2012
DOI: 10.1190/geo2011-0068.1
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Streaming potentials at hydrocarbon reservoir conditions

Abstract: We have examined the behavior of the streaming potential under multiphase conditions, and under conditions of varying temperature and salinity, to evaluate the feasibility of using downhole streaming-potential measurements to determine fluid distributions in a reservoir. Using new insights into the pore-scale distribution of fluids and of electric charge, we found that the saturation dependence of the streaming potential coupling coefficient is important in determining the resulting streaming potential. Throug… Show more

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Cited by 29 publications
(35 citation statements)
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“…When a second fluid phase is present in the pore space, the magnitude of the streaming potential coupling coefficient becomes dependent on a number of factors including the wettability of the rock, the composition of the pore fluids, and the saturation of each phase Saunders et al, 2012). According to Saunders et al (2012), in the simplest case, the nonwetting phase is nonpolar and its flux causes no streaming current.…”
Section: The Helmholtz-smoluchowski Equation In the Steady Statementioning
confidence: 99%
See 1 more Smart Citation
“…When a second fluid phase is present in the pore space, the magnitude of the streaming potential coupling coefficient becomes dependent on a number of factors including the wettability of the rock, the composition of the pore fluids, and the saturation of each phase Saunders et al, 2012). According to Saunders et al (2012), in the simplest case, the nonwetting phase is nonpolar and its flux causes no streaming current.…”
Section: The Helmholtz-smoluchowski Equation In the Steady Statementioning
confidence: 99%
“…A number of relative streaming potential coefficient functions C i have been proposed Saunders et al, 2012), three of which are given in Figure 27. A number of relative streaming potential coefficient functions C i have been proposed Saunders et al, 2012), three of which are given in Figure 27.…”
Section: The Helmholtz-smoluchowski Equation In the Steady Statementioning
confidence: 99%
“…The best productivity occurs in the location with the highest microseismic activity. (b) Exploring the potential use of spontaneous potential to detect water encroachment (from Saunders et al 2012). The two plots represent results from a simulation of a heterogeneous reservoir model at two different times, showing water moving towards a horizontal well.…”
Section: Discussionmentioning
confidence: 99%
“…As water approaches the well (high saturation in the lower plot), but is still several tens of metres away, the SP signal increases (lower plot). Modelling and experiments by Saunders et al (2012) suggest that this method can be used for several monitoring objectives, including: early detection of a waterfront approaching a well; mapping a moving waterfront from multiple wells; identifying and tracking injected fluids during EOR processes and monitoring steam flooding.…”
Section: Discussionmentioning
confidence: 99%
“…Recent theoretical and experimental studies found that considerable signals of streaming potential, which respond to approaching water, are detectable in a production well, and the investigation distance ranges from tens of meters up to a few hundred meters (Vinogradov and Jackson, 2011). However, the measured magnitude is limited by the production rate, formation water salinity, and coupling coefficient between fluids and electric potential, among which the latter two are poorly understood (Saunders et al, 2012). These reservoir imaging techniques, even though some of them are under development, are suited only for large-scale (tens to hundreds of meters) water flooding monitoring with a low-resolution requirement.…”
Section: Introductionmentioning
confidence: 99%