smaller Throat and Bypassing in Larger Throat
Figure 2‑70 illustrates the drainage and imbibition mechanisms for the pore doublet model.
Figure 2-70: Imbibition and Drainage Mechanisms in a Pore Doublet Model
The condition that bypassing happen in the larger pore during the imbibition could be found by using the capillary and viscous forces formula.