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Plasma separation by filtration is performed through high permeability membranes.
Open image in new window Fig. 10 Dynamic displacement experiment through high permeability core sample.
Previous research showed that these materials can reduce the flow through high permeability zones by selectively altering the viscosity (Golombok and van der Wijst 2013; Smeets and Golombok 2010).
The shear thinning nature of these fluids is favorable for injectivity but it can increase the unfavorable effect of preferential flow through high permeability zones (AlSofi et al. 2009; Delshad et al. 2008; Silva et al. 2012).
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It is more likely, even in highly overpressured settings, that lateral flow through higher permeability strata toward the basin margins would be the dominant fluid migration route at depth (Deming 1994b), although this lateral flow is itself associated with long travel times (e.g., millions of years or longer; Kreitler 1989; Stueber and Walter 1991; Thornton and Wilson 2007).
First, we discuss the former effect of pore pressure increase, associated with fluid infiltration from the surface through high-permeability pathway (e.g., fault).
Problems of poor volumetric sweep efficiency, gas channeling through high-permeability streaks, and gravity override are frequent (Hanssen et al. 1994).
Foam injection has advantages over simple gas injection, and it is demonstrated that the use of foam can mitigate gas channeling, improve apparent gas density and hinder gas escape through high-permeability zones to achieve good oil recovery (Julio and Emanuel 1989; Huh and Rossen 2008; Lee et al. 1991; Schramm and Wassmuth 1994).
Some PCE, however, passed quickly through this layer and subsequently through the high permeability sand below it.
Modelling results showed that despite the fact that groundwater heads were all below the streambed and that an unsaturated zone was present beneath the streambed, the stream and the aquifer become laterally connected within several hours of flow onset through a high permeability preferential path in the streambank.
Figure 10 shows the dynamic displacement experiment through a high permeability (750 mD) core sample.
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