Research on Organic Nanopore Adsorption Mechanism and Influencing Factors of Shale Oil Reservoirs

The adsorption properties of shale oil are of great significance to the development of shale oil resources. This study is aimed at understanding the microscopic adsorption mechanism of shale oil in organic nanopores. Thus, a molecular model of organic micropore walls and multicomponent fluids of CO2, C4H10, C8H18, and C12H26 is constructed to investigate the adsorption pattern of multicomponent fluids in organic nanopores under different temperature and pore size conditions. The quantity and heat of adsorption are simulated with the Monte Carlo method, which has been used in previous studies for single-or twocomponent fluids. The results demonstrate that the ability of CO2 to displace various alkanes is different. Specifically, mediumchain n-alkanes are slightly weaker than light alkanes in competitive sorption, and long-chain n-alkanes are less conducive to competitive sorption. The higher the CO2 sorption ratio, the more the sorption sites occupied by CO2. Thus, it is the best replacement for shale oil. The adsorption quantity of carbon dioxide, n-butane, and n-octane in organic nanopores first increases and then decreases as temperature rises. Meanwhile, the adsorption quantity of n-dodecane decreases firstly and then increases. With the increase in the pore size, the adsorption quantity of carbon dioxide, n-butane, and n-octane in organic nanopores increases while the adsorption quantity of n-dodecane first increases and then decreases. Besides, the model with larger pore sizes is more sensitive to pressure changes in the adsorption of carbon dioxide and n-butane than the model with smaller pore sizes. The heat of adsorption is CO2, C12H26, C8H18, and C4H10 in descending order. All are physical adsorption. Moreover, the adsorption quantity of all four components mixed fluid in the organic matter nanopores is positively correlated with the heat of adsorption.


Introduction
With the increasing demand for energy sources and the gradual depletion of conventional oil and gas resources around the world, searching for another unconventional alternative energy source is an inevitable trend for future energy development. Shale oil is a typical unconventional oil and gas resource, an essential supplementary and alternative energy source. Thus, countries around the world are beginning to focus on shale oil exploration and extraction. Generally, most shale oil in an adsorbed or free state is stored in the shale, and a small amount of shale oil keeps a dissolved (or miscible) state [1][2][3]. The characteristics of shale oil stored in shale reservoirs with low porosity and low permeability make it more difficult to exploit shale oil. Therefore, it is necessary to explore the adsorption and desorption of shale oil in organic nanopores. Its laws will provide theoretical guidance for shale oil extraction [4]. In recent years, molecular dynamic simulation techniques have presented great potential for quantitative characterization of adsorption resolution, interactions, and fluid transport in nanomaterials. They have been gradually introduced into petroleum research. Shale oil possesses a higher alkane content compared with conventional crude oil. However, it is a typical multicomponent fluid whose component composition is extremely complex [5]. Typically, shale oil under stratigraphic conditions may contain short-chain n-alkanes (such as methane CH 4 ), medium-chain n-alkanes (such as n-hexane n-C 6 H 14 ), and long-chain n-alkanes (such as ndodecane n-C 12 H 26 ), which are generally stored in organic nanopores in an adsorbed or free state. Shale oil is mainly composed of hydrocarbons, sulphur-containing compounds, nitrogen-containing compounds, etc. From the microscopic mechanism point of view, n-C 12 H 26 , as the main compound component of the oil phase of shale oil, can be a good substitute for shale oil at the nanoscale to simulate the competitive sorption of CO 2 and shale oil. As the pore size of shale parent material is in the nanometer range, the permeability coefficient of shale oil in shale parent material is extremely small. Besides, the macroscopic flow mechanism does not apply to the flow pattern of shale oil in the shale parent material [6,7]. Therefore, it significantly increases the difficulty of studying the adsorption and desorption of shale oil in nanopores.
The sorption and desorption of shale gas in organic and in organic nanopores have been extensively studied by many researchers [8][9][10], while there are few studies on the sorption and desorption of shale oil in organic and inorganic nanopores [11,12]. Pathank et al. [13] discovered that carbon dioxide can effectively replace shale gas adsorbed in shale cheesecake by investigating the adsorption-desorption law of methane and carbon dioxide in the three systems of methane-carbon dioxide-kerogen. Wu and Liu [14] employed the GCMC method to simulate the effects of temperature, pressure, and gas molar fraction on the adsorption and separation of CO/H 2 mixture in carbon nanopores and obtained the optimal pore width for the separation of CO/ H 2 . Zhou et al. [15] explored the effects of reservoir temperature, pressure conditions, and the molar fraction of CO 2 in the CO 2 /CH 4 gas mixture on the separation of CO 2 /CH 4 in slit-type pores in coal seams with the GCMC method. With the increase in pressure, the equilibrium separation coefficient of CO 2 relative to CH 4 , SCO 2 /CH 4 , initially increases until it reaches the peak, then decreases, and lastly tends to be constant at 20 MPa. Besides, Chen et al. [16] discovered the adsorption characteristics of CH 4 and C 2 H 6 on illite at high-temperature conditions (60°C, 90°C, and 120°C) by Monte Carlo method, revealing that the main influencing factor of CH 4 and C 2 H 6 adsorption is the layer spacing, and the excess adsorption of C 2 H 6 is twice as much as that of CH 4 at layer spacing above 2 nm. Wang et al. [17] investigated the storage pattern of straight-chain alkanes in slit pores formed by organic matter through molecular dynamics simulations, concluding that multiple alkane adsorption layers existed on the slit pore surface whose layer thickness is approximately 0.42 nm. Moreover, Wang [18] established an initial model of scCO 2 repelling shale oil in rock pores and performed the kinetic simulations to observe the microconfiguration diagrams of the oil repelling process and qualitatively analyze the mechanism of scCO 2 oil repelling. They revealed the microaction mechanism of scCO 2 repelling shale oil. Most of the shale oil adsorption simulation studies were conducted with two components. There are few simulation experiments for exploring the adsorption and desorption of multicomponent fluids such as CO 2 /CH 4 /C 2 H 6 and some polymeric alkanes under reservoir conditions. Many researchers have investigated the effects of temperature and pore size and other conditions on the adsorption and desorption of shale gas in organic nanopores and inorganic nanopores. However, the effect of temperature, pore size, component ratio, and other conditions on the adsorption of organic nanopores in shale oil reservoirs is rarely studied. Therefore, the Grand Canonical Monte Carlo (GCMC) and Molecular Dynamic (MD) methods are employed to research the effect of different molar ratios of CO 2 , C 4 H 10 , C 8 H 18 , and C 12 H 26 on the competitive adsorption pattern of each component with molecular dynamic simulations to address the above issues. The effect of formation temperature on the adsorption of multicomponent fluids composed of CO 2 , C 4 H 10 , C 8 H 18 , and C 12 H 26 in organic nanopores was investigated using the controlled variable method with the same formation pressure and the unchanged pore space, at various temperatures of the formation [19]. Under the same conditions of formation temperature and formation pressure, the size of organic nanopores in shale reservoirs was exchanged to explore the effect of the adsorption of multicomponent fluids in organic nanopores, so as to analyze the influence of changes of organic nanopores in shale oil reservoirs on the adsorption mechanism of shale reservoirs.

Construction of the Molecular Model.
Graphite is a three-dimensional structure, which was composed of carbon atoms. The first step to be taken in this paper is to select the graphene single cell structure from the Materials Studio database. Then, the single-layer graphene structure is constructed using the build window of the software, and the graphene slit model is established by the build layer under the Visualizer task module. The vacuum layer between the two graphene sheets is the pore space. Its thickness of 20 Å, 40 Å, and 60 Å is taken to build a 15a × 10b × c supercell graphene structure model, respectively. The X and Y directions are set as a periodic structure while a, b, α, and β are fixed to repeatedly meet on infinite space to simulate the macroscopic system, as illustrated in Figure 1. CO 2 , C 4 H 10 , C 8 H 18 , and C 12 H 26 fluid molecular models are constructed by the Visualizer task module. Figure

Optimization of the Calculation
Model. The graphene structural model and the CO 2 , C 4 H 10 , C 8 H 18 , and C 12 H 26 molecular models need to be structurally optimized before the adsorption simulations of the molecules, so as to reach the lowest point of potential energy, that is, energy minimization. The resulting optimized models are used for molecular simulations. Firstly, the geometry of the constructed models was optimized by selecting the smart option in the task Geometry Optimization under the Molecular Dynamics Forcite module to obtain a stable graphene slit structure. Afterward, the COMPASS force field was selected for the force field; the atom-based summation method was used for the van der Waals forces; the rest of the settings were 2 Geofluids kept as the software defaults. The fluid models of CO 2 , C 4 H 10 , C 8 H 18 , and C 12 H 26 were optimized in the same way Error! Reference source not found [20]. This is exhibited in Figure 2.
2.3. Potential Energy Model. In this paper, the simulations of CO 2 , C 4 H 10 , C 8 H 18 , C 12 H 26 , and the C atoms in the graphite layer and the molecule-molecule interactions are performed for the L-J potential energy model [21], whose specific parameters are provided in Table 1. The van der Waals forces between the covalently bonded molecules in the system are described by the potential energy function: where: r ij is the distance between particles i and j, q i is the charged quantity of particle i, q j is the charged quantity of particle j, ε ij is the energy action parameter, and σ ij is the dimensional action parameter; 2.4. Simulation Program. The adsorption processes of carbon dioxide, n-butane, n-octane, and n-dodecane in organic matter nanopores were simulated to investigate the effects of different pore sizes, different temperatures, and different molar ratios of different fluids on the adsorption capacity of carbon dioxide, n-butane, n-octane, and n-dodecane in organic matter nanopores. The components of fluids were carbon dioxide, n-butane, n-octane, and n-dodecane in molar ratios of 1 : 1 : 1 : 1, 4 : 1 : 1 : 1, and 1 : 4 : 1:1 to simulate the competing adsorption patterns of different molar ratios of the different components in the organic nanopores, respectively [22]. The simulated pore sizes range from 10 Å to 60 Å, and the simulated temperatures range from 333 K to 433 K. The default temperature in all simulation scenarios is 373 K, the pore sizes are 40 Å, and the pressures are 0-30 MPa, except for the temperature mechanism effect, which is divided into 11 pressure points. Besides, the simulations are developed separately. The simulations are detailed as follows. Periodic boundary conditions are set in the X and Y directions of the organic nanopores. The COMPASS force field is used for all calculations. Besides, the NVT system is used. It is a system in which the atomic number N, volume V, and temperature T are constants. The calculation is conducted using the Fix Pressure task under the Sorption module. The total number of production steps is 100,000, of which 10,000 are equilibration steps. The parameters such as van der Waals force, cut-off radius, and key tooth width are set as the same as those used in the structural optimization.

Competitive Adsorption Laws for the Same Molar Ratio.
The main component of shale oil contains some long-chain n-alkanes. Currently, a large number of studies have been conducted to enhance the recovery of shale oil by injecting carbon dioxide into the shale reservoir. Since different types of fluids have different adsorption capacities, the grand canonical Monte Carlo method is used to simulate the competitive adsorption of multicomponent mixed fluids with the same molar ratio in the pores of organic shale. The competing sorption patterns of carbon dioxide, n-butane, n-octane, and n-dodecane in organic nanopores were explained from a microscopic perspective. Besides, the competitive adsorption of a mixture of carbon dioxide, n-butane, n-octane, and ndodecane in the same molar ratio (carbon dioxide : n − butane : n − octane : n − dodecane = 1 : 1 : 1 : 1) in organic nanopores with a pore size of 40 Å was simulated at 373 K. The adsorption quantity of the multicomponent fluids was obtained for pressure variations from 1 to 30 MPa. The adsorption isotherm curves for a molar ratio of 1 : 1 : 1 : 1 are illustrated in Figure 3. Additionally, the adsorption configuration for a multicomponent fluid mixed with the same molar ratio is exhibited in Figure 4.
As observed in Figure 3, the adsorption of carbon dioxide, n-butane, n-octane, and n-dodecane in the pores of organic matter all rapidly increased with pressure before the low-pressure stage, followed by a slow rise. The four fluids reached saturation at approximately 10 MPa, and carbon dioxide reached saturation before n-butane, n-octane, and n-dodecane [23]. The sorption of carbon dioxide is approximately five times greater than that of n-butane while the difference in sorption between n-octane and n-dodecane is not significant, with n-octane slightly higher than ndodecane. There was a significant reduction in the adsorption of the three-component fluids compared to the adsorption of n-butane, n-octane, and n-dodecane as single components in the pores of the organic matter.
The adsorption configuration diagram demonstrates a clear adsorption layer on the organic wall. Besides, the adsorption pattern of different components of the fluid on the organic wall is different, reflecting that CO 2 has different abilities to displace various types of alkanes [24,25]. A large number of long-chain n-alkanes were adsorbed on the graphene wall, such as CO 2 and n-butane. Regarding the medium-chain n-alkanes, n-octane (green in the adsorption configuration diagram) is more apparently adsorbed in aggregates on the organic wall. Due to the strength of the adsorption capacity, the medium-chain n-alkanes are slightly weaker than the light alkanes in competitive adsorption. Moreover, most of the adsorption sites on the organic wall are occupied by CO 2 and n-butane. The competitive adsorption capacity of long-chain n-alkanes is the weakest, 3 Geofluids and the adsorption quantities are the smallest among the multicomponent fluids. This reveals that long-chain nalkanes are not conducive to competitive adsorption while shale oil is composed mostly of medium-chain and longchain n-alkanes. Additionally, it is extremely difficult to develop shale oil. Therefore, this multicomponent competitive adsorption model well explains the competitive adsorption law of CO 2 , n-butane, n-octane, and n-dodecane in organic nanopores at the microscopic level. Experimental studies of shale oil are limited by the difficulty of observing the microscopic processes of CO 2 -repelled shale oil, and the microscopic mechanisms of CO 2 -repelled shale oil in nanopores are unclear. Therefore, it is important to simulate the process of CO 2 repelling shale oil through the competitive adsorption between CO 2 and multicomponent to achieve the guidance of studying the microscopic mecha-nism of CO 2 repelling shale oil in nanopores, and this has important practical significance to guide the CO 2 extraction of shale oil. These curves demonstrate that the sorption ratios of carbon dioxide to n-butane, n-octane, and n-dodecane all first increase and then tend to equilibrate. Overall, the increase in the adsorption ratio indicates that carbon dioxide consistently occupies more adsorption sites in competition with nbutane, n-octane, and n-dodecane in the adsorption process. The larger the proportion of carbon dioxide in the fluid mixture, the more the adsorption sites occupied by carbon dioxide and the relatively less the n-butane, n-octane, and ndodecane adsorbed in the organic matter pores. The effect of the different ratios of molarity on the adsorption ratio is still significant. As reflected from the adsorption ratio curves, the adsorption ratios of carbon dioxide to n-butane, n-octane, and n-dodecane mixed ratios are 4 : 1, 1 : 1, and 1 : 4, respectively. The adsorption ratio when carbon dioxide is 4 molar ratio is greater than the adsorption ratio when nbutane, n-octane, and n-dodecane are 4 molar ratio to 1 molar ratio. This indicates that the higher the carbon dioxide adsorption ratio, the more carbon dioxide. Moreover, the replacement effect on shale oil is best and contributes more to significant CO 2 sequestration. Simultaneously, the ability of adsorption of crude oil itself is different under stratigraphic conditions owing to different components. The magnitude of the sorption ratio of CO 2 to n-butane, noctane, and n-dodecane reflects the sorption rate of each component. Furthermore, the 4 : 1 mixture of CO 2 to nbutane, n-octane, and n-dodecane leads to a large difference

Effect of Temperature on Competitive Adsorption
The effect of temperature on the adsorption of multicomponent fluid mixtures was investigated with the adsorption quantity and adsorption configurations of carbon dioxide [27], n-butane, n-octane, and n-dodecane in organic matter nanopores at a mixture ratio of 1 : 1 : 1 : 1 as an example. The simulated temperature interval is 333-433 K, the pore width is 40 Å, and the simulated pressure is 0.1-30 MPa. The giant regular Monte Carlo method is employed for simulation. The isothermal adsorption curves of carbon dioxide, nbutane, n-octane, and n-dodecane under different temperature conditions are presented in Figures 8-11, respectively. As indicated in the graph above, the adsorption quantity of carbon dioxide, n-butane, and n-octane in the organic nanopores of the multicomponent fluids first increases and then decreases with temperature, reaching a maximum for all three components at 373 K. As the temperature increases, the adsorption quantity decreases because the increase in temperature and pressure at the beginning of the simulation causes n-butane to add more kinetic energy and move more vigorously. Meanwhile, the chance of collision between    5 Geofluids carbon dioxide, n-butane, n-octane, and organic matter nanopore walls increases, as well as the adsorption quantity. As the temperature and pressure continue to increase, the nbutane molecules gain more kinetic energy and thus tend to adsorb away from the organic nanopore structure, and the adsorption volume decreases.
The temperature-dependent adsorption pattern of ndodecane in organic matter nanopores is opposite to that of carbon dioxide, n-butane, and n-octane. Figures 4 and 5 reveals that the amount of n-dodecane adsorbed first decreases and then increases with increasing temperature, and the maximum adsorption of n-dodecane was discovered at a temperature of 433 K, ascribed to the competition between the multicomponent mixture of carbon dioxide, n-butane, and n-octane. As the temperature increased to 373 K, the molecular movement of carbon dioxide, n-butane, and n-octane intensified, and the adsorption quantity reached its maximum [28]. When the temperature reaches 373 K, n-dodecane as a long-chain n-alkane does not intensify the movement of n-dodecane molecules, and the chance of collision between n-dodecane and organic matter nanopore walls does not increase, contributing to the reduction of adsorption quantity. Therefore, the maximum adsorption quantity of n-dodecane was achieved at a temperature of 433 K.
The temperature dependence of the adsorption of the mixed fluids competing for adsorption in the organic nanopores can be compared with that of the single-component fluids, demonstrating that the effect of temperature on the adsorption of the multicomponent fluids in the organic nanopores is weaker than that in the pure components nbutane, n-octane, and n-dodecane.

Geofluids
As revealed from the graph above, the sorption ratios of carbon dioxide to n-butane, n-octane, and n-dodecane all tend to first increase and then decrease with the increasing temperature increases. The ratio eventually stabilizes. This can be explained that n-butane is a long-chain alkane, and molecular movement is more intense when the temperature increases. The sorption ratio of carbon dioxide to ndodecane was less affected by temperature, and the effect of temperature change on n-dodecane in the fluid mixture was negligible. This suggests that short-chain alkanes are more susceptible to temperature influence compared to long-chain alkanes, and high temperature is more conducive to the desorption of alkanes and more beneficial to the replacement effect of shale oil.

Effect of Pore Size on Competitive Adsorption
The effect of pore size on the adsorption of multicomponent fluid mixtures was investigated by analyzing the adsorption and adsorption configurations in the nanopores of organic matter under a 1 : 1 : 1 : 1 mixture ratio of carbon dioxide, n-butane, n-octane, and n-dodecane [29]. The majority of shale oil storage environments are found in shale mesopores ranging in size from approximately 10 Å to 60 Å, which contains three intervals of pore size, including micropore, mesopore and macropore, and the range of pores in this interval allows for effective analysis of the effect of pore size on organic nanopore adsorption in shale reservoirs. The isothermal adsorption curves of carbon dioxide, n-butane, noctane, and n-dodecane under different pore sizes are provided in Figures 12-15, respectively. Figures 16 and 17 present the adsorption configurations for pore sizes of 10 Å and 60 Å, respectively. As indicated in Figures 12-15, the adsorption of carbon dioxide, n-butane, and n-octane in multicomponent fluids in the organic matter pore model at six pore sizes from smallest to largest is 10 Å, 20 Å, 30 Å, 40 Å, 50 Å, and60 Å. This implies that the adsorption of carbon diox-ide, n-butane, and n-octane by organic matter nanopores increases with the increase in pore size. However, the adsorption quantity of n-dodecane in multicomponent fluids in six pore sizes of organic matter pore models from smallest to largest is 10 Å, 60 Å, 50 Å, 40 Å, 30 Å, and 20 Å. The adsorption quantity of n-dodecane first increased and then decreased with the increasing pore size. Besides, the pore size had a greater influence on the adsorption of fluids in the organic structure. The variation of carbon dioxide, n-butane, and n-octane adsorption with temperature and pressure is the smallest in the 10 Å organic matter nanopore model. The variation of carbon dioxide, n-butane, and n-octane adsorption with temperature and pressure is the largest in the 60 Å organic matter nanopore model. Thus, it can be assumed that competitive adsorption has no greater effect on the increase in the adsorption quantity of carbon dioxide, n-butane, and n-octane with the increasing pore size.

Geofluids
It can be concluded that the model with larger pore size has a greater effect on the adsorption quantity of carbon dioxide, n-butane, and n-octane than the model with smaller pore size in the adsorption quantity of carbon dioxide, nbutane, and n-octane adsorbed that is more sensitive to pressure changes [30]. The pore size was in the range of 20 Å~40 Å when the pore size was a large variation in the adsorption of n-dodecane. It can be hypothesized that the competitive adsorption of long-chain alkanes in multicomponent fluids is gainful at 20 Å~30 Å of organic matter nanopores, and the smaller pore size models are more sensitive to pressure changes in the adsorption of n-dodecane than the larger pore size models.
The graph of Figure 18 suggests that the sorption ratio of carbon dioxide to n-butane, n-octane, and n-dodecane in the mixed fraction significantly decreases as the pore size increases. The sorption ratio of carbon dioxide to n-butane changes most significantly, which has a small increase in pore size from 10 Å to 20 Å, a significant decrease in the section from 20 Å to 30 Å and then a steady decrease. The adsorption ratio of n-octane and n-dodecane decreases gradually with increasing pore size, and there is no process of increasing the adsorption ratio first, which is quite different from n-butane. As the adsorption ratio decreases, the decrease in carbon dioxide sorption sites increases in nbutane, n-octane, and n-dodecane sorption sites. Therefore, the larger the pore size, the lower the sorption ratio, the more favorable the competition between carbon dioxide and the multicomponent fluid adsorption, and the more favorable to CO 2 replacement of shale oil in shale storage [31].

Heat of Absorption
The heat of adsorption is the heat released by the adsorption of adsorbent molecules on the adsorbent. It is an essential thermodynamic property of the adsorption process, which reflects the adsorption capacity of the adsorbent on the adsorbent and the nature of adsorption. The heat of adsorption is a crucial thermodynamic parameter distinguishing chemisorption from physical adsorption. The heat of adsorption is greater than 42 kJ/mol for chemisorption and less than 42 kJ/mol for physical adsorption [32]. Simultaneously, Figure 19 illustrates the molecular simulation of the heat of adsorption with pressure and temperature for the same proportion of a mixture of carbon dioxide, nbutane, n-octane, and n-dodecane in organic nanopores at a pore size width of 40 Å, a temperature of 333-433 K, and pressure of 10 MPa.
The graph above indicates that the heat of adsorption is CO 2 , C 12 H 26 , C 8 H 18 , and C 4 H 10 in descending order. The heat of adsorption of carbon dioxide, n-butane, n-octane, and n-dodecane by organic nanopores is less than 42 kJ/ 8 Geofluids mol, which is physical adsorption. The equivalent heat of adsorption of carbon dioxide, n-butane, n-octane, and ndodecane increases with the increasing pressure at the same temperature. The equivalent heat of adsorption of ndodecane first decreases and then increases as the temperature increases. It is positively correlated with the amount of n-dodecane mixed component fluid adsorbed in the organic matter nanopores. Carbon dioxide, n-butane, and n-octane all first increase and then decrease in the equivalent heat of adsorption with the increasing temperature. This is positively associated with the amount of carbon dioxide, nbutane, and n-octane adsorbed in the organic nanopores, that is in that the increase in temperature leads to an increase in the kinetic energy of carbon dioxide, n-butane, and n-octane seeds, making it easier for them to escape from the surface of the organic nanopore model, resulting in a decrease in the heat of adsorption.

Conclusion
(1) In simulations of competitive adsorption of the same molar ratios of CO 2 , n-butane, n-octane, and ndodecane, the adsorption patterns of the different components of the fluids on the pore surfaces of the organic matter and the ability of CO 2 to displace the various alkanes were different. Medium-chain alkanes are slightly weaker than short-chain alkanes in competitive adsorption while long-chain alkanes are less favorable to competitive adsorption (2) In the multicomponent fluid competition adsorption law, the adsorption quantity of each component in the pores of organic matter increases with pressure. Besides, the adsorption quantity changes significantly when each component is adsorbed due to the different molar ratios. The sorption ratio of carbon dioxide at 4 molar ratios is greater than that of n-butane, n-octane, and n-dodecane at 4 molar ratios versus 1 molar ratio. This demonstrates that the higher the carbon dioxide sorption ratio, the more the carbon dioxide present, and the more the sorption sites occupied by the carbon dioxide. More-over, it is the best replacement for shale oil and contributes more to the massive sequestration of carbon dioxide. When CO 2 is mixed with n-butane, noctane, and n-dodecane in a 4 : 1 ratio, the difference in sorption between the components is large, and CO 2 does not have the same replacement capacity for different components (3) The adsorption of carbon dioxide, n-butane, and noctane in the organic matter nanopores of the multicomponent fluids first increased and then decreased with temperature, reaching a maximum at a temperature of 373 K. The adsorption of n-dodecane first decreased and then increased until the maximum adsorption of n-dodecane was reached at a temperature of 433 K (4) The adsorption of carbon dioxide, n-butane, and noctane by organic nanopores increases as the pore size increases. Meanwhile, the adsorption occupancy of n-dodecane in the competitive adsorption of multicomponent fluids first increases and then decreases. The larger the pore size, the lower the adsorption ratio. This is more conducive to the competitive adsorption between carbon dioxide and multicomponent fluids and the replacement of shale oil in shale storage by carbon dioxide (5) The heat of adsorption is CO 2 , C 12 H 26 , C 8 H 18 , and C 4 H 10 in descending order. As the temperature increases, the equivalent heat of adsorption of carbon dioxide, n-butane, and n-octane firstly increases and then decreases while that of n-dodecane firstly decreases and then increases. Moreover, there is a positive correlation between the adsorption amount of all four components in organic nanopores

Data Availability
All data included in this study are available upon request by contact with the corresponding author.

Conflicts of Interest
The authors declare no conflicts of interest. Behavior and Migration Mechanism of CO2 and Multicomponent Alkanes in Shale Dynamical Nanopore. The authors also would like to appreciate the support of the General Project of Natural Science Research in Colleges and Universities of Jiangsu Province [No. 20KJB440003], study on carbon dioxide-methane transport mechanism of coal seam nanopores with multiple inducement deformation fields.