Introduction and background

A large fraction of original oil in place (OOIP) remains trapped in the reservoir after both primary and secondary recoveries. The latter necessitates the need for enhanced oil recovery (EOR) techniques to improve the oil recovery in an economic way under certain market and technology conditions (Lake 1989). Different EOR techniques are being used including solvents, chemical flooding, thermal methods, and others (Al-Shalabi et al. 2015; Al-Shalabi and Sepehrnoori 2016, 2017).

Polymer flooding is a widely used chemical EOR technique that has been studied and practiced for many years (Chang 1978). In this technique, polymers are added to the water in order to increase its viscosity and hence, improve water sweep efficiency through decreasing the mobility ratio between the displacing fluid (water) and the displaced fluid (oil). Consequently, this viscous water dampens viscous fingering effects and results in better volumetric sweep efficiency (Sorbie 1991). This paper discusses in particular, the application of “biopolymer” flooding as an EOR technique on oil recovery from “carbonate” reservoirs under “harsh” conditions.

Carbonates under harsh conditions

More than half of the world’s hydrocarbon proven reserves are present in carbonate reservoirs. The majority of these reservoirs have a complex nature that leads to low oil recovery (about 30% in average) including both primary and secondary recovery stages. The complexity of these reservoirs includes high temperature (above 80 °C), high formation water salinity (TDS above 60,000 ppm), presence of divalent cations (hardness), low permeability (less than 100 mD), and the wetting nature (about 90% are mixed-to-oil wet) (Austad et al. 2008; Chandrasekhar and Mohanty 2013; Adegbite et al. 2018; Diab and Al-Shalabi 2019). The low recovery in carbonate reservoirs assures higher potential for enhanced oil recovery (EOR).

Biopolymer types

Two main types of polymers are generally used for EOR purposes including synthetically produced partially hydrolyzed polyacrylamides (HPAM) and biologically produced polysaccharides such as Xanthan biopolymers. Polyacrylamides have long molecules with small effective diameters, which results in a high sensitivity to mechanical degradation and consequent viscosity reduction. In addition, polyacrylamides are sensitive to saline solutions where in high salinity water, polymer molecules tend to curl up and lose their viscosity-building capability.

On the other hand, Xanthan polymers are more tolerant to mechanical shear and saline conditions, but they are very sensitive to biological degradation. Xanthan polymers are not retained on rock surfaces whereas polyacrylamides are subjected to retention, which causes reduction in rock permeability. Both polymers are unstable in high temperature conditions and oxidation by dissolved oxygen in the injected water (Green and Willhite 1998; Delamaide 2018). Promising biopolymers include Scleroglucan and Schizophyllan biopolymers, which have many similarities to Xanthan. Pu et al. (2017) reported different eco-friendly and tough biopolymers as opposed to synthetic polymers including Scleroglucan, HEC, CMC, Welan gum, Guar Gum, Schizophyllan, Mushroom polysaccharides Cellulose, and Lignin.

The main challenge with biopolymers is the poor filterability and plugging during flow in the porous media. This plugging problem is due to the presence of organic material or microgels (Carter et al. 1980). Kohler and Chauveteau (1981) stated that a potential polymer should be qualified through corefloods with low polymer retention (< 84 μg/g of rock) and less pore volumes to achieve a steady state pressure drop (2–3 PVs).

Biopolymer applications

Several applications have been reported for biopolymers by which they improve volumetric sweep efficiency beyond conventional waterflooding. These applications include improving oil fractional flow, reduction mobility ratio, diverting water to unswept regions of the reservoir, and improving vertical sweep efficiency through conformance control (Needham and Doe 1987; Huh and Pope 2008; Qi et al. 2017; Erincik et al. 2018; Azad and Trivedi 2019).

Biopolymer screening studies

Several factors affect the performance of polymer flooding including characteristic of polymer solution itself, technical, economical, and reservoir conditions. Characteristics of polymer solution include but not limited to polymer molecular weight, polymer concentration, degree of hydrolysis, viscoelastic properties of the polymer solution, salinity, and pH of make-up water solution. Better sweep efficiency is usually achievable with a combination of low salinity, high molecular weight, and high concentration of polymers. Other technical, economical, and reservoir factors include injectivity problems, shear dependence behavior of polymers, polymer retention/adsorption, connate water salinity, pH, rock wettability, reservoir temperature, oil viscosity, and amount of mobile oil saturation left after conventional waterflooding (Sorbie 1991; Green and Willhite 1998). Polymer retention affects the economics as well as the performance of polymer. Initial rock wettability state was found to affect polymer adsorption. Usually, in intermediate-wet reservoirs, significant portions of rock surface are occupied by crude oil components, which reduce the adsorption sites available for polymers. Hence, in water-wet reservoirs, polymer adsorption is more pronounced which results in a poor sweep efficiency (Chiappa et al. 1999). As most of carbonates are mixed-to-oil wet, then polymer adsorption is expected to be lower than that of sandstones.

Biopolymer corefloods

Polymer screening studies are followed by corefloods to qualify a polymer for EOR. The Polymer corefloods have been mainly conducted on sandstones with a limited application on carbonates where the promising results motivated researchers to perform further studies (Manrique et al. 2006). The corefloods conducted on carbonates are few with temperature up to 109 °C and salinity of 343,000 ppm using mainly synthetic polymers as opposed to biopolymers (Al-Hashim et al. 1996; Bennetzen et al. 2014; Han et al. 2014; and Zhu et al. 2015).

Biopolymer numerical modeling

After conducting both polymer screening studies and corefloods, the properties of these qualified polymers are needed as an input in a numerical simulator for history matching as well as upscaling of these corefloods to field-scale studies. The simulations are later used to optimize polymer flooding through running sensitivity studies on polymer concentration, injection rates, and other factors that affect the economics of this process (Lee 2015).

Bondor et al. (1972) introduced rheological behavior modeling of polymers with an emphasis on polymer injectivity and near wellbore effect. The authors included the non-ideal mixing of polymer and water, polymer adsorption, and permeability reduction due to polymer adsorption in their simulator. Since that time, several numerical studies have been performed to highlight the effect of polymer flooding on enhancing oil recovery as well as optimizing this process. A summary of the basic functions in a polymer module was provided by Goudarzi et al. (2013), which include models for polymer viscosity as a function of both concentration and shear rate, polymer adsorption, permeability reduction, inaccessible pore volume, salinity, and hardness. One should note that very few numerical studies investigated the effect on polymer flooding in carbonates under harsh conditions.

Therefore, this work focuses on the numerical investigation of biopolymer injection in carbonate reservoirs under harsh conditions. The focus of this work is mainly on the core-scale simulations, which is considered the first step towards field-scale studies.

Experimental data

This work includes predictions of Schizophyllan biopolymer effect on oil recovery from carbonate cores. The study starts with history matching a waterflooding process on a Middle Eastern carbonate cores. The latter is followed by modeling the Schizophyllan biopolymer properties as reported from the screening studies by Quadri (2015). Afterwards, predictions of oil recovery by this biopolymer are performed in both secondary and tertiary modes of injection. The simulator used in this work is UTCHEM (Technical Documentation 2000), which is a 3D multiphase-flow, transport, and chemical-flooding simulator developed at the University of Texas at Austin.

Quadri (2015) presented a screening study for Schizophyllan biopolymer to be used in Middle Eastern carbonate reservoirs with high temperature and high salinity conditions. The latter polymer showed shear thinning behavior with excellent thermal stability (at 120 °C) and salt tolerance (up to 200,000 ppm). In addition, Schizophyllan showed good injectivity on cores with permeability higher than 30 mD. Dynamic adsorption was also discussed on cores of different permeabilities (3–163 mD) and was found to be low within 7–48 μg/g of rock. Later, Li (2015) conducted several corefloods to highlight the injectivity of this Schizophyllan biopolymer. Moreover, a polymer concentration of 200 ppm was used in these experiments. The current study utilizes polymer solution properties through the screening studies conducted by Quadri (2015) as well as rock and fluid properties through corefloods conducted by Li (2015). The latter data are used to numerically investigate the effect of this biopolymer with the proposed concentration (200 ppm) on enhancing oil recovery for the target reservoirs in the Middle East.

One of the corefloods conducted by Li (2015) was utilized to get rock and fluid data as well as relative permeability and capillary pressure curves for formation waterflooding through history matching using UTCHEM. In this coreflood, the core was flooded with formation water at reservoir conditions (248 °F and 3000 psig). The core plug used has an average porosity of 13.12% and an average liquid permeability of 30.5 mD. More details about this coreflood including rock and fluid properties are listed in Tables 1 and 2. More information about the screening work of the Schizophyllan biopolymer used can be found elsewhere (Quadri 2015).

Table 1 Rock petrophysical properties
Table 2 Fluid properties

Simulation model

A 2D Cartesian grid was used with 10 × 1 × 10 gridblocks to simulate the heterogeneous carbonate core plug for the coreflood. The simulation model was created horizontally to match the coreflood that was run in the lab. The heterogeneity was considered by generating permeability distribution with an arithmetic mean of 30.5 mD and Dykstra Parson’s coefficient (VDP) of 0.85. The arithmetic mean value matches the core’s average permeability. Also, the latter VDP was selected based on the experiences in dealing with carbonate cores from the same formation (Al-Shalabi 2014a, 2014b; Al-Shalabi et al. 2014a, 2014b). A spherical variogram and a lognormal permeability distribution were used. The spherical variogram was utilized which represents a medium level of heterogeneity between Gaussian and Exponential variograms. Equal correlation lengths in x- and y-directions were used; however, a lower value was assigned in the z-direction. This resulted in generating horizontal layers of different permeabilities as shown in Fig. 1. The latter horizontal layers aided in capturing the breakthrough of water observed during the experimental coreflood. It is worth mentioning that the number of gridblocks and the heterogeneity distribution used were chosen in a way to capture the physics and mimic the heterogeneity of the actual core where several grid sensitivities were performed. The simulation model has two vertical wells including an injector and a producer. More details about the simulation model are listed in Table 3.

Fig. 1
figure 1

Simulation model used in different runs with heterogeneous permeability

Table 3 Heterogeneous core model data

The sections below discuss formation water cycle history matching, biopolymer properties modeling, analytical determination of optimum biopolymer concentration, both fractional flow and mobility ratio analyses, and numerical core-scale simulations.

Results and discussion

Waterflooding history matching (secondary injection)

The experimental data of the formation water coreflood, including pressure drop and oil recovery, were analyzed to find the relative permeability curves. Darcy’s law and the stabilized pressure drop were used to determine the water endpoint relative permeability (krw*) and the oil endpoint relative permeability (kro*) was provided in the experimental work. The latter two parameters were used in Corey’s correlation along with Corey’s oil and water exponents (no and nw) to estimate the relative permeability curves for the formation water injection cycle. Moreover, Brooks-Corey correlation for imbibition capillary pressure of mixed-wet rocks was used to estimate the capillary pressure curve for this injection cycle (Brooks and Corey 1966).

One should note that the final selection of Corey’s exponents and capillary pressure parameters was based on the best history matching of both oil recovery and pressure drop experimental data for the formation water cycle. Endpoint relative permeability data analysis as well as a summary of relative permeability and capillary pressure parameters for the formation water injection cycle are listed in Tables 4 and 5, respectively.

Table 4 Endpoint relative permeability data analysis (formation water cycle)
Table 5 Summary of relative permeability and capillary pressure parameters (formation water cycle)

Relative permeability and capillary pressure curves used in history matching are depicted in Figs. 2 and 3, respectively. Both relative permeability and capillary pressure curves are consistent as they show a mixed-to-weakly water wet carbonate rock.

Fig. 2
figure 2

Relative permeablity curves (formation water cycle)

Fig. 3
figure 3

Capillary pressure curve (formation water cycle)

The latter curves resulted in a good history match for both oil recovery and pressure drop data as shown in Figs. 4 and 5, respectively. As seen from these figures, both heterogeneity and capillary pressure effects were considered in the history matching process. It is worth to highlight that a reasonable history match was only obtained after considering the contributions of both heterogeneity and capillary pressure.

Fig. 4
figure 4

Cumulative oil recovery match (formation water cycle)

Fig. 5
figure 5

Overall pressure drop match (formation water cycle)

Biopolymer properties modeling

In this section, modeling of the different properties of the Schizophyllan biopolymer is discussed. It is worth mentioning that the equations used below are usually applicable for both synthetic- and bio-polymers; however, the input parameters for these equations are different and usually they are obtained from the screening studies in the lab. In this work, the screening tests by Quadri (2015) were utilized.

Polymer viscosity, salinity, and concentration

Polymer viscosity is important in mobility control of the injected polymer solution. Polymer viscosity increases with increasing polymer concentration whereas it decreases with increasing the solution salinity. The dependence of polymer solution viscosity at zero shear rate (\(\mu_{p}^{0}\)) on both polymer concentration and salinity are modeled using the Flory–Huggins equation (Flory 1953):

$$\mu_{p}^{0} = \mu_{w} \left( {1 + \left( {A_{p1} C_{p} + A_{p2} C_{p}^{2} + A_{p3} C_{p}^{3} } \right)C_{sep}^{{S_{p} }} } \right),$$
(1)

where \(\mu_{w}^{{}}\) is the water viscosity in cP, Cp is the polymer concentration in water, Ap1, Ap2, Ap3, and Sp are fitting constants, and Csep is the effective polymer salinity. It should be noted that the units for the parameters inside the parentheses must be dimensionless so that the unit for \(\mu_{p}^{0}\) be the same as \(\mu_{w}^{{}}\). Csep captures the dependency of polymer viscosity on both salinity and hardness, and is defined as:

$$C_{{{\text{sep}}}} = \frac{{C_{51} + \left( {\beta_{p} - 1} \right)C_{61} }}{{C_{11} }},$$
(2)

where C51 and C61 are the anion and the divalent concentrations in the aqueous solution in meq/mL, respectively. C11 is the water concentrations in the aqueous phase and it is expressed as water volume fraction in the aqueous phase. βp is measured in the laboratory, with typical value of about 10. In Csep calculation, usually the total amount of chloride ion is considered because NaCl is the most common salt in the water used and the current technology cannot describe the effect of every single ion on chemical EOR. Also, βp was assumed to be equal to 1, which means the hardness effect on polymer solution was ignored. Moreover, C11 was assumed to be 1.

It is worth mentioning that Sp is the slope of \(\frac{{\mu_{{\text{p}}}^{{0}} - \mu_{{\text{w}}} }}{{\mu_{{\text{w}}} }}\) versus Csep on a log–log plot (Fig. 6). Figure 7 shows the viscosity experimental data as well as data matching using Eq. (1). The results show that Ap1, Ap2, and Ap3 are 2929, 44,528, 44,528, respectively, Csep is 2.3 meq/mL, \(\mu_{w}^{{}}\) is 1.25 cP, and Sp is − 0.33.

Fig. 6
figure 6

Calcualtion of Sp

Fig. 7
figure 7

Polymer viscosity versus polymer concentration at 25 °C and 10 s−1 shear rate

Shear effect

Biopolymer solutions are pseudoplastic or shear thinning fluids, which means that their viscosity decreases with increasing the shear rate. The shear effect on polymer viscosity is modeled using Meter’s equation (Meter and Bird 1964):

$$\mu_{{\text{p}}} = \mu_{{\text{w}}} + \frac{{\mu_{{\text{p}}}^{{0}} - \mu_{{\text{w}}} }}{{1 + \left( {\frac{{\dot{\gamma }_{{{\text{eq}}}} }}{{\dot{\gamma }_{1/2} }}} \right)^{{\left( {P_{\alpha } - 1} \right)}} }} ,$$
(3)

where Pα is an empirical parameter that is obtained by matching laboratory-measured viscosity data, \(\mu_{{\text{p}}}^{0}\) is the limiting viscosity at low shear limit (approaching zero), \(\mu_{{\text{w}}}\) is the water viscosity which is the limiting viscosity at high shear limit (approaching infinity), and \(\dot{\gamma }_{1/2}\) is the shear rate at which polymer viscosity is the average of the \(\mu_{p}^{0}\) and \(\mu_{w}^{{}}\). The equivalent shear rate (\(\dot{\gamma }_{eq}\)) is defined using Cannella equation (Cannella et al. 1988):

$$\dot{\gamma }_{eq} = \frac{{\dot{\gamma }_{c} \left| {u_{l} } \right|}}{{\sqrt {\overline{k}k_{rl} \emptyset S_{l} } }}{ },$$
(4)
$$\dot{\gamma }_{c} = 3.97 C{ },$$
(5)

where u is Darcy’s velocity in ft/day, \(\overline{k}\) is the formation average permeability in Darcy, and C is the shear rate coefficient that depends on permeability and porosity. In this work, C was assumed as 2.55 as the reported C value for Scleroglucan is around 2 to 3.1 (Kulawardana et al. 2012). Figure 8 depicts the shear rate effect on polymer viscosity where the results show that Pα is 1.7, \(\dot{\gamma }_{c}\) is 10.12, and \(\dot{\gamma }_{1/2}\) is 0.173.

Fig. 8
figure 8

Shear effect on polymer viscosity at 25 °C

One should note that polymer concentration and shear rate effects on Schizophyllan biopolymer viscosity are presented at 25 °C in Figs. 7 and 8, respectively. This is because Quadri (2015) observed a negligible effect of temperature on this biopolymer through his temperature sweep tests.

Polymer adsorption

Polymer retention could be either dynamic (mechanical trapping and hydrodynamic trapping) or static (adsorption). Mechanical trapping occurs due to the use of polymers with sizes greater than the pores of the porous medium and it happens during polymer flow. The latter could be controlled by using polymers in high permeability medium or pre-shearing of polymer solution. Hydrodynamic trapping occurs also during polymer flow in the medium where the polymer retention depends on the flow rate. Usually, this effect is negligible especially at field-applications. Adsorption is the most important mechanism, which occurs due to the interaction between polymer molecules and the solid rock surface. Adsorption depends on the surface area exposed to the polymer solution. Researchers usually use the term polymer retention to describe polymer loss or they simply use the term adsorption (Sheng 2011).

The Langmuir isotherm was used to describe adsorption (Lakatos et al. 1979):

$$\hat{C}_{p} = min\left( {C_{p} , \frac{{a_{p} \left( {C_{p} - \hat{C}_{p} } \right)}}{{1 + b_{p} \left( {C_{p} - \hat{C}_{p} } \right)}}} \right){ },$$
(6)

where Cp is the injected polymer concentration, \(\overset{\lower0.5em\hbox{$\smash{\scriptscriptstyle\frown}$}}{C}_{p}\) is the adsorbed polymer concentration, \(C_{p} - \hat{C}_{p}\) is the equilibrium concentration in the rock-polymer solution system, ap and bp are empirical constants. It should be noted that both Cp and \(\overset{\lower0.5em\hbox{$\smash{\scriptscriptstyle\frown}$}}{C}_{p}\) have the same units, and bp has the reciprocal unit of Cp. Also, ap is dimensionless and defined as:

$$a_{{\text{p}}} = \left( {a_{{{\text{p1}}}} - a_{{{\text{p2}}}} C_{{{\text{sep}}}} } \right)\left( {\frac{{k_{{{\text{ref}}}} }}{k}} \right)^{0.5}$$
(7)

where ap1 and ap2 are fitting parameters, Csep is the effective salinity, k is the formation permeability, and kref is the reference permeability of the rock used in the laboratory measurement for adsorption. It must be noted that Langmuir model assumes equilibrium conditions, instantaneous polymer adsorption as well as reversible adsorption in terms of polymer concentration. Polymer adsorption depends on polymer type, salinity, and rock surface. Figure 9 shows polymer adsorption modeling using the simulator where ap1, ap2, and bp obtained through data matching are 1.857, 0, and 100, respectively. The experimentally reported adsorption is 6.9 μg/g of rock using a 200 ppm polymer concentration and a 30.5 mD reference core permeability.

Fig. 9
figure 9

Polymer adsorption modeling using UTCHEM at 120 °C

Permeability reduction

There is a noticeable formation permeability change during polymer flooding compared to waterflooding. This permeability reduction is due to polymer adsorption. The permeability reduction factor (Fkr) is defined as:

$$F_{kr} = \frac{{k_{eff,w} }}{{k_{eff,p} }}{ },$$
(8)

where keff,w is the effective permeability when rock is flooded by water and keff,p is the effective permeability when the rock is flooded with polymer solution. This factor is modeled using the following equations:

$$F_{{{\text{kr}}}} = 1 + \left( {F_{{\text{kr,max}}} - 1} \right)\left( {\frac{{b_{{{\text{kr}}}} C_{{\text{p}}} }}{{1 + b_{{{\text{kr}}}} C_{{\text{p}}} }}} \right)$$
(9)
$$F_{{\text{kr,max}}} = \min \left\{ {\left( {1 - \frac{{c_{{{\text{kr}}}} \left( {A_{{{\text{p1}}}} C_{{{\text{sep}}}}^{{{\text{S}}_{{\text{p}}} }} } \right)^{1/3} }}{{\sqrt {\frac{k}{\emptyset }} }}} \right)^{ - 4} ,10} \right\}$$
(10)

where bkr and ckr are input parameters derived from data matching, Ap1 is the constant in Eq. (1), Csep is calculated using Eq. (2), and Sp is from Fig. 6. It should be noted that the term bkrCp must be dimensionless, similarly is the case for Fkr,max, which has an assumed empirical value of 10. Permeability reduction was modeled as seen in Fig. 10 through data matching using bkr, and ckr values of 1000 and 0.00883, respectively.

Fig. 10
figure 10

Permeability reduction modeling using UTCHEM at 120 °C

As the polymer adsorption process can be considered sometimes irreversible due to the prolonged pore volumes of water injection to restore the initial permeability, the residual resistance factor (Frr) was introduced. The latter parameter is defined as the ratio of water mobility before polymer flow to water mobility after polymer flow. However, Frr does not take into account the increase in viscosity caused by polymer flooding. Hence, the resistance factor term (Fr) was introduced, which is defined as the ratio of water mobility during water flow to polymer mobility during polymer flow. It should be noted that viscosity increase and permeability reduction due to polymer flooding is only applicable to the water phase by modifying the polymer viscosity by Fkr.

Inaccessible pore volume (IPV)

It refers to the fraction of pore volume where the radii of the pores are smaller than the size of polymer particles, especially when polymers with high molecular weight are used. These pores are usually filled with irreducible water. IPV has a positive effect on sweep efficiency of polymer solutions and hence, better oil recovery due to boosting the advancement of the polymer solution front. Moreover, the IPV is useful from an economical point of view where it results in less contact between rock surface and polymer solution and hence, less polymer adsorption/retention. The only disadvantage of IPV is when these inaccessible pores have movable oil droplets. In this situation, polymer solutions will not be able to contact these oil droplets and that oil remains as residual oil saturation (Dawson and Lantz 1971). IPV is modeled by multiplying the porosity in the conservation equation for polymer by an input parameter (EPHI4) defined as the effective porosity. EPHI4 is 1 – IPV and assumed to be 1.0 in this study.

A summary of the parameters used in modeling the properties of the Schizophyllan biopolymer using the UTCHEM simulator is listed in Table 6. More details about modeling of polymer properties can be found elsewhere (Sheng 2011).

Table 6 A summary of the parameters used in modeling the properties of the Schizophyllan biopolymer using the UTCHEM simulator

Optimum biopolymer concentration analysis

The optimum concentration of the Schizophyllan biopolymer was determined using an analytical method, which is based on achieving the minimum total relative mobility of oil and water phases during the formation water injection cycle. The total relative mobility (\(\lambda_{{{\text{rT}}}}\)) is defined as:

$$\lambda_{{{\text{rt}}}} = \lambda_{{{\text{rw}}}} + \lambda_{{{\text{ro}}}} = \frac{{k_{{{\text{rw}}}} }}{{\mu_{{\text{w}}} }} + \frac{{k_{{{\text{ro}}}} }}{{\mu_{o} }}$$
(11)

where \(\lambda_{{{\text{rw}}}}\) and \(\lambda_{{{\text{ro}}}}\) are the relative mobility of water and oil phases, respectively. Figure 11 shows the calculated total relative mobility for water and oil phases where the minimum mobility was determined. Afterwards, the designed polymer viscosity is the inverse of this minimum total relative mobility as follows:

$$\mu_{{\text{p}}} = \frac{1}{{\lambda_{{{\text{rT}}, \min }} }}.$$
(12)
Fig. 11
figure 11

Totall relative mobility of water and oil phaes during formation water injection

The obtained desired polymer viscosity of 10 cP was used in Fig. 12 to determine the required optimum polymer concentration. The analysis shows that the optimum polymer concentration is 200 ppm, which results in a polymer viscosity of 10 cP. The latter is consistent with the polymer concentration used in Li (2015) studies.

Fig. 12
figure 12

Optimum polymer concnetration design at 120 °C and 10 s−1 shear rate

Fractional flow and mobility ratio analyses

In this subsection, both fractional flow and mobility ratio analyses for biopolymer flooding are discussed.

Fractional flow analysis

Several assumption were considered in the fractional flow analysis including no dispersion, uniform adsorption of polymer on rock, one-dimensional linear flow, continuous injection of polymer, no chemical reactions, polymer only in aqueous phase (does not partition to oil), polymer viscosity depends on polymer concentration, isothermal reservoir, and local equilibrium adsorption of polymer on rock.

Two fractional flow curves were considered. First, the water–oil fractional flow equation for horizontal flow and neglecting capillary pressure effect:

$$f_{{\text{w}}} = \frac{1}{{1 + \frac{{k_{{{\text{ro}}}} \mu_{{\text{w}}} }}{{k_{{{\text{rw}}}} \mu_{{\text{o}}} }}}} .$$
(13)

Second, the polymer-oil fractional flow equation for horizontal flow and neglecting capillary pressure effect:

$$f_{{\text{p}}} = \frac{1}{{1 + \frac{{F_{{{\text{kr}}}} k_{{{\text{ro}}}} \mu_{{\text{p}}} }}{{k_{{{\text{rw}}}} \mu_{{\text{o}}} }}}}.$$
(14)

It is worth mentioning that the fractional flow analysis was conducted for the secondary mode of injection. The frontal advance loss (Dp) in cc polymer/cc pore volume was calculated using the following equation:

$$D_{p} = \frac{{w_{ps} \rho_{s} \left( {1 - \emptyset } \right)}}{{\emptyset C_{p} }}{ },$$
(15)

where wps is the mass concentration of adsorbed polymer and \(\rho_{{\text{s}}}\) is the rock density (2.71 g/cc). Afterwards, the intercept of the water saturation axis (\(\phi_{{\text{e}}} - D_{{\text{p}}}\)) was found and a tangent was drawn to polymer fractional flow curve resulting in (Sw*, fp*) values and the intersection of this tangent with the water–oil fractional flow curve, results in the water shock (oil bank) saturation and fractional flow values (SwB, fwB). The parameter \(\phi_{{\text{e}}}\) is defined as follows:

$$\emptyset_{e} = \frac{{\emptyset_{{{\text{IPV}}}} }}{\emptyset }$$
(16)

It should be noted that \(\phi_{{\text{e}}}\) is zero in this study as IPV is zero. Water saturation at breakthrough and the corresponding water fractional flow value were considered in the analysis (Swbt, fwbt). The fractional flow analysis is shown in Fig. 13 where a more favorable fractional flow curve was obtained using polymer flooding as opposed to conventional formation water flooding.

Fig. 13
figure 13

Fractional flow curves of waterflood and polymer flood in the secondary mode of injection

This finding is consistent with Fig. 14a–d showing water cut, oil cut, dimensionless cumulative oil recovery, and saturation profile at 0.2 PV using fractional flow calculations. The positive response of polymer flooding is clearly seen in the latter figures where a piston like displacement front was obtained using polymer flooding to the extreme of having one shock instead of the conventional two shocks solution. It should be noted that this solution was obtained under the assumptions made in this study.

Fig. 14
figure 14

Fractional flow calculations of water and polymer floods in the secondary injection

Mobility ratio analysis

This analysis is essential in designing a polymer flooding process for a certain field. One should make sure that the mobility ratio is less than 1 for achieving a good mobility control by polymer and avoiding water fingering through the oil as well as early water breakthrough. In this work, the endpoint mobility ratio was calculated before and after polymer flooding using Eqs. (17) and (18), respectively.

$$M_{{\text{w/o}}}^{*} = \frac{{k_{{{\text{rw}}}}^{*} }}{{k_{{{\text{ro}}}}^{*} }}\frac{{\mu_{{\text{o}}} }}{{\mu_{{\text{w}}} }},$$
(17)
$$M_{{\text{p/o}}}^{*} = \frac{{k_{{{\text{rw}}}}^{*} }}{{F_{{{\text{kr}}}} k_{{{\text{ro}}}}^{*} }} \frac{{\mu_{{\text{o}}} }}{{\mu_{{\text{p}}} }}.$$
(18)

The results show that the endpoint mobility ratio during formation waterflooding (\(M_{{\text{w/o}}}^{*}\)) is 1.29 whereas the endpoint mobility rate during polymer flooding (\(M_{{\text{p/o}}}^{*}\)) is 0.013. The latter results indicate a slightly favorable endpoint mobility ratio during the formation waterflooding; however, this mobility ratio was further improved using the Schizophyllan biopolymer. This finding further indicates the capability of this biopolymer on improving volumetric sweep efficiency in carbonate reservoirs with harsh conditions of high temperature, high salinity, and low permeability.

Fractional flow and mobility ratio analyses give an indication about the performance of the polymer flooding technique; however, capillary pressure and heterogeneity effects are not captured. Therefore, the next subsections discuss the predictions of polymer flooding in secondary and tertiary modes of injection using the UTCHEM simulator with comparison between these two injection modes.

Biopolymer flooding prediction (secondary injection)

The prediction of biopolymer injection in the secondary mode of injection was investigated. Figure 15 shows cumulative oil recovery prediction, and Fig. 16 depicts total pressure drop prediction.

Fig. 15
figure 15

Cumulative oil recovery (polymer flooding-secondary injection mode)

Fig. 16
figure 16

Total pressure drop (polymer flooding-secondary injection mode)

The figures show two polymer concentrations include 200 and 800 ppm. The reason behind using an 800 ppm polymer concentration is the small-scale heterogeneity of the core model, which resulted in higher effective shearing effects and hence, lowers polymer viscosity than the desired polymer viscosity (10 cP). Figure 17 shows the polymer viscosity corresponding to polymer concentration of 200 ppm whereas Fig. 18 shows that the use of 800 ppm polymer concentration achieves the desired polymer viscosity of 10 cP. In these two figures, there are zones with high viscosity, which is related to their corresponding high permeability. This can be crosschecked with the permeability model, which was previously shown in Fig. 1. Zones with high permeability experience low effective shear rate, and consequently, high polymer viscosity, which is consistent with Eqs. (3) and (4).

Fig. 17
figure 17

Polymer viscoisty at 200 ppm polymer concentration (polymer flooding-secondary injection mode)

Fig. 18
figure 18

Polymer viscoisty at 800 ppm polymer concentration (polymer flooding-secondary injection mode)

The higher polymer viscosity results in better sweep efficiency as shown in the 3D saturation maps in Figs. 19 and 20.

Fig. 19
figure 19

Water saturation map at 3 PV of formation water injection (formation waterflooding-secondary injection mode)

Fig. 20
figure 20

Water saturation map at 3 PV of polymer injection using 800 ppm polymer concentration (polymer flooding-secondary injection mode)

Figure 19 shows the water saturation in the core model as a result of formation water flooding at 3 pore volumes of water injection where it is clear that zones with high permeability have better sweep compared to others. On the other hand, Fig. 20 shows the improvement in sweep efficiency as a result of polymer injection in the secondary mode at 3 pore volumes of injection. The improvement is related to the decrease in water mobility by decreasing effective water permeability and increasing water viscosity by using the Schizophyllan biopolymer at concentration of 800 ppm. The results of secondary biopolymer injection are also listed in Table 7.

Table 7 Prediction of secondary polymer flooding using the UTCHEM simulator

Both Fig. 15 and Table 7 show that polymer flooding with 800 ppm concentration results in better oil recovery compared to the 200 ppm polymer concentration. Moreover, biopolymer flooding is more favorable as opposed to conventional formation waterflooding resulting in incremental oil recovery of about 1.36 and 2.26% OOIP for 200 and 800 ppm polymer concentrations, respectively. In addition, it is worth mentioning that the injectivity of polymer is lower than that of waterflood due to the increase of pressure drop, which is about 2–5 times higher than that of the waterflood when using 200 and 800 ppm polymer concentrations, respectively (Fig. 16). It is worth mentioning that permeability, viscosity, and saturation maps are consistent in justifying the incremental oil recovery achieved by polymer flooding.

Biopolymer flooding prediction (tertiary injection)

The injection of the Schizophyllan biopolymer was also investigated in the tertiary mode of injection using UTCHEM. This mode starts with injecting formation water for about 3 pore volumes followed by polymer injection for another 3 pore volumes, which makes the total injection of 6 pore volumes. Figures 21 and 22 depict the cumulative oil recovery and the total pressure drop predictions as a result of tertiary polymer flooding.

Fig. 21
figure 21

Cumulative oil recovery (polymer flooding-teritary injection mode)

Fig. 22
figure 22

Total pressure drop (polymer flooding-tertiary injection mode)

The stabilized pressure drop during the polymer flooding indicates that there is no injectivity or plugging problems. However, it is also evident from Fig. 22 that the injectivity of polymer is lower than that of waterflood due to the increase of pressure drop, which is about 2 to 5 times higher than that of the waterflood when using 200 ppm and 800 ppm polymer concentrations, respectively. The findings are consistent with the secondary mode of injection where the 800 ppm polymer resulted in better oil recovery than the 200 ppm polymer and that the tertiary polymer injection is more favorable compared to conventional formation water injection for about 6 PVs. The incremental oil recovery using tertiary polymer flooding is about 1.38 and 2.29% OOIP for 200 and 800 ppm polymer concentration, respectively (Table 8).

Table 8 Prediction of tertiary polymer flooding using the UTCHEM simulator

Biopolymer flooding comparison (secondary vs. tertiary injections)

The results of Schizophyllan biopolymer injection in both secondary and tertiary modes of injection are shown in Table 9 as well as Fig. 23. The comparison was considered for polymer concentration of 800 ppm, which achieves the desired polymer viscosity of 10 cP needed for reduction of water mobility and improvement of oil sweep efficiency.

Table 9 Prediction of secondary vs. tertiary polymer flooding using the UTCHEM simulator
Fig. 23
figure 23

Comparison between secondary vs. tertiary polymer flooding using 800 ppm polymer concentration

The results show that in terms of cumulative oil recovery, both secondary and tertiary modes of polymer flooding are comparable as they result in about 2% incremental OOIP compared to conventional formation water injection. The latter makes sense as the biopolymer used does not have a viscoelastic effect and hence, it is not expected to decrease residual oil saturation. Nevertheless, secondary polymer injection is more favorable compared to tertiary polymer injection in terms of economics through early boosting oil production rate and achieving higher money time value. One should note that more experimental datasets are needed to further validate and generalize the results obtained in this study.

Summary and conclusions

The performance of Schizophyllan biopolymer in carbonates with high temperature, high salinity, and low permeability conditions was successfully evaluated at core-scale. The following findings can be made based on the particular experimental dataset used in this work:

  • Small-scale heterogeneity of the core is important in history matching formation water corefloods as well as in modeling polymer properties, particularly the shear effect on polymer viscosity.

  • Formation permeability, polymer viscosity, and oil saturation maps should be consistent in justifying incremental oil recovery achieved by polymer flooding.

  • The Schizophyllan biopolymer improves both displacement and volumetric sweep efficiencies through achieving favorable water fractional flow curve as well as endpoint mobility ratio compared to conventional waterflooding.

  • Schizophyllan biopolymer improves oil recovery compared to conventional waterflooding through decreasing effective water permeability as well as increasing water viscosity, and hence reducing the water phase mobility.

  • Secondary injection of Schizophyllan biopolymer is more favorable as opposed to tertiary injection due to boosting oil production rate at earlier time and hence, higher money time value.

  • An optimum concentration of 800 ppm is recommended for maintaining the desired polymer viscosity as well as achieving a minimum total relative mobility of oil and water phases.

In the future work, validation of polymer corefloods through considering different polymer datasets as well as field-scale studies will be considered to highlight the advantages of using Schizophyllan biopolymer on oil recovery from carbonate reservoirs. Moreover, sensitivity analysis as well as optimization studies will be performed.