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The following procedure was sand packing.
Three major steps involved in preparing each porous medium included seizing the sand, packing the core holder, and determining properties of the porous medium.
Experiments were performed to investigate the pressure drops for both single and immiscible two component liquid-liquid aqueous-organic flows through the same rectangular serpentine channel with medium sand packing.
The clayey sand packing is 1.6 cm in diameter and 7 cm in length; the pore velocity is 3.6 m/day.
Sand packing method is carried out to simulate greatly varied sedimentary facies between injection and production points, permeability is controlled by particle size, and porosity is controlled by cement content and packing pressure (Pi 2010).
Possible influences on the experimental data including sand packing, measurement location, finite amplitude wave effects, unsaturated zone truncation and multiple wave mode effects are unable to explain the discrepancy.
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(3) Oil was injected into each sand pack until no more water was produced at the end of the sand packs to establish initial oil saturation.
(4) CO2 was injected into the double sand packs simultaneously when no more oil was produced at the end of each sand pack.
Table 1 Properties of three types of porous media used for emulsion flow tests Sand pack Sand size Length L, cm Diameter D, cm Area A, cm2 Permeability k, Darcy Porosity ϕ, % Sand pack A IS 12 30 40 3 7.069 0.899 31.82 Sand pack B IS 30 60 40 3 7.069 1.079 35.36 Sand pack C IS 60 70 40 3 7.060 70160 70.14.
Core flood experiment was conducted on the above sand packed core.
A matching relationship also existed in the sand packed tube displacement experiment, and plugging could occur effectively only if sand packed tubes with low permeability were used.
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