2013
DOI: 10.2118/154218-pa
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Four-Phase Equilibrium Calculations of Carbon Dioxide/Hydrocarbon/Water Systems With a Reduced Method

Abstract: Summary Three hydrocarbon phases can coexist at equilibrium at relatively low temperatures in many carbon dioxide (CO2) floods. The formation of an aqueous phase in contact with hydrocarbon phases is inevitable in almost all recovery processes, because of the permanent presence of water in the reservoirs either as injection fluid or as initial formation water. As the number of phases increases, flash calculations become more difficult and time-consuming. A possible approach to reduce the computa… Show more

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Cited by 30 publications
(25 citation statements)
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“…Figure 1 gives the CO 2 solubility in brine as a function of partial pressure with and without calcite. A modified Peng Robinson EOS was used to calculate the hydrocarbon and aqueous phase behavior and CO 2 dissolution following the procedure of Søreide and Whitson (1992) and Mohebbinia et al (2013). The parameters for the modified PR EOS are shown in Tables 1 and 2.…”
Section: Methodsmentioning
confidence: 99%
“…Figure 1 gives the CO 2 solubility in brine as a function of partial pressure with and without calcite. A modified Peng Robinson EOS was used to calculate the hydrocarbon and aqueous phase behavior and CO 2 dissolution following the procedure of Søreide and Whitson (1992) and Mohebbinia et al (2013). The parameters for the modified PR EOS are shown in Tables 1 and 2.…”
Section: Methodsmentioning
confidence: 99%
“…In this subsection, the significance of Equation (4) is elucidated by comparing predictions made using it with those made with a BIP value of 0.5, which is a representative value from the literature (Heidman et al, 1985;Peng and Robinson, 1976b;Tsonopoulos and Heidman, 1986;Nasrifar and Moshfeghian, 2002;Eubank et al, 1994;Mohebbinia et al, 2013;Søreide and Whitson, 1992). Equation (4) gives a much lower value of 0.242 for water with heavy nalkanes (see Table 1).…”
Section: Comparison Of the New Bips With Other Recommended Valuesmentioning
confidence: 99%
“…On the other hand, the Le Chatelier principle for geochemical reactions proposes that when a system at equilibrium experiences a change (e.g., in concentration, partial pressure, and temperature), the equilibrium shifts to counteract the imposed change and establish a new equilibrium (Le Chatelier 1884; Monk 2008). 1a through 1d compare the predicted ion production of some aqueous ions (Na þ , Ca þ2 , and HCO À 3 ) and pH values for the cases considered.…”
Section: Multiphase Reactive-transport Modeling By Use Of Utcomp-iphrmentioning
confidence: 99%