3.1 Rock mineral composition and its influence
As the object and main material of this paper, firstly, we studied the rock mineral composition and its structural characteristics of conglomerate reservoir, and completed the research on the microscopic physicochemical characteristics of conglomerate reservoir reservoir.
3.1.1 Reservoir classification
This article divides conglomerate oil reservoirs into four categories based on pore structure and physical parameters (Tang and Qi 2014) (Table 2). Among them, high permeability reservoirs in categories I and II (Table 3) will be the main targets for chemical flooding, while reservoirs III and IV cannot be completed due to the difficulty of polymer entry, so this article will not discuss them.
Table 2
Reservoir Classification Evaluation Table
Reservoir type
|
Ⅰ
|
Ⅱ
|
Ⅲ
|
Ⅳ
|
Pore types
|
Primary intergranular pores, Intergranular dissolved pores
|
Internal micropores, and intergranular pores
|
Pore structure parameters
|
Coefficient of variation(G)
|
>0.3
|
0.15~0.3
|
0.16~0.22
|
<0.1
|
Median pressure(MPa)
|
<2.2
|
2.2~4
|
4~6
|
<4
|
Displacement pressure(MPa)
|
Lower
|
0.2~0.7
|
0.5~1.1
|
>1
|
Pore-throat radius(µm)
|
>80
|
<80
|
Small
|
Very small
|
Maximum connected roar radius(µm)
|
<15
|
7.5~1.4
|
1.4~0.83
|
0.38
|
Physical parameters
|
Porosity(%)
|
>20
|
15~20
|
10~15
|
<10
|
Permeability(mD)
|
>100
|
50~100
|
10~50
|
<10
|
Reservoir evaluation
|
Good ~ Excellent
|
Medium
|
Bad
|
Very poor
|
The conglomerate cores were processed, the cores were scanned, drilled, sliced, observed and oil washed, and the porosity and permeability of the conglomerate natural core samples were gas measured using a high temperature overpressure pore penetrometer, of which there were three pieces of Class I cores, three pieces of Class II cores, and one piece of Class III cores, which will be used as the core material for the research of this paper.
Table 3
Parameter Table of Conglomerate Samples
Sample label
|
Depth/m
|
Porosity/%
|
Permeability/mD
|
Reservoir classification
|
S09511
|
1178.09
|
23.50
|
118.00
|
I
|
S09521
|
942.28
|
25.00
|
675.00
|
I
|
S09551
|
944.88
|
23.10
|
168.00
|
I
|
S7
|
945
|
18.11
|
53.18
|
II
|
S8
|
945.4
|
18.00
|
52.89
|
II
|
S11
|
791
|
18.77
|
56.38
|
II
|
S20
|
1132
|
14.71
|
36.72
|
III
|
3.1.2 Rock composition and structure
The medium and high permeability conglomerate reservoir reservoir rocks were selected for cast thin section fabrication, microscopic observation, and were visible by fabricating oriented slices for observation under incident and reflected light microscopes:
The lithology of Class I reservoir is dominated by coarse sandy fine conglomerate, the particle size is greater than 0.5mm, mainly distributed in 1 ~ 5mm, and the rock fragments are particle-supported with point - line contact. The gravel composition is complex, the particle sorting is medium, and the rounding is dominated by sub-rounded-sub-angular shape. The minerals are mainly quartz and potassium feldspar, followed by plagioclase feldspar; mica flakes are common, mainly intergranular filling and flake or curved flake output on the surface of the grains. The distribution of filler is uneven, including fine sand grade clastic particles, water mica, mud cement and carbonate cement.The porosity of the sample of Class I reservoir is 23%~25%, and the permeability is more than 100×10− 3µm2, which is a medium-high permeability reservoir. The content of intergranular heterogeneous base is high, the particle sorting is poor, the dissolution pore is developed, the distribution of pore throat is not uniform, the filler is clay with poor crystalline shape, etc., and the residual intergranular pore is developed. The pore type is dominated by primary intergranular pores, and the residual intergranular pores are developed (Fig. 2), showing the Combination of intergranular dissolution porosity - intergranular porosity - intragranular dissolution porosity.
The lithology of Class II reservoir is mainly sand-based supporting conglomerate, with moderate grain sorting and mainly sub-angular and sub-rounded. The minerals are mainly quartz and potassium feldspar, followed by plagioclase feldspar. The content of filler is high, including fine sand-grade clastic particles, hydrous mica and mud cement, carbonate cement.The porosity of Class II reservoir is 15%-20%, permeability is 50×10− 3~100×10− 3µm2, which is a medium-porous and medium-permeable reservoir. The pores are dominated by intergranular pores and secondary dissolution pores (Fig. 3), the type of pore-throat combination is small pore micro-throat type, the distribution of pore throats is single-peak biased fine type, and the mainstream throats are a small number of coarse throats.
The lithology of class III reservoir is mainly sand and gravel mud mixed, with poor particle sorting and high content of filler.The porosity of class III reservoir is less than 15%, and the permeability is 10×10− 3~50×10− 3µm2, which is a medium-porous and medium-low permeability reservoir (Fig. 4). Minerals are dominated by quartz and feldspar; quartz is fractured and secondary enlarged, feldspar is clay mineralized and severely altered, and sodium feldspar is aggregated in sheets of bicrystals; the content of debris is high, and the particles are not oriented.
3.1.3 Mineral composition and content
The surfaces of the conglomerate sample particles were first scanned by energy spectroscopy (EDS) to analyze the elemental composition of these physicochemically active minerals. The filler material of the conglomerate samples was then analyzed by scanning electron microscopy (SEM) for mineral characterization (after oil washing treatment).
The elemental composition of the conglomerate reservoir rocks can be known by energy spectrum analysis (Fig. 5), in which, in addition to the conventional elements such as C, N, O, S, conglomerate samples contain a large number of Si and Al elements, and it is known that the reservoir backbone minerals are composed of feldspars and quartz, and their chemical structures are Na/K[AlSi3O8] and SiO2, respectively; In addition, clay minerals and zeolite minerals are hydroaluminosilicate mineral products (see Table 4).
Table 4
Chemical formula of hydroaluminosilicate minerals
Minerals
|
Chemical formula
|
Kaolinite
|
Al4[Si4O10](OH)8
|
Montmorillonite
|
Ex(H2O)4{(Al2 − x,Mgx)2[(Si,Al)4O10](OH)2}
|
Illite
|
KAl2[(SiAl)4O10](OH)2·nH2O
|
Turbidite
|
Ca[AlSi2O6]2·4H2O
|
Then through the scanning electron microscope images, the conglomerate reservoir skeleton mineral surface is indeed complex in composition, with the presence of a large number of clay minerals as well as zeolite-like minerals.The most extensive distribution of kaolinite was observed in the samples, with page-like kaolinite monomers and aggregates seen in almost every sample, as well as illite in the form of bridging pseudohexagonal wafers, acicular and lath-like chlorite growing secondarily on the mineral surfaces, and honeycomb and flamed illite-montmorillonite mixing layers filling the inside of the pore spaces, as well as monocrystalline structural turbidite zeolites and globular grains of galena zeolites, as shown in Fig. 6.
In order to more accurately analyze the mineral composition and ingredients, x-ray diffraction (XRD) analysis was used to characterize the composition of the conglomerate samples filler and to do quantitative analysis, and the results of mineral content analysis are shown in Fig. 7.
Conglomerate reservoir reservoir filler is dominated by feldspar and quartz, with feldspar content of 34.07% and quartz content of 37.53%; colluvium is dominated by sulfate minerals and clay minerals, with contents of 10.8% and 10.45%, and conglomerate reservoir filler does contain zeolite minerals, with contents of about 3.7%, mainly turbidite zeolites and square zeolites. The relative content of clay minerals was also analyzed (Fig. 8).
The result of the analysis tells that the relative content of kaolinite is the highest among the clay minerals, reaching 36.92%, followed by Illite Montmorillonite mixed layer(Later in this article, it is referred to as the Imon mixed layer) with 30.48%,illite with 29.2% and chlorite with the least relative content, 3.38%.
3.1.4 Influence of rock minerals on chemical drive
The rock mineral research finally analyzed the extracted material from Xinjiang conglomerate oil reservoir, the extracted material sample is the treated dirty oil mud, and then more than one week of drying treatment, and finally for the oil-free powdered samples. The analysis results are shown in Fig. 9 and Fig. 10.
Through the quantitative analysis of the samples before and after the chemical drive of the conglomerate reservoir reservoir filler, the mineral species did not change essentially, the proportion of zeolite in the extracted material became higher, the proportion of carbonate minerals became less, and the approximate proportion of the rest of each kind of minerals did not change significantly. The content of clay minerals in the total content did not change much, but the relative content had obvious changes, the content of immonite mixed layer in the post-drive extract was the most, illite and kaolinite content was the second, chlorite was the least, analyzing the reason for this may be related to the ion exchange capacity, lattice substitution occurred. When clay minerals are in contact with water, water can enter between the crystal layers and dissociate the exchangeable cations, and then the surface of the crystal layer establishes a diffuse double electric layer, which produces a negative electronegativity (Su et al. 2002). In clay mineral crystals, some of the cations are replaced by other cations, while the crystal structure remains unchanged, producing an excess charge.
Kaolinite is 1:1 crystal type, the upper and lower adjacent levels, one side is OH surface, the other side is O surface, and O and OH are easy to form hydrogen bonds, interlayer gravity is strong, the interlayer connection is tight, water molecules are not easy to enter the crystal layer, the number of adsorbed cations around is small, and the number of cations that can be exchanged is even smaller. Montmorillonite 2:1 type clay minerals, up and down the adjacent levels are O surface, interlayer gravity to intermolecular force is dominated by interlayer gravity is weaker, water molecules are easy to enter the crystal layer, due to lattice substitution produces more negative charge, around it, it will certainly be adsorbed equal amount of cations, hydration of cations to the clay to bring a thick hydration film, so that the montmorillonite expansion. Montmorillonite exists lattice substitution, the number of cations that can be exchanged is high. Elysite due to lattice substitution of the negative charge generated by the K+ to balance, due to ilmenite substitution position mainly in the Si-O tetrahedron, resulting in a negative charge from the surface of the crystalline layer is close to the surface of the crystal layer, so with the K+ to produce a very strong electrostatic force, K+ is not easy to exchange down the K+ size is just embedded in the neighboring crystalline layer of oxygen atoms between the lattice of the formation of the cavities, to play a role in connecting the 12 oxygen around it with the pairing, so, the K+ connection is usually very strong, not easy to exchange down. That's why illite is less likely to swell. Chlorite is also due to the presence of hydrogen bonding in its crystalline layers and compensates for the imbalance of the electrovalence resulting from lattice substitution with hydromagnesite instead of exchangeable cations, among other things (Zhao 2010).
Zeolite minerals belong to silica-aluminate minerals, zeolite can be formed in the alkaline environment, Xinjiang conglomerate reservoirs in the diagenetic evolution process of the Permian period have appeared in the alkaline environment (Guo et al. 2002), and clay minerals and zeolite minerals can be transformed into each other, the formation of smaller secondary pore space. Montmorillonite and zeolite both have strong adsorption, ion exchange, but not "a mother and a brother", zeolite is a shelf-structured aluminosilicate, montmorillonite is a layered silica-aluminate mineral, zeolite molecular cage structure has a stronger adsorption, and montmorillonite will be swollen when it comes into contact with water, and its affinity for heavy metal ions is low, poor adsorption capacity. The presence of zeolite minerals also has a great influence on the injection of chemical agents, and previous studies in this area have been largely uninvolved. In this paper, we analyzed and concluded that the ilmenite mixing layer in the stratigraphic output is a mixing layer of illite and montmorillonite minerals, and usually, the mixing layer of minerals is more likely to be swollen and dispersed than a single clay mineral in contact with water (Zhao 2010).
Specific surfaces and pore sizes of block samples from conglomerate reservoirs and minerals contained in conglomerate reservoirs were determined (Table 4). It can be seen that montmorillonite and zeolite have the largest specific surface, while the specific surface of the conglomerate natural core is larger than that of the skeletal minerals quartz and feldspar, indicating that the constituent minerals of the conglomerate reservoir are more complex.
Table 5
Mineral and core specific surfaces of conglomerate reservoirs
Reservoir Mineral Formation
|
Sample Name
|
Measurement Methods((m2/g))
|
BET Specific Surface
|
Langmuir specific surface
|
Skeleton minerals
|
Quartz sand
|
0.05
|
0.12
|
Feldspar
|
1.47
|
2.89
|
Carbonate minerals
|
Calcite
|
3.67
|
5.71
|
Dolomite
|
0.84
|
1.67
|
Clay minerals
|
Kaolinite
|
15.7
|
22.67
|
Illite
|
20.62
|
21.06
|
Chlorite
|
23.76
|
25.87
|
Montmorillonite
|
40.21
|
57.54
|
Aluminosilicate minerals
|
Zeolite
|
31.58
|
43.24
|
Actual core of conglomerate reservoir
|
S9551
|
5.327
|
6.943
|
S7
|
3.127
|
4.119
|
S8
|
2.358
|
3.654
|
S20
|
2.116
|
3.147
|
S4
|
2.446
|
3.715
|
S9511
|
4.502
|
5.379
|
S11
|
2.19
|
3.186
|
Stratigraphic extracts
|
Oil Sludge Extract
|
3.685
|
5.492
|
The high proportion of zeolite and immonium mixed layer in oilfield recovered oil sludge also indicates that these two minerals are easy to hydrate, strong adsorption, and have a large specific surface area, zeolite and immonium mixed layer large amount of adsorption of formation water and chemical agent, along with the migration of the injection agent is taken out of the formation, resulting in the formulation of the chemical drive system in the reservoir has been changed. Therefore, in the face of conglomerate reservoirs with high content of clay minerals and zeolite minerals, it is especially important to choose suitable chemical formulation.
3.2 Formulation optimization
Chemical drive to improve the recovery of conglomerate reservoirs involves three important indicators, namely, formation inhomogeneity, wave coefficient and oil washing efficiency, and these three indicators are interrelated, conglomerate reservoirs of strong inhomogeneity caused by formation inhomogeneity, resulting in polymers and surfactants composed of oil repellents injected after the wave to the limited volume of the formation, and then so that the efficiency of the oil washing is not high, which formed the formation of recovery improvement of the disadvantageous factors, and therefore can be put forward to the direction of the formation of chemical modification and chemical optimization of the direction of the oil reservoir chemical agent.
Zhang et al. (2011) from Xinjiang Oilfield Exploration and Development Research Institute compounded the surfactant with polymers HA and HB in response to the inability to achieve ultra-low interfacial tension (10− 3 mN/m) between a single Karamay petroleum sulfonate surfactant KPS and crude oil. The experimental formulations KPS/HA, KPS/HB and KPS/HA/HB systems were able to achieve ultra-low interfacial tension and enhanced recovery by more than 20%.
The key to achieve the success of chemical drive for crude oil extraction is the performance of surfactant, analyzed from the performance index of surfactant for oil drive, the amount of adsorption on the rock surface, the ability to reduce interfacial tension, salt and temperature resistance, price and other factors are the key indicators affecting the use of this surfactant (Zhang 2013). The degree of adsorption of the surfactant in the aqueous system depends largely on the nature of the hydrophilic head group of the surfactant monomer (Harendra et al. 2012). On this basis, experimental verification of the actual ability to drive off the oil needs to be carried out both indoors and in the field.
KPS as Xinjiang conglomerate reservoir site is currently the main application of surfactants, its anionic surfactant, synthesis process is simple, economical and practical, for Xinjiang conglomerate reservoir comprehensive performance is also better, the raw material oil for the Xinjiang conglomerate reservoir oil minus two lines or minus three lines of distillate, belong to the local materials, so this paper is still the main surfactant KPS to carry out the formulation of the formulation of the compounding and optimization.
The molecular structure of KPS is schematic:
Secondly, according to the more widely used oil repellent surfactants in the oilfield: nonionic-anionic surfactants and anionic surfactants, amphoteric betaine surfactants and nonionic surfactants are also selected in this paper, and a total of 17 kinds of oil repellent surfactants in the oilfield are selected.Through the interfacial tension measurement, optical contact angle measurement, evaluation of emulsification with crude oil, static adsorption experiments with Xinjiang oilfield water, the final preferred formulation was obtained through a series of evaluation experiments.
Secondly, this paper selects the surfactants that are widely used in oilfields at this stage: nonionic-anionic surfactants, anionic surfactants, amphoteric betaine surfactants and nonionic surfactants, which are 18 surfactants in total. The solution was prepared with formation water, and interfacial tension measurement, video optical contact angle measurement, evaluation of emulsification with crude oil, and adsorption experiments were conducted to arrive at the final preferred formulation through a series of evaluation experiments.
3.2.1 Interface Tension
Surfactant solution is injected into the oil formation to reduce the interfacial tension between oil and water, oil and rock, and change the wettability of the rock so as to improve the recovery rate. The ability to reduce the oil-water interface to ultra-low interfacial tension (10− 3 mN/m) is one of the main criteria for surfactant systems for tertiary oil recovery. It is widely recognized that only by lowering the oil-water interfacial tension to the ultra-low interfacial tension region, the residual crude oil in the reservoir void can be deformed and flowed (Wang et al. 1995).So in this paper, the interfacial tension was measured as the primary index of surfactant, and the results are shown in Table 6.
Table 6
Data table of interfacial tension between surfactants for oil recovery and crude oil produced from Xinjiang conglomerate reservoirs
Anionic surfactant
|
Interfacial tension(mN/m)
|
Nonionic surfactant
|
Interfacial tension(mN/m)
|
Amphoteric surfactants
|
Interfacial tension(mN/m)
|
Pure KPS
|
0.06
|
AES
|
1.45
|
18 Alkyl Dimethyl Hydroxypropyl Sulfobetaine
|
0.002
|
KPS703
|
0.008
|
AEO-7
|
0.44
|
12 Alkyl Dimethyl Hydroxypropyl Sulfobetaine
|
0.18
|
Sodium dodecylbenzene sulfonate
|
0.08
|
AEO-9
|
0.53
|
18 alkyl betaine
|
0.002
|
Petroleum sulfonate ND
|
0.37
|
6501-C120
|
0.004
|
12-Alkyl dimethyl betaine
|
0.29
|
Petroleum sulfonate NH
|
0.38
|
6501-C115
|
0.006
|
14-Alkyl dimethyl betaine
|
0.19
|
Petroleum sulfonate NB-N
|
0.13
|
6501-1: 1LC
|
0.01
|
Lauramidopropyl hydroxysulfobetaine
|
0.35
|
The results of the interfacial tension measurements of the 18 surfactants at a concentration of 3000 ppm showed that the betaine of octadecyl had the lowest interfacial tension of 10− 3 mN/m. Although the lowest interfacial tension of octadecyl betaine was found, the longer the carbon chain, the more hydrophobic groups increased, the poorer the solubility, and the lower the CMC was,thus, it can be seen that there is a positive correlation between the hydrophobicity of ionic surfactants and the ultra-low tension at the oil-water interface. In the solubilization of ionic micelles, the solubilization is mainly governed by the hydrocarbon chain length of the solubilizer molecules because the polar substances do not enter the interior of the micelles, but only solubilize on the surface of the micelles (Gong et al. 2019). And 6501 (coconut oil fatty acid diethanolamide) is good water solubility, 6501 series interfacial tension also reached a super low 10− 3mN/m, and the proportion of diethanolamine the greater its water solubility, so in the 6501 series, 6501-C120 interfacial tension is the lowest. KPS703 is a modified KPS product with lower interfacial tension than pure KPS, it also reaches the 10− 3 mN/m range.
Han et al. (2012) realized the ultra-low interfacial tension of oil and water in the Shengli Oilfield of PetroChina by using a generalized anionic-cationic surfactant complex with nonionic surfactant, and then understood the regional range of the surfactant concentration ratio for the ultra-low interfacial tension in the corresponding system, and obtained a large window of practical application. In this kind of generalized surfactant compounding dosage form, nonionic surfactant and anionic surfactant are actually two relatively independent factors, the former plays a role in regulating the oil-water equilibrium of the anionic and cationic surfactant compounding system, while the latter is the main factor in reducing the interfacial tension of the system.
The selected 6501 nonionic surfactant in this paper can achieve ultra-low interfacial tension by itself for the crude oil of Xinjiang conglomerate reservoirs, and we further compounded KPS703 and pure KPS with 6501, respectively, and the interfacial tension of the compounded surfactant decreased dramatically (see Fig. 11), which indicates that the nonionic surfactant 6501 and the anionic surfactant KPS are better mated to produce a positive effect.
Because the KPS series has been used for many years in the production site and its comprehensive performance has been affirmed, we initially decided to use KPS703 as the main surfactant, and the octadecyl betaine with ultra-low interfacial tension and 6501-C120 as the co-surfactant based on the results of the laboratory tests.
3.2.2 Surface wettability reversal
The experiment simulated the actual oil reservoir surface sample making, the surface is oily, the contact angle of conglomerate reservoir formation water is more than 100°, 0.3% concentration KPS703 can change the wettability of the rock surface, the contact angle is about 60°, the contact angle of 0.3% concentration betaine is about 31°, and the 0.3% concentration 6501 changes the wettability of the rock surface with a better effect, and the contact angle is about 30% (Fig. 12). And choosing a point on the sample thin section, dropping 6501 first, and then dropping simulated formation water at the same point, it was found that the contact angle was reduced to a very low level (Fig. 13), so that the surface was changed from oleophilic to hydrophilic. The contact angle on the surface of the oil-bearing natural core sand model was reduced, and the wettability was obviously reversed, so that the oil film on the surface of the oil-bearing natural core sand model could be stripped off and the residual oil could be initiated, which is very important for improving the crude oil recovery (Sun et al. 2015).
KPS703 was compounded with 6501 in a 1:1 ratio and the contact angle decreased to 46.8° (Fig. 14).
In addition to alkanes, most crude oils contain small amounts of surface-active polar components, and divalent cations combined with acidic components in the oil can control the wettability of the oil-water-rock system.Frieder Mugele et al. removed divalent ions from the water, and observed that the contact angle between the water and the rock surface was reduced by about 10°, which could improve crude oil recovery by several percentage points (Mugele et al. 2015; Herminghaus 2012). In this paper, the ionic surfactant was replaced with a nonionic surfactant, which again reduces the number of ions in the water that can be exchanged with the rock system, and controls the wettability by controlling the adsorption of ions to the solid-liquid interface, which from the results does change the wettability of the surface.
3.2.3 Emulsification performance with crude oil
The four surfactants were mixed and stirred with the crude oil of seven districts in the ratio of 1:1, and the emulsification effect was observed under the polarized light microscope. KPS and 6501 were oil-in-water (O/W) and hydrophilic with the crude oil, while KPS703 was water-in-oil (W/O) and lipophilic with the betaine (Fig. 15).The type of emulsion formed is due to the hydrophilic-lipophilic balance (HLB) of the surfactant and the disintegration of the emulsion phase also leads to an increase in the oil phase, an observation that implies that the oil is the dispersed phase. With the formation of O/W emulsions, the stability of the emulsions formed is due to the presence of electrical or spatial barriers to agglomeration on the dispersed droplets (Rosen and Kunjappu 2012).
Oil-in-water emulsions can improve oil repulsion in inhomogeneous reservoirs, especially conglomerate reservoirs with large extreme permeability differences. When the surfactant solution entering the oil reservoir is mixed with the crude oil, the oil-in-water emulsion is formed, the crude oil is dispersed phase, and the water is continuous phase, so that the thick oil molecules do not form a continuous mesh structure, and the friction between the water mostly replaces the friction between the oil in the flow, which reduces the viscosity of the crude oil at the leading edge of the displacement. At the same time, the oil-in-water emulsion can reduce the initial pressure gradient of crude oil seepage in the reservoir in the near-well zone, improve the seepage rheology of crude oil, thus increase the driving differential pressure of crude oil seepage, improve the oil recovery rate and increase the crude oil production. Ding et al. (2020) the W/O emulsification mechanism is more robust than the ultra-low interfacial tension and O/ W emulsification mechanisms.
Then from the stability of the emulsion to make a comparison (Fig. 16), it was found that KPS703 and 6501 precipitation rate of water is relatively low, after 2 hours of precipitation rate of about 80%, octadecyl betaine 2 hours of precipitation rate of water up to 100%, the highest relative. So all in all, 6501 has good overall emulsification properties.
3.2.4 Evaluation of adsorption performance
The adsorption of surfactant is mainly: electrical adsorption, ion exchange adsorption, intermolecular gravitational adsorption, formation of hydrogen bond adsorption and other physical and chemical adsorption. In this paper, different types of reservoir conglomerate samples with different types of surfactants were also selected to determine the nature of the surface charge of rock minerals and surfactants, and the results are shown in Tables 7.
Table 7
Table of zeta potential analysis results for the materials used in this paper
Sample name
|
Zeta(mV)
|
Mineral name
|
Zeta(mV)
|
Chemical agent name
|
Zeta(mV)
|
S09511
|
-28.45
|
Kaolinite
|
-8.98
|
2000ppm concentration KPS703
|
-37.7
|
S09521
|
-30.02
|
Montmorillonite
|
-21.03
|
S09551
|
-27.61
|
5000ppm concentration KPS703
|
-43.23
|
S7
|
-17.32
|
Illite
|
-8.18
|
S8
|
-18.21
|
Chlorite group
|
-17.8
|
Salt resistant polymer
|
-3.87
|
S11
|
-19.71
|
Calcite
|
0.22
|
S20
|
-4.033
|
Albite
|
-4.75
|
6501
|
-3.3
|
S13
|
-12.26
|
Zeolite
|
-24.47
|
Octadecyl Betaine
|
-2.09
|
Core fragment
|
-39.63
|
One of the main uses of zeta potential is to study colloid-electrolyte interactions. Since many colloids are electrically charged, they interact with electrolytes in complex ways. When a solid is in contact with a liquid, the solid-liquid interface carries a charge of opposite sign. Charged ions of opposite polarity to its surface charge (counterions) will be adsorbed to it, while ions of the same charge (co-ions) will be repelled.Zeta potential is the potential at the shear surface, and it is an important indicator of the stability of a colloidal dispersion system.
The DLVO theory (the theory describing colloidal stability) suggests that the stability of a colloidal system is the net structure of the bilayer mutual repulsion and van der Waals mutual attraction between particles when they are in close proximity to each other. It is in the form of a colloidal solution that clay minerals exist in subsurface reservoirs. The energy barrier between particles as they approach each other arises from the repulsive forces, and when the particles have enough energy to overcome this barrier, the mutual attraction will bring the particles closer together and irreversibly stick together (Derjaguin and Landau 1941; Elimelech and O’Melia 1990).
Generally, particles have many negative or positive charges and they repel each other, thus stabilizing the whole system. The particles carry few negative or positive charges, and they will attract each other, thus reaching the instability of the whole system. Zeta potential distribution of conglomerate reservoir ranges from 0 to -40mV, and the potential of underground reservoir spans a wide range, mostly belonging to the unstable system. The larger the specific surface area of clay minerals, such as montmorillonite and zeolite, the higher the potential, and calcite is a carbonate mineral with basically positive charge.
KPS surfactant belongs to anionic surfactant, Zeta potential in -40mV or so, the higher the concentration, the better the stability, but the later need to comprehensive cost considerations, the general field concentration of 3000ppm. 6501 nonionic surfactant charged smaller, amphoteric surfactant betaine is the smallest charged.
The results of static adsorption experiments showed that the polymer adsorption on montmorillonite was the largest, reaching 14 mg/g, on zeolite the amount of adsorption and montmorillonite roughly comparable to the amount of adsorption on the actual conglomerate cores of less than 5 mg/g, and in the loose conglomerate cores of the adsorption amount is greater than that in the dense conglomerate cores of the adsorption amount of the order from the largest to the smallest order is as follows: montmorillonite ≥ zeolite > chlorite > illite > kaolinite > calcite > feldspar > rock cores (Fig. 17).
The adsorption amount of surfactant KPS703 on montmorillonite and zeolite is the largest (Fig. 18), reaching more than 40mg/g, and the adsorption equilibrium concentration is also the highest, and the adsorption equilibrium is 5000 ppm, while the adsorption amount of the backbone minerals, feldspar and calcite, etc., is less than 10 mg/g. In the conglomerate cores, the adsorption amount of KPS703 is around 10 mg/g, and the adsorption equilibrium is around 3,500-4,000ppm. It can be seen that the adsorption amount of surfactant is much larger than that of polymer, especially on clay minerals, the adsorption amount reaches three times as much as that of polymer.
The results of dynamic adsorption experiments show (Tables 8) that the adsorption amount of polymer is much smaller than the adsorption amount of surfactant because its molecular weight is 15 million, which mainly occurs along the large pore channel scurrying as well as blocking the phenomenon of small pore channels, while surfactant is mostly a small molecule solvent, which, in addition to the reduction of the physical retention of the polymer, is more of the loss brought about by the chemical reaction. Therefore, the loss of adsorption and retention of binary composite oil repellent solution mainly occurs on the surfactant (Li et al. 2016).
Table 8
Dynamic adsorption of binary composite oil repellent chemistries on rock cores
Core number
|
Permeability(mD)
|
Polymer dynamic adsorption capacity(mg/g)
|
Surfactant dynamic adsorption(mg/g)
|
9511
|
118
|
0.110
|
0.216
|
11
|
56.38
|
0.127
|
0.261
|
20
|
26.72
|
0.139
|
0.255
|
Permeability is negatively correlated with dynamic adsorption, i.e., cores with high permeability have low adsorption of oil repellents, and cores with high permeability contain more highly adsorbed minerals. From the X-diffraction whole-rock analysis (Tables 9), The measured 9511 kaolinite content of Class I core is the highest, up to 7%, the content of immonite mixed layer is 6.3%, and the zeolite content is 1.1%. The content of immonite mixed layer of Class II core decreases and becomes 4.2%, but the content of zeolite rises to 7.4%, and the total content of clay minerals is also higher than that of the Class I reservoir, so that the degree of adsorption of the chemical agent in the Class II reservoir is greater than that of the Class I reservoir. Class III cores are too dense, so that large polymers are stuck in the pores, so the polymer retention in class III cores becomes larger, and the dynamic adsorption of surfactant in class III cores is not significantly larger than that in class I and II cores, the reason for the analysis is that Class III core samples contain a large amount of mirabilite, which is a sulfate mineral. The KPS surfactant is a sulfonated product of sulfur trioxide (SO3), which reacts with water to form sulfuric acid (H2SO4). In nature, minerals such as mirabilite, anhydrous mirabilite, and calcium mirabilite can even extract sodium sulfate (Na2SO4). mirabilite is generally highly soluble in water and easily weathered, So it is speculated that the solution after dynamic adsorption can detect a large number of absorption peaks of sulfate groups (-SO3H) or sulfate groups (-SO4H) under ultraviolet light, allowing the concentration of surfactants to increase instead of decrease.
Table 9
Mineral content analysis of cores from different reservoir types
Core number
|
Skeleton mineral content (%)
|
Carbonate mineral content(%)
|
Sulfate mineral content(%)
|
Silicon-aluminate mineral content(%)
|
Clay mineral content(%)
|
Reservoir type
|
feldspar
|
quartz
|
calcite
|
dolomite
|
limonite
|
mirabilite
|
barite
|
anhydrite
|
zeolites
|
corundum
|
kaolinite
|
illite
|
chlorite
|
Imon mixed layer
|
S09511
|
33.1
|
36.2
|
0.5
|
2.9
|
|
10.2
|
1.6
|
|
1.1
|
1.0
|
7.0
|
|
|
6.3
|
I
|
S11
|
27.7
|
42.9
|
|
|
|
6.7
|
1.2
|
|
7.4
|
|
3.2
|
6.8
|
|
4.2
|
II
|
S20
|
16.9
|
22.9
|
1.7
|
1.5
|
3.2
|
43.1
|
0.6
|
|
2.0
|
0.3
|
1.0
|
2.7
|
|
4.0
|
III
|
Considering that the degree of adsorption of surfactant is greater than that of polymer, and the degree of its action is closely related to the minerals contained in the reservoir, therefore, in the later optimization of the formula, the main research direction is to improve the surfactant, and the type and concentration of polymer can remain unchanged.
The role of polymer (HPAM) molecules and clay mineral surface: ① the electrostatic attraction between -COO- of HPAM and the metal active center or Stern layer on the clay surface; ② dispersion force, induced force and hydrogen bonding between the clay mineral surface and HPAM molecules.The level of polymer adsorption depends on three factors. First, the most important of these is the type and nature of the polymer, such as molecular weight, molecular size and charge density or degree of hydrolysis (for HPAM). Secondly, the solvent (only aqueous solutions are considered here) PH, salinity (Na+, C1−, etc.) and hardness (Ca2+, Mg2+) are the most important factors. The presence of other substances (e.g., alcohols) in the solution may also affect the solvent quality and thus the level of polymer adsorption.Thirdly, surface area and type of surface (silica, calcium carbonate, clay, etc.) are very important factors. Surface charge is also an important factor in determining polymer adsorption (Yun and Kovscek 2015).
For the surfactant KPS, the -SO3− group, hydrocarbon group and clay mineral surface have strong adsorption, the metal active centers on the clay surface (Al3+, Fe3+, Fe2+, Ca2+, Mg2+, etc.) will be electrically attracted to the surfactant ions, and there is an electrical attraction between the Sten layer on the negatively charged clay surface and the surfactant -SO3−, and there are also dispersion forces, induced forces, hydrogen bonding, and colloidization of surfactants that have already adsorbed on the clay minerals, which ultimately lead to multilayer adsorption.
Sol particles are electrically charged, and the main source of these charges is the selective adsorption of certain ions from the aqueous solution: adsorbed positive ions are positively charged, adsorbed negative ions are negatively charged, but an equal amount of counter-ions should also be present for the whole solution. The ions of the solid particles and the counterions in solution form a double electric layer.
Counterions are acted upon in solution in two opposite directions: ① the gravitational force of the ions adsorbed on the surface of the solid particles, which seeks to pull them toward the interface; and ② the thermal movement of the ions themselves, which causes them to diffuse out of the interface and into the solution.
As a result, the counterions show an equilibrium distribution outside the surface of the solid particles: the concentration of counterions is larger near the interface; as the distance from the interface increases, the counterions go from more to less, forming a diffuse distribution. Here we can lead to the Stern bilayer model, Stern that the solid surface due to electrostatic gravity and van der Waals gravity and attract a layer of counterions, close to the solid surface to form a fixed adsorption layer, this adsorption is known as the characteristic adsorption, this adsorption layer (fixed layer) is called the Stern layer.
Del Hoyo et al. (2008) have found that surfactants adsorb in the spaces between the layers of montmorillonite, while the adsorption of anionic surfactants by kaolinite and illite is not altered x-ray maps, suggesting adsorption on the surfaces or in the structural channels of these minerals.Surfactants interact with hydroaluminosilicates through functional groups of organic compounds,variable cations of clay minerals formed by ion-dipole or hydrogen bonding.On the other hand, rearrangement of the adsorbed surfactant molecules was also observed.So surfactant-mineral interaction produces adsorption and also changes both.
According to the results of the previous experiments, the preferred nonionic surfactant 6501 and the amphoteric surfactant octadecyl betaine, respectively, were static adsorbed with the minerals of conglomerate reservoirs, and it can be seen that the adsorption amount of 6501 was much lower than that of KPS703 and octadecyl betaine (Fig. 19), and the amount of adsorption of octadecyl betaine on the minerals was comparable to that of KPS703 (Fig. 20).
It can be seen that adsorption of anionic surfactants is inevitable in the face of conglomerate reservoirs with complex mineral compositions, and even though the electrical adsorption between negatively charged mineral rocks was reduced, multilayer adsorption still occurs.Therefore, this paper synthesizes all the above results and prefers nonionic surfactant 6501 as the co-surfactant for chemical drive in Xinjiang conglomerate reservoirs, followed by octadecyl betaine, and both of them are compounded with the main surfactant KPS703, and then carry out the dynamic drive validation experiments.