Colloids in the Aquatic Environment 1993
DOI: 10.1016/b978-1-85861-038-2.50020-6
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Water sensitivity of sandstones containing swelling and non-swelling clays

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Cited by 37 publications
(65 citation statements)
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“…Moreover, the presence of clay minerals is seen to be a key requirement for low-salinity EOR to operate. 4,[6][7][8] This is due to the role that clays play in determining the wettability state of a rock. Clay minerals and quartz grains are widely present in the pores of sandstone reservoirs, where they form surface coatings.…”
Section: Introductionmentioning
confidence: 99%
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“…Moreover, the presence of clay minerals is seen to be a key requirement for low-salinity EOR to operate. 4,[6][7][8] This is due to the role that clays play in determining the wettability state of a rock. Clay minerals and quartz grains are widely present in the pores of sandstone reservoirs, where they form surface coatings.…”
Section: Introductionmentioning
confidence: 99%
“…It has been established that the salinity and saturation of connate water, 3-5 the reservoir's initial wettability 3 along with the presence of clay minerals 6,7 and polar oil components 4 all 1 play an important role on the degree to which the injection of low-salinity water increases oil production. Moreover, the presence of clay minerals is seen to be a key requirement for low-salinity EOR to operate.…”
Section: Introductionmentioning
confidence: 99%
“…Kaolinites and illites are non-swelling clays that tend to detach from the rock surface and migrate when the colloidal conditions are conducive for release. The migrating particles can get trapped in pore throats, thus causing a reduction in permeability (Mohan et al, 1993). This is generally observed for the samples with a large fracture apertures (greater than 40 Am) (BarakaLokmane, 2002), where the values of liquid permeability are lower than the values of the gas permeability; this is explained by the presence of the clay minerals within the fracture aperture, which are responsible for the reduction of the water flow rate.…”
Section: Migration Of Clay Particlesmentioning
confidence: 94%
“…Much work has been carried out to study the formation damage in sandstone (Mungan, 1965;Khilar et al, 1983;Khilar and Fogler, 1984;Mohan et al, 1993;Rahman et al, 1995;Civan, 2000;De Lima and Niwas, 2000). The experiments conducted by Mohan et al (1993) and Mohan and Fogler (1997) have shown that the critical salt concentration (CSC) of sodium chloride needed to prevent damage is between 4 and 5 M for Stevens sandstone and 0.07 M for Berea sandstone. According to the studies reported above, the brine used in the experiments was 9% NaCl brine, with a density of 1.067 g/cm 3 and a viscosity at 20 jC of 1.31 cP.…”
Section: Determination Of the Hydraulic And Pneumatic Parametersmentioning
confidence: 99%
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