Page 37 - Hybrid Enhanced Oil Recovery Using Smart Waterflooding
P. 37

CHAPTER 2 Mechanisms of Low-Salinity and Smart Waterflood   29

          increases. Surfactants are in situ generated from the  TABLE 2.1
          residual oil at elevated pH. The study formulated a hy-  Mechanisms of Association Between Organic
          pothetical mechanism of in situ generation of surfactant  Functional Groups and Soil Minerals (Sposito,
          by pH increase and validated the mechanism with  1989)
          the coreflooding observations. The coreflooding obser-
          vations of Tang and Morrow (1999) are referred to sup-           Organic Functional Group
          plement the proposed mechanism. In the observations,  Mechanisms  Involved
          the pH increases from 8 to 10 when injecting brine is  Cation exchange  Amino, ring NH, heterocyclic N
          changed from the formation brine with 15,150 ppm                 (aromatic ring)
          TDS to the low-salinity water with 1515 ppm TDS. It is
                                                         Protonation       Amino, heterocyclic N, carbonyl
          concluded that the acid or polar components in the               carboxylate
          crude oil are saponified by the generalized reactions of
                                                         Anion exchange    Carboxylate
          Eqs. (2.1) and (2.2), and then, surfactants are in situ
          generated from the reactions. The in situ generated sur-  Water bridging  Amino, carboxylate, carbonyl,
                                                                           alcoholic OH
          factant alters wettability and reduces IFT between water
          and oil. In addition, they act as emulsifying agents to  Cation bridging  Carboxylate, amines, carbonyl,
          disperse oil into the water. In the study, it is documented      alcoholic OH
          that an additional advantage of low salinity prevents  Ligand bridging  Carboxylate
          a precipitation of the surfactant because of low concen-  Hydrogen bonding  Amino, carbonyl, carboxyl,
          tration of divalent cations. The study summarized the            phenolic OH
          following prerequisites for the successful LSWF: (1)  Van der Waals  Uncharged organic units
          acidic components in crude oil; (2) water-sensitive  interaction
          minerals; (3) initial water saturation; and (4) injecting
          low-salinity water with less than 5000 ppm.
            ðRCOOÞ C 3 H 5 þ 3NaOH/3ðRCOONaÞþ C 3 H 5 ðOHÞ 3
                  3
                                                 (2.1)  during LSWF and it influences the four adsorption mech-
                                                        anisms of organic materials. The multivalent cations at a
            2ðRCOONaÞþ CaðHCO 3 Þ /ðRCOOÞ Ca þ 2NaHCO 3  clay surface bond to polar compounds of crude oil (resin
                              2
                                      2
                                                 (2.2)
                                                        and asphaltene) forming organometallic complexes. The
                                                        adsorbed complexes on the clay surface lead to
          Multicomponent Ionic Exchange                 oil-wetness of rock surface. Simultaneously, some
          Lager, Webb, Black, Singleton, and Sorbie (2008)  organic polar compounds substitute the most labile
          reviewed the previous mechanisms and devised a new  cations and directly bond to the mineral surface. This
          mechanism to explain the experimental observations of  substitution also promotes the initial oil-wetness of the
          LSWF in sandstone reservoirs. The study carried out an  clay surface. When LSWF is applied to the oil-wet
          effluent analysis of coreflood injecting low-salinity and  sandstone rocks, the MIE occurs and replaces both
          high-salinity waters and investigated water chemistry. It  organic  polar  compounds  and  organometallic
          showed a drop of Ca 2þ  and Mg 2þ  concentrations being  complexes by uncomplexed cations on the clay surface.
          lower than their concentrations in injecting brines (Fig.  This study concluded that the replacement by MIE
          1.7). These results indicate the strong adsorption of  modifies the wettability of sandstone reservoirs toward
          Ca 2þ  and Mg 2þ  onto the rock matrix. Based on these ob-  water-wet and increases oil recovery.
          servations, a multicomponent ionic exchange (MIE)
          mechanism is proposed in sandstone. According to  Salting-In Effect
          Arnarson and Keil (2000) and Sposito (1989),organic  Salting-out or salting-in effects have been used to
          matters are possible to adhere onto clay minerals  describe the solubility of polar organic material in water
          depending on the organic function of the organic matter  as a function of salinity or ionic composition in the
          and the clay surface conditions. The eight potential  area of chemistry. RezaeiDoust, Puntervold, Strand,
          mechanisms of the adsorption exist as described in  and Austad (2009) applied this theory to explain the
          Table 2.1. The four mechanisms including cation  observations of LSWF experiments and proposed
          exchange, ligand bonding, cation bridging, and water  the salting-in effect as another mechanism of LSWF.
          briding are strongly affected by the cation exchange  In the theory, organic compounds in water are solvated
          (Fig. 2.2). It is explained that the cation exchange occurs  by the water structure, which is made by hydrogen
   32   33   34   35   36   37   38   39   40   41   42