Investigation of the effect of diethylene triamine pentaacetic acid chelating agent as an enhanced oil recovery fluid on wettability alteration of sandstone rocks

  • PARHIZGAR KERADEH Mahsa ,
  • TABATABAEI-NEZHAD Seyyed Alireza , *
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  • Faculty of Petroleum and Natural Gas Engineering, Sahand University of Technology, Tabriz 51335-1996, Iran

Received date: 2022-10-09

  Revised date: 2023-04-15

  Online published: 2023-06-21

Abstract

This study used the diethylene triamine pentaacetic acid (DTPA)-seawater (SW) system to modify the sandstone rock wettability and enhance oil recovery. The investigation involved conducting wettability measurement, Zeta potential measurement, and spontaneous imbibition experiment. The introduction of 5% DTPA-SW solution resulted in a significant decrease in the rock-oil contact angle from 143° to 23°, along with a reduction in the Zeta potential from −2.29 mV to −13.06 mV, thereby altering the rock surface charge and shifting its wettability from an oil-wet state to a strongly water-wet state. The presence or absence of potential determining ions (Ca2+, Mg2+, SO42−) in the solution did not impact the effectiveness of DTPA in changing the rock wettability. However, by tripling the concentration of these ions in the solution, the performance of 5% DTPA-SW solution in changing wettability was impaired. Additionally, spontaneous imbibition tests demonstrated that the 5% DTPA-SW solution led to an increase in oil recovery up to 39.6%. Thus, the optimum mass fraction of DTPA for changing sandstone wettability was determined to be 5%.

Cite this article

PARHIZGAR KERADEH Mahsa , TABATABAEI-NEZHAD Seyyed Alireza . Investigation of the effect of diethylene triamine pentaacetic acid chelating agent as an enhanced oil recovery fluid on wettability alteration of sandstone rocks[J]. Petroleum Exploration and Development, 2023 , 50(3) : 675 -687 . DOI: 10.1016/S1876-3804(23)60419-7

Introduction

Despite developing enhanced oil recovery methods, waterflooding in oil reservoirs is still used to maintain reservoir pressure and transfer oil to production wells due to its simplicity and low cost [1]. Studies have shown that the salinity and composition of injected water significantly affect oil recovery. McGuire et al. [2] stated that injecting low salinity water (LSW) increases oil recovery in carbonate and sandstone reservoirs. Salinity reduction or decreased total dissolved solids (TDS) of the injected water changes rock wettability and reduces the surface tension and capillary pressure [3]. Therefore, LSW produces more oil than SW due to low salt concentration [4-5]. Tang and Morrow [6] performed different experiments on sandstone samples and reported three necessary conditions for increasing oil recovery using LSW: the presence of clay, initial water saturation and crude oil containing polar compounds. Al-Otaibi et al. [7] performed different wettability studies on limestone cores and showed that synthetic aquifer water made the carbonate rock water- wet, but SW and formation water (FW) changed the rock wettability to more oil-wet. Al-Otaibi et al. [8-9] stated that as the brine salinity decreases, the negative surface charges and the electric double layer thickness increase. Nasrallah et al. [10] attributed enhanced oil recovery to wettability alteration of carbonate cores from less water-wet to more water-wet. LSW injection is a good technique to increase oil recovery due to economic and environmental considerations. However, despite the positive aspects of LSW, this technique can cause damage in some cases, such as scale precipitation and fine migration in carbonate and sandstone reservoirs[11-12]. SW treatment is also expensive to overcome precipitation problems, and SW dilution is unavailable in many countries. All these factors affect the selection of LSW as an enhanced oil recovery fluid [13]. Kumar et al. [14] stated that by increasing NaCl concentration and decreasing CaCl2 concentration in solution, the solubility of CaSO4•2H2O increases. LSW means reducing salts concentration such as NaCl in SW, which is responsible for keeping CaSO4 in solution.
Kumar and Calberg [14-15] reported that adding chelating agents to SW keeps Na+ concentration constant, but chelates Ca2+ in the fluid and prevents the CaSO4 precipitation. In order to investigate the effects of ions on various parameters, the authors have conducted several studies. Sultani et al. [16] showed that the presence or absence of SO42− in injected water would not significantly affect the ultimate oil recovery. However, compared to deionized water (DIW), adding Mg2+ to injected water would increase oil recovery by 10% to 15%. Rashid et al. [17] concluded that SO42− plays a significant role in rock wettability alteration and act as catalysts. However, they reported that the presence of SO42− is not critical to change the rock wettability. Karimi et al. [18] stated that during spontaneous imbibition tests, enrichment of LSW with Mg2+ leads to a decrease in ultimate oil recovery. Ali et al. [19] prepared different smart water solutions by adding 2500, 5000 and 1000 mg/L of monovalent and divalent salts within DIW. They also reported that by adding nanocomposite (TiO2/SiO2/poly(acrylamide)) to these smart solutions, the IFT decreased by 65%, and the performance of wettability alteration was influenced by 32%.
Chelating agents can be used as chemical enhanced oil recovery fluids and reduce the salinity of injected water by capturing and chelating metal ions such as Ca2+, Mg2+ and Fe2+ from fluid and rock and behave like LSW [13,20 -23]. Chelating agents such as EDTA are stable at high temperatures up to 200 °C [24]. They are not absorbed on the rock surface and do not damage the pores and also prevent precipitation by chelating different metal ions from rock and fluid [25-28]. Fredd and Fogler [29] were the first to use EDTA chelating agent as stimulation fluid in oil and gas fields, and Attia et al. [13] also used EDTA chelating agent for the first time to enhance oil recovery. Chelating agents are compatible with sandstones and carbonate rocks and are available in different pH values. Previous studies have shown that using chelating agents at high pH increases oil recovery and improves the performance of chelating agents [13,20,30 -32]. Injecting chelating agents at high pH can disturb the initial equilibrium between crude oil and rock and increase oil recovery [13,20]. Chelating agents can also be mixed with untreated SW, which is an effective way to reduce the costs of enhanced oil recovery and flooding projects [13,30]. SW contains high concentrations of sulfate ions, while FW contains divalent ions such as Ba2+, Ca2+ and Sr2+. By mixing FW with SW, an unstable solution is formed and precipitates CaSO4, SrSO4, BaSO4 in the reservoir [12,33]. Chelating agents capture metal ions and prevent them from reacting with other ions. Capturing metal ions from the solution prevents some problems, such as corrosion, precipitation and permeability reduction. Therefore, chelating agents in undiluted SW can behave the same as LSW and affect the rock dissolution and enhanced oil recovery process[34-36]. However, unlike LSW, chelating agents prevent precipitation and do not cause any formation damage. For these reasons, chelating agents have been proposed as an alternative to LSW flooding [13,35]. The dependence of the chelating agent on a metal ion is defined by the stability constant. High stability constant means high dependence of chelating agent on metal ions. For example, for all chelating agents, the stability constant with Fe2+ is high, which means chelating agent first separates Fe2+ from rock or solution and then separates other ions, such as Ca2+ and Mg2+ [21]. DTPA has the highest stability constant among all chelating agents, which means it takes ions from the solution more strongly and prevents ions precipitation [32]. Also, compared to other chelating agents, DTPA has the most carboxylic groups in its structure [37-41]. The additional carboxylic group in DTPA solubilizes more oil and decreases the IFT. Because of these reasons, in this study, we used DTPA chelating agent to perform different experiments. Wettability is one of the essential parameters in reservoirs that controls the location, distribution and fluid flow in the porous media[42]. Wettability affects almost all parameters required for reservoir management, including relative permeability, electrical properties, saturation distribution and capillary pressure [43]. Various methods are used to determine rock wettability alteration, including spontaneous imbibition tests, contact angle measurement, Zeta potential measurement, capillary pressure diagrams, relative permeability diagrams, and nuclear magnetic resonance. Ali [44] reduced the rock/oil contact angle from 134° to 22° by mixing 1000 mg/L Fe3O4-mineral-soil nanocomposites within SW. Wettability alteration is the first oil recovery mechanism proposed using chelating agents as enhanced oil recovery fluids [11]. Chelating agents at high pH separate various metal ions from solution, so the rock surface must release cations from its surface to achieve equilibrium. This dissolution process changes the rock wettability to more water-wet and with the release of ions from the rock surface, more oil will be recovered [11,22 -24,31,45 -46]. Mahmoud et al. [47] found that rock dissolution, IFT reduction and wettability alteration are possible mechanisms to improve oil recovery using HEDTA chelating agent. They also stated that EDTA of mass fraction 5% (5% EDTA for short) flooding in limestone core and 5% HEDTA flooding in sandstone core recovered more than 20% of OOIP. Hassan et al. [48] performed sequential flooding of EDTA chelating agent in carbonate rocks. The CT scan and pressure drop results showed that high concentrations of chelating agent led to rock dissolution and wormhole creation. They recommended using EDTA chelating agent at a mass fraction of less than 10%. Zeta potential measurements also showed that increasing the concentration of chelating agent leads to more negative charges on limestone surface. Hassan et al. [49] investigated the performance of EDTA in enhanced oil recovery from carbonate samples. They considered 3% of EDTA chelating agent as the optimum concentration, which resulted in maximizing oil recovery without causing severe rock dissolution. Mahmoud et al. [20,23] investigated the performance of EDTA in chelating Fe2+ from iron-rich minerals and used EDTA chelating agent to enhance oil recovery from sandstone samples. They were able to increase oil recovery up to 19% of OOIP using 10% EDTA solution without any formation damage. Hassan and Al-Hashim [50] showed that carbonate core flooding using EDTA solution altered wettability towards more water-wet. Also, ICP analysis confirmed that Ca2+ were chelated from the rock during EDTA flooding and their concentration increased in flooding effluent.
In this study, we used DTPA chelating agent as a new enhanced oil recovery fluid that can be used as an alternative to LSW. While previous studies used one of the quantitative or qualitative methods to investigate the rock surface charge, we considered both qualitative and quantitative techniques to determine rock surface charge and wettability alteration. Therefore, in order to investigate rock wettability alteration caused by using DTPA chelating agent, we used the set of Zeta potential, rock/oil contact angle, and imbibition measurements. Unlike previous studies which they considered light oil in their studies, we used heavy oil in this study to perform different tests. The effects of mass fraction, brine salinity, and for the first time, the impact of potential determining ions (Ca2+, Mg2+ and SO42−) and their concentrations on the performance of DTPA were also evaluated. Moreover, spontaneous imbibition experiments were conducted and the effect of capillary and gravity forces on oil recovery was discussed. Finally, using the results of different experiments, the optimum mass fraction of DTPA chelating agent was determined.

1. Experiment

1.1. Materials

Different synthetic solutions were prepared by mixing pure salts (NaCl, CaCl2·2H2O, MgCl2·6H2O, Na2SO4 and NaHCO3) with deionized water (DIW). Table 1 shows the composition of synthetic brine solutions. The ionic strength of synthetic water solutions was obtained using Eq. (1) [51-52]. It should be noted that in each solution, with increasing and decreasing NaCl, the ionic strength was kept constant and equal to the ionic strength of SW.
$I=\frac{1}{2}\sum\nolimits_{i=1}^{n}{{{C}_{i}}z_{i}^{2}}$
Table 1. Ionic composition of all solutions used in this study
Solution name Ion mass concentration/(mg·L−1) Ionic strength/
(mol·L−1)
Na+ Cl K+ HCO3 Mg2+ Ca2+ SO42−
SW 12 649 23 287 459 92 1641 499 3069 0.83
LSW(0.1 SW) 1264 2328 45 9 164 49 306 0.83
SW(1Ca2++0Mg2++0SO42−) 18 384 29 607 459 92 0 499 0 0.83
SW(3Ca2++0Mg2++0SO42−) 17 234 29 604 459 92 0 1499 0 0.83
SW(0Ca2++1Mg2++0SO42−) 15 856 29 615 459 92 1641 0 0 0.83
SW(0Ca2++3Mg2++0SO42−) 9651 29 625 459 92 4925 0 0 0.83
SW(0Ca2++0Mg2++1SO42−) 17 464 25 039 459 92 0 0 3069 0.83
SW(0Ca2++0Mg2++3SO42−) 14 477 15 898 459 92 0 0 9207 0.83
DTPA chelating agent (C14H18N3O10K5) with an initial mass fraction of 40% was used. It was diluted in SW and mass fractions of 1%, 3%, 5% and 7% DTPA were prepared at pH of 9.48, 10.13, 12.33 and 12.45, respectively. The molecular weight, density and pH value of 40% DTPA were 583.8 g/mol, 1.25 g/cm3 and 11, respectively. Fig. 1 shows the chemical structure of DTPA chelating agent. In all experiments, HCl and NaOH were used to adjust the pH of the solution. Dead oil from one of the oil reservoirs in southern Iran with molecular weight of 376.2 g/mol, API=16.97 and specific gravity of 0.953 6 g/cm3 at 15.56 °C was used. The viscosity of the oil was 80 mPa·s at 80 °C. The oil composition is listed in Table 2 and the results of SARA analysis are presented in Table 3. Sandstone rock with high amounts of Ca2+ was used in this study. Fig. 2 indicates the mineralogical characteristics of this sandstone [53-56]. The composition of different ions in this rock is given in Table 4.
Fig. 1. Chemical structure of DTPA chelating agent.
Table 2. Composition of crude oil used in this study
Component Mass
fraction/%
Component Mass
fraction/%
C2 0.01 C7 0.47
C3 0.01 C8 1.92
iso-C4 0.01 C9 2.46
n-C4 0.02 C10 1.69
iso-C5 0.12 C11 2.37
n-C5 0.14 C12+ 89.6
C6 1.18
Table 3. SARA analysis of crude oil in this study
Component Mass fraction/%
Saturates 23.55
Aromatic 43.47
Resin 16.58
Asphaltene 16.40
Fig. 2. XRD analysis of sandstone used in this study.
Table 4. Elemental analysis of sandstone using XRF
Element Mass fraction/% Element Mass fraction/%
SiO2 47.590 MnO 0.219
CaO 15.100 SrO 0.202
Al2O3 13.300 Cl 0.180
Fe2O3 7.950 BaO 0.100
K2O 3.640 CuO 0.092
Na2O 2.360 SO3 0.084
MgO 2.110 ZrO2 0.039
TiO2 1.210 Rb2O 0.013
P2O5 0.300 ZnO 0.008

1.2. Wettability measurement

This study investigated rock wettability using contact angle and Zeta potential measurements. To measure the rock-oil contact angle, sandstone cores were cut into thin sections and rubbed to obtain a relatively smooth surface. The sandstone tablets have a diameter of 3.8 cm and a thickness of 0.2 cm. They were washed with distilled water to remove dust from their surface and then dried at 80 °C for 24 h. The rock-oil contact angle was measured using the contact angle measurement setup shown in Fig. 3. First, sandstone tablets were placed in FW for one week at 80 °C, and the rock-oil contact angle was measured for all samples at the initial water-wet angle (θi). Then, they were immersed in crude oil at 80 °C for 21 d. The rock surface became completely oil-wet, and the rock-oil contact angle was considered as the oil-wet angle at time zero (θ0). Oil-wet sandstone tablets were immersed in different brine solutions and different mass fractions of DTPA chelating agent, in order to study the impact of DTPA chelating agent on wettability alteration.The rock-oil contact angle was measured for all samples at times 2, 4, 8, 12, 24, 48, 72, 120, 240, 360, 504 h and θf was considered as the final contact angle. In all measurements, oil droplets were placed on both sides of the thin sections to make sure the contact angles are similar and reduce the topographic effects. The contact angle was determined using Image-J analysis software.
Fig. 3. Schematic of the contact angle measurement setup.

1.3. Zeta potential measurements

Zeta potential measurements were performed to observe the rock surface charge. 1% of sandstone powder was added to the different solutions and conditioned for 24 h using a shaker at 30 °C and atmospheric pressure. After 24 h, the samples were removed from the shaker and allowed to settle for half an hour. The homogeneous sample was taken by syringe at the top of each solution and filtered through a 5 mm filter. Finally, the zeta potential was measured using the Zeta potential instrument, and the electrophoretic mobility of suspended particles was measured using Smoluchowsky equation [57].
$\zeta =\mu \frac{\eta }{{{\varepsilon }_{\text{0}}}{{\varepsilon }_{\text{r}}}}$

1.4. Spontaneous imbibition experiments

First, the dry weight of the core samples was measured. Then, the cores were saturated with FW and their porosity and permeability were measured. After that, they were placed in a desiccator containing oil for 24 h. Oil was sucked into the cores by a vacuum pump. Still, due to the high oil viscosity and density, the core samples were not able to be completely saturated with oil, so all core samples were aged in crude oil for four months at 80 °C and atmospheric pressure and their saturated weight were measured. After four months, graduated Amott cells were filled with different mass fractions of DTPA chelating agent (1%, 3%, 5% and 7%), and oil-wet cores were placed in them for 31 d. The properties of core samples are summarized in Table 5. Over time, DTPA imbibed into the core and produced oil by affecting rock wettability and surface tension. Due to the low density, the produced oil moved upward on top of the graduated cells and was monitored and recorded over time. Finally, the oil recovery was measured by calculating the oil volume in each sample and the amount of produced oil.
Table 5. Properties of the sandstone cores used in imbibition experiments
Experiment No. Length/
cm
Diameter/
cm
Porosity/
%
Permeability/
10−3 μm
1 7.5 3.8 18.5 74.6
2 7.5 3.8 18.2 73.3
3 7.2 3.8 19.3 75.6
4 7.3 3.8 18.8 76.9

2. Results and discussion

2.1. Wettability alteration

The wettability alteration of sandstone thin sections was investigated in the presence of different solutions. The performance of various solutions in changing rock wettability was determined using the wettability alteration index (WAI), which is given below:
$W=\frac{{{\theta }_{0}}-{{\theta }_{f}}}{{{\theta }_{0}}-{{\theta }_{i}}}$
WAI close to zero indicates an oil-wet state, and WAI close to one indicates water-wet wettability. Table 6 contains information about WAI for all wettability tests performed in this study. In order to investigate the impact of PDIs and their concentrations on wettability alteration, three PDIs (Ca2+, Mg2+ and SO42−) were selected and by adding and removing these ions from SW, their effects on rock wettability alteration were investigated. "SW(1Ca2++ 0Mg2++0SO42−)" represents SW, in which Mg2+ and SO42− have been eliminated and Ca2+ are the only PDIs being present in the aqueous phase. "SW(0Ca2++1Mg2++0SO42−)" and "SW(0Ca2++0Mg2++1SO42−)" represent SW only contain Mg2+ and SO42−, respectively, which other two ions have been removed. Also, "5% DTPA-SW" and "5% DTPA-LSW" indicates 5% DTPA was prepared in SW and LSW, respectively. ​"5% DTPA-SW(1Ca2++ 0Mg2++0SO42−)" indicates SW in which Mg2+ and SO42− have been omitted and 5% DTPA was prepared in it. Similarly, "SW(3Ca2++ 0Mg2++0SO42−)" indicates SW with three times of Ca2+ concentration, which Mg2+ and SO42− have been removed.
Table 6. WAI for different solutions
Number solution θi/
(°)
θ0/
(°)
θf/
(°)
WAI
1 SW 28 160 105 0.40
2 LSW 24 152 36 0.91
3 5% DTPA-LSW 21 156 19 1.00
4 DIW(pH=7) 21 150 81 0.52
5 DIW(pH=12) 18 141 27 0.93
6 1% DTPA-SW 30 138 93 0.41
7 3% DTPA-SW 28 141 82 0.52
8 5% DTPA-SW 22 143 23 0.99
9 7% DTPA-SW 27 153 22 1.03
10 SW(1Ca2++0Mg2++0SO42-) 23 144 115 0.24
11 SW(0Ca2++1Mg2++0SO42-) 28 133 112 0.20
12 SW(0Ca2++0Mg2++1SO42-) 28 145 118 0.23
13 5% DTPA-SW(1Ca2++0Mg2++0SO42-) 21 151 24 0.98
14 5% DTPA-SW(0Ca2++1Mg2++0SO42-) 18 154 23 0.96
15 5% DTPA-SW(0Ca2++0Mg2++1SO42-) 24 148 25 0.99
16 SW(3Ca2++0Mg2++0SO42-) 25 142 115 0.23
17 SW(0Ca2++3Mg2++0SO42-) 31 135 122 0.12
18 SW(0Ca2++0Mg2++3SO42-) 30 130 111 0.19
19 5% DTPA-SW(3Ca2++0Mg2++0SO42-) 22 124 58 0.64
20 5% DTPA-SW(0Ca2++3Mg2++0SO42-) 21 140 99 0.34
21 5% DTPA-SW(0Ca2++0Mg2++3SO42-) 24 140 76 0.55

Note: Except for Solution 5, pH value is about 7 for other solutions.

Based on the WAI values, Fig. 4 was divided into several wettability zones [58]. For instance, WAI between 0.5 to 0.7 indicates a neutral-wet state, WAI beyond 0.9 represents a strongly water-wet level and WAI below 0.2 shows a strongly oil-wet state [17]. According to WAI results, Solution 17 with WAI of 0.12 caused the lowest wettability alteration in the system. However, solutions of number 2, 3, 5, 8, 9, 13, 14, and 15 with a WAI close to one caused the highest wettability alteration.
Fig. 4. WAI for different solutions.

2.1.1. Effect of DTPA chelating agent mass fraction

To investigate the effect of DTPA chelating agent mass fraction on sandstone wettability alteration, 40% DTPA were diluted in SW and mass fractions of 1%, 3%, 5%, and 7% DTPA were prepared. Fig. 5 shows the initial and final contact angles before and after the thin sections were placed in the mass fractions of DTPA solutions. This series of experiments show that wettability shifts towards more water-wet with increasing DTPA mass fraction, which agrees with previous studies [20-21,34,48]. 5% and 7% DTPA-SW changed the rock wettability to more water-wet, but 1% and 3% DTPA-SW could not change the rock wettability to completely water-wet so that 1% DTPA-SW had WAI equal to SW (0.40) basically. Chelating agents trap metal ions and prevent them from reacting with other ions. With increasing DTPA mass fraction, the chelation force increases, and more cations will be chelated from the solution. In other words, when the mass fraction of DTPA chelating agent is less than 5%, DTPA does not have sufficient strength to chelate metal ions from rock and solution. By increasing DTPA mass fraction to 5%, wettability alteration reached the maximum. On the other hand, a further increase in mass fraction up to 7% did not affect the wettability alteration much. Therefore, 5% DTPA-SW was enough to chelate cations from solution and rock.
Fig. 5. The sandstone-oil contact angle in the presence of different mass fractions of solutions.
Fig. 6 shows the rock wettability alteration using different mass fractions of DTPA solution over time. 5% DTPA-SW solution decreased the rock-oil contact angle from 143° to 23°, and 7% DTPA-SW changed the rock-oil contact angle from 153° to 22°. As mentioned, the chelation power decreased by decreasing DTPA mass fraction to less than 5% so that 1% and 3% DTPA-SW could not change the wettability as much as 5% and 7% DTPA-SW solutions and most of metal ions remained in the solution. The presence of ions in the solution decreases the electrical double layer thickness, which reduces the repulsive force between oil and rock surface. Therefore, separating oil molecules from the rock surface does not occur easily[59]. Previous studies stated that electrical double layer thickness increases with increasing chelating agent mass fraction, which indicates the rock water-wetness [20-21,34,60 -61]. Chelating different ions causes a negative charge of rock and increases the repulsive force of oil-brine and rock-brine interfaces [62]. Hence, it seems that with increasing chelating agent mass fraction, wettability alteration will increase due to three reasons: (1) With ion concentration decreasing, ionic strength decreases and electrical double layer thickness increases. (2) Due to the chelation of cations from SW, the initial equilibrium between the rock and solution is disturbed. So, to create equilibrium, the cations are separated from the rock surface, transferred to the aqueous phase, and leading to more water-wet condition [13,20 -21,34 -36]. (3) By capturing cations from solution, salinity decreases and the effect of salting in occurs [63]. Therefore, with the incident of these mechanisms, the density of negative charge on the rock surface increases, which in turn releases carboxylic acids from the rock surface and makes the rock more water-wet.
Fig. 6. The rock-oil contact angle after using different mass fractions of DTPA solution.

2.1.2. Effect of salinity

Nasralla and Nasr-El-Din [64] found that compared to monovalent cations, the presence of multivalent cations in the solution caused less oil recovery. Chelating agents chelate all multivalent cations from solution and improve oil recovery. LSW injection changes the rock surface to more water-wet. Also, by chelating metal ions from brine solution, chelating agents change brine structure to LSW structure and make the rock strongly water-wet. To investigate the effect of salinity on rock wettability alteration, experiments were conducted using SW, LSW (10 times diluted SW) and DIW. As shown in Fig. 7, SW could not change the rock wettability to water-wet. It is necessary to note that reducing salinity to an optimum concentration changes the rock wettability to more water-wet (LSW), but with further salinity reduction (DIW), the rock wettability acts in the opposite direction and becomes more oil-wet. Since the purpose of this study was to use DTPA in combination with SW, 5% DTPA-SW system was prepared to remove metal ions from SW and create a structure similar to LSW. However, the results showed that 5% DTPA-SW system changed the rock wettability even more than LSW (23° compared to 36°). It is observed that, due to the low concentration of cations in LSW compared to SW, diluting DTPA in LSW (5% DTPA-LSW system) has a greater effect on wettability alteration. Previous studies have reported that pH dramatically affects the rock wettability alteration [63,65 -67]. By increasing the pH of DIW to 12, the rock-oil contact angle reached 27°. Furthermore, comparing the performance of DIW at pH=12 and 5% DTPA-SW solution, we find that the DTPA performance in wettability alteration is almost the same as DIW at pH=12.
Fig. 7. The rock-oil contact angle using solutions with different salinities.

2.1.3. Effect of potential determining ions

Extensive studies have been conducted to determine the effect of smart water and different ions on rock wettability alteration and oil recovery. Three ions were selected to investigate the effect of PDIs on the performance of DTPA chelating agent. several studies have shown that the presence of SO42−, Ca2+ and Mg2+ in the injected water is the main reason for rock wettability alteration[68-70]. Because due to the high charge density and capacity of divalent ions, they are more capable of separating polar components from the rock surface [71]. As shown in Fig. 8, by diluting DTPA chelating agent in SW(1Ca2++0Mg2++0SO42−), wettability significantly improved and the rock-oil contact angle changed from 151° to 24°. DTPA captures metal ions from the solution. As the ions are chelated from the solution, the rock releases cations from its surface to create an equilibrium. Therefore, the release of cations from the solution changes the rock wettability. The elimination of Ca2+ and SO42− in SW caused a slight change in the rock-oil contact angle, but diluting DTPA in this solution caused the rock-oil contact angle to change from 154° to 23° and created a water-wet condition. Also, by eliminating Ca2+ and Mg2+ from SW, the contact angle decreased from 145° to 118°. However, by adding DTPA to this solution, at first hours, the rock-oil contact angle decreased from 148° to 25° and changed rock wettability from oil-wet to the strongly water-wet state. Therefore, by introducing DTPA chelating agent to SW in presence or absence of any potential determining ions, wettability changed from oil-wet to strongly water-wet. From Fig. 8, we can conclude that the presence or absence of PDIs in the solution does not affect the performance of DTPA chelating agent. By capturing and chelating metal ions, DTPA prevents them from reacting with other ions. As a result, the type of ion had no impact on the performance of DTPA and the only difference can be in the stability constant of DTPA with different ions [21]. DTPA first attacks ions with high stability constant and then attacks the ions with lower stability constant.
Fig. 8. Effect of PDIs on the performance of DTPA chelating agents in changing rock-oil contact angle.
As shown in Table 6, Figs. 8 and 9, the concentrations of Ca2+, Mg2+, and SO42− in solutions 19-21 have tripled compared to solutions 13-15, respectively, and the rock wettability alteration has weakened. In fact, by increasing PDIs concentration in the solution, the chelation force decreases, so that 5% DTPA is not enough to chelate all PDIs from the solution. Comparison between solutions 19, 20, and 21 shows that the wettability alteration for Solution 20 is less than two other solutions, and with a smaller WAI. It can be due to the low concentration of Na+ (9651 mg/L, Table 1) in Solution 20 compared to the two other samples. In the clay surfaces, Na+ in the aqueous phase replace with divalent cations [72]. In fact, as metal ions chelated from the solution, Ca2+ and Mg2+ are separated from the rock surface to create an equilibrium, which are replaced by Na+ on the clay surface. In Solution 20, because it has a low concentration of Na+, the substitution of cations does not occur well. On the other hand, by changing the concentration of ions from one to three times, 5% DTPA cannot chelate all metal ions from solution and rock, and consequently, rock wettability cannot change to strongly water-wet. For these reasons, the wettability alteration of Solution 20 is lower than solutions 19 and 21. However, it should be noted that high concentration of Na+ in solution reduces the activity of the divalent ions and prevents them from accessing the electrical double layer.
Fig. 9. The effect of PDI concentration on the performance of DTPA in changing rock wettability.

2.2. Zeta potential

Zeta potential measurements were performed to investigate the effect of DTPA chelating agent on the electrical double layer and to confirm the wettability results in the previous section. The Zeta potential value indicates the surface charge of the rock. When clay minerals are exposed to the aqueous solution, a thin layer (Stern layer) containing cations will form on the clay surface. Besides a Stern layer, a thick layer (diffuse layer) outside the Stern layer will be created, which includes a significant number of ions. The shear plane exists between the diffuse layer and the Stern layer. Zeta potential measures the potential at this shear plane [73]. When the charges of rock-brine and brine-oil surfaces are the same, a repulsive force is created, so the negative magnitude of Zeta potential and the water film thickness increase. As a result, the rock becomes more water-wet. The negative magnitude of Zeta potential indicates the negative surface charge of the rock and the water-wetness of the rock surface. As mentioned, the Zeta potential depends on electrical double layer thickness. The Gouy-Chapman model (Eqs. (4) and (5)) shows the relationship between electrical double layer thickness and the Zeta potential [74]. It can be seen from these two equations, in high salinity solutions, due to the high salt concentration and high amount of multivalent cations, the electrical double layer thickness decreases, and absolute Zeta potential increases. Therefore, by chelation of multivalent cations, chelating agents reduce the salinity of the injected fluid and increase the electrical double layer thickness. Mahmoud [32] stated that the negative value of Zeta potential is increased due to the high pH of fluid and the chelation of multivalent cations.
${{\kappa }^{-1}}={{\left( \frac{{{\varepsilon }_{0}}\varepsilon kT}{2{{n}_{0}}{{e}^{2}}{{z}^{2}}} \right)}^{\frac{1}{2}}}$
$\zeta =\frac{2kT}{ze}{{\sinh }^{-1}}\frac{{{\sigma }_{e}}}{4{{\kappa }^{-1}}{{n}_{0}}ze}$

2.2.1. Effect of DTPA mass fraction

Various factors such as concentration, pH value and ionic strength can affect the charge and magnitude of Zeta potential [34,75 -77]. Zeta potential was measured for sandstone powder and DTPA-SW solutions, and the effect of DTPA on the Zeta potential at the solid-liquid interface was investigated (Fig. 10). It can be seen that, by increasing DTPA mass fraction, the negative magnitude of Zeta potential increases. In fact, the repulsive force increases by increasing the concentration of similar charges at two interfaces [20,64,78 -79]. Zeta potential values for 1%, 3%, 5% and 7% DTPA-SW solutions were −2.31, −2.81, −13.06, −13.60 mV, respectively. Although solutions of 1% and 3% showed a negative Zeta potential, they were not able to dissolve rock and change the rock surface charge. So, higher mass fractions of DTPA solution should be used to dissolve the rock surface and increase the negative magnitude of Zeta potential. As mentioned in wettability alteration experiments, increasing DTPA mass fraction from 5% to 7% did not much affect the Zeta potential because 5% DTPA was enough to chelate metal ions from rock and solution. Increasing DTPA mass fraction means increasing the chelation force, which increases the electrical double layer thickness and indicates a water-wet state in the system. By increasing electrical double layer thickness, oil droplets separate from the rock and oil mobility increases significantly [20]. Increasing water film thickness is considered as one of the effective methods in improving oil recovery because increasing water film thickness is usually associated with water-wet conditions.
Fig. 10. Effect of DTPA with different mass fractions on Zeta potential of sandstone.

2.2.2. Effect of salinity

Chen et al. [80] found that salinity affects the Zeta potential. As the salinity of the solution increases, Zeta potential becomes a positive value. Since SW is composed of multivalent cations such as Mg2+ and Ca2+, these cations tend to reduce the negative value of Zeta potential and change the surface charge to zero and positive values. Compared to divalent cations, trivalent cations such as Al3+ have a more effect on the surface charge, so that Al3+ compresses the electrical double layer more than Ca2+ and creates a more positive charge on the surface [81]. High salinity water is not recommended to increase oil recovery from sandstone reservoirs with high clay content, because it reduces electrical double layer thickness due to high salinity and high concentration of divalent cations.
Fig. 11 shows that the Zeta potential on sandstone surface in SW was −2.29 mV, while that in DIW and LSW reaches −7.22 mV and −6.31 mV, respectively. Ramez et al.[82] stated that by decreasing salinity, the negative magnitude of Zeta potential and oil recovery increased. Attia et al. [62] reported that compared to SW and LSW, chelating agents change the charge of rock to a more negative value. To further evaluate the effect of salinity on Zeta potential value, Zeta potential measurements were performed for sandstone in combination with SW, LSW, DIW, 5% DTPA-SW, 5% DTPA-LSW, and 5% DTPA-DIW solutions. Introducing DTPA into SW decreased the Zeta potential from −2.29 mV to −13.06 mV, and adding DTPA to LSW reduced the Zeta potential value from −6.31 mV to −17.75 mV. Furthermore, adding DTPA to DIW due to the lack of divalent ions in the solution and the direct impact of DTPA on the sandstone surface increased the negative amount of Zeta potential from −7.22 mV to −19.13 mV. The advantage of DTPA compared to other solutions (SW and LSW) is that DTPA separates all metal ions from solution and rock and increases the negative value of Zeta potential. Therefore, in high salinity solutions due to the presence of large amounts of multivalent cations, the performance of chelating agents decreases. Still, in low salinity solutions, the negative surface charge increases, and the Zeta potential shows a more negative value, which means that the metal ions are chelated from rock and solution.
Fig. 11. Zeta potential on sandstone surface with different solutions.

2.3. Spontaneous imbibition tests

Spontaneous imbibition experiments were conducted to evaluate the performance of DTPA chelating agent in oil recovery from sandstone cores. It is observed that oil recovery increases with increasing DTPA chelating agent mass fraction (Fig. 12). 1% and 3% DTPA-SW solutions recovered 13.2% and 16.5% of OOIP, respectively, while 5% and 7% DTPA-SW solutions recovered 39.6% and 40.1% of OOIP, respectively. In fact, unlike high mass fractions, DTPA at low mass fractions cannot completely chelate metal ions from the rock surface and dissolve the rock. Therefore, DTPA at low mass fractions provides less oil recovery than that at high concentrations. Hasan and Al-Hashim reported that 5% EDTA solution released oil from carbonate samples and recovered 80% of OOIP, but SW and DIW recovered 19% and 50% of OOIP, respectively [34]. As can be seen from Fig. 12, 5% and 7% DTPA-SW solutions had almost similar oil recovery. Therefore, similar to the wettability alteration and Zeta potential experiments, 5% DTPA was selected as the optimum mass fraction in this series of experiments.
Fig. 12. Oil recovery from spontaneous imbibition experiment using different mass fractions of DTPA chelating agent.
In static spontaneous imbibition, capillary and gravity forces are the main driving forces in the recovery process. Depending on rock wettability, the gravity force is dominated when the rock is water-wet, and the capillary force is dominated when the rock is oil-wet. 5% and 7% DTPA solutions, due to their high ability to chelate ions and dissolve rock, make the rock strongly water-wet. Therefore, gravity force becomes dominant and produces oil from the rock. However, solutions of 1% and 3% DTPA, due to the presence of large amounts of multivalent cations, cannot dissolve the rock significantly, so gravity force cannot overcome the capillary pressure and produce oil as much as 5% and 7% DTPA solutions. Fig. 13 shows that, in 3% DTPA-SW solution, large oil droplets can be seen on the top of rock surface; but in 5% and 7% DTPA-SW solutions, small oil droplets are observed on the rock surface.
Fig. 13. Oil displacing effects by spontaneous imbibition in sandstone cores with different mass fractions of DTPA solutions.
To evaluate the effect of driving forces in the imbibition process, the sandstone cores immersed in 1% and 7% DTPA-SW chelating agents were divided into two halves. As shown in Fig. 14, the core that was immersed in 7% DTPA-SW solution has a uniform profile on its cut surface. This profile indicates that the gravity force was dominant and imbibed DTPA solution into the core and produced oil. But in the core sample that was immersed in 1% DTPA-SW solution, due to the weak ability of DTPA chelating agent in changing rock wettability, capillary force kept the oil in the rock and prevented it from producing. In fact, the crescent profile on the cut surface of this core indicates that capillary force was a dominant force and acted in the opposite direction of gravity force.
Fig. 14. Cutting surface of cores used in spontaneous imbibition experiments.

3. Conclusions

Due to some problems such as precipitation, clay swelling, and cost of dilution that existed in LSW injection, we used DTPA chelating agent as an alternative to LSW. DTPA chelating agents capture metal ions from rock and solution, dissolve rock, and change the rock wettability toward water-wet without any formation damage. In order to investigate the impact of DTPA on the rock surface and oil recovery, experiments of rock wettability, Zeta potential, and imbibition were performed. Preparing 5% DTPA chelating agent in seawater changed the rock-oil contact angle from 143° to 23° and decreased the Zeta potential from −2.29 mV to −13.06 mV. In comparison with LSW, 5% DTPA made the rock more water-wet. The presence or absence of PDIs such as Ca2+, Mg2+ and SO42− in the solution could not affect the performance of DTPA in changing wettability. However, the performance of 5% DTPA-SW in wettability alteration was impaired by tripling these ions concentrations. By increasing DTPA mass fraction and decreasing the salinity of the solution, the absolute Zeta potential increases, and the rock wettability changed to water-wet. Imbibition experiments showed that the oil recovery factor increases with the increasing DTPA mass fraction. 5% and 7% DTPA-SW solutions recovered 39.6% of OOIP and 40.1% of OOIP. Therefore, 5% DTPA was suggested as an optimum mass fraction.

Nomenclature

Ci—molar concentration of species i, mol/L;
e—electrical charge, C;
i—ion SN;
I—ionic strength, mol/L;
k—boltzmann constant, J/K;
n—number of ionic species I;
n0—ion concentration, m−3;
t—time, h;
T—temperature, K;
W—wettability alteration index;
z—ion valence of the species;
ε—water dielectric constant;
ε0—permittivity of free space, F/m;
εr—relative permittivity of the fluid;
${{\kappa }^{-1}}$—double layer thickness, m;
ζ—Zeta potential, V;
η—viscosity of the fluid, Pa·s;
θf—final rock-oil contact angle after placing thin section in the designed solutions, (°);
θi—initial rock-oil contact angle before aging thin section in oil, (°);
θ0—rock-oil contact angle after aging thin section in oil, (°);
μ—electrophoretic mobility, m2/(V·s);
σe—electrokinetic charge density, C/m2.
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Outlines

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