1. Introduction
In the global energy transition, coalbed methane, a low-carbon and clean energy source, has significant potential to reduce greenhouse gas emissions and is therefore regarded as one of the key transitional energy sources for achieving the Sustainable Development Goals [
1,
2]. Coalbed methane is typically found within the fractures of coal seams, with deposits buried at depths exceeding one thousand to several thousand meters referred to as “deep coalbed methane” [
3]. The development of deep coalbed methane is significant for increasing natural gas supplies and optimizing the energy structure [
4], yet it also faces technical challenges and economic risks [
5,
6]. As technology advances and experience accumulates, the exploitation of deep coalbed methane will gradually achieve scalability and economic viability [
7,
8].
Hydraulic fracturing technology plays a key role in the development of deep coalbed methane [
9,
10,
11]. It significantly enhances the production capacity of coalbed gas wells and extends the stable production period, thus becoming one of the main technologies currently used in coalbed methane development [
12]. The width of the fractures created by fracturing is crucial for long-term stable production. A 20% reduction in fracture width could lead to a 50% to 60% decrease in production capacity [
13]. Therefore, appropriately increasing the fracture width can effectively enhance the conductivity of coalbed methane, thereby ensuring that the production capacity of gas wells continues to meet development demands [
14]. However, as the burial depth increases, the closure stress of the coal rock reservoir gradually intensifies [
15].
Due to the relatively soft nature of coal rock reservoirs, the embedding of proppants under high closure stress significantly impacts the effective support fracture width [
16,
17]. Li studied how proppant arrangements affect fracture conductivity in coal reservoirs. They highlighted that coalbed rock has a low elastic modulus and a high Poisson’s ratio. During fracturing and flowback, proppant embedding causes contact deformation between proppants and fracture surfaces, impacting conductivity [
18]. In coal seams, Li analyzed proppant embedding mechanisms in fractures and their effect on conductivity. They identified various coal fracture surface damages and energy release mechanisms, suggesting proppant embedding reduces fracture opening and affects conductivity [
19]. However, these regularities are mainly summarized from experimental studies, and it is difficult to analyze the causes of this phenomenon from a mechanistic perspective.
Numerous experimental studies have demonstrated that factors such as closure stress, reservoir rock hardness, proppant hardness, and type significantly affect proppant embedment [
20]. Sheng noted that higher closure pressure correlates with increased embedment depth of proppants within shale plates, which concurrently induces local stress concentration and narrows unsupported fracture channels, thereby diminishing fracture conductivity [
21]. Lacy contends that the hardness of the formation is a more significant factor influencing proppant embedment. In soft, wet sandstone, when the proppant concentration is two pounds per foot, it can lead to a reduction in fracture width by 60% or more [
13]. Ahamed argues that coal reservoirs exhibit a greater susceptibility to proppant embedment issues due to their comparatively softer rock surfaces relative to surrounding reservoir rocks. They identify key factors impacting the performance of proppants in coal reservoirs as including proppant concentration, size, fracturing fluid type, and selection of the appropriate proppant type [
22]. Mittal simulated long-term permeability characteristics of proppant-filled layers under oil reservoir conditions in the laboratory, finding that normalized compaction in shale plates was 5% greater than in metal plates due to effects from embedded proppants [
23]. Bandara conducted an experimental investigation under multi-cycle loading conditions to elucidate the crushing and embedding mechanisms associated with various types of proppants during fracturing processes, analyzing how different sizes and concentrations influence these phenomena under similar loading conditions [
24]. Although previous experimental investigations have provided intuitive or indirect insights into the adverse impacts of proppant embedding on permeability within filled layers, conducting experiments specifically focused on measuring fracture permeability related to this phenomenon may require several hours or longer, making multiple tests time-consuming and costly.
Theoretical simulation calculations can quantitatively assess the influence of proppant embedding depth on fracture width to a certain extent. Volk investigated the factors affecting proppant embedment depth and proposed an empirical equation for non-crushed proppants embedded in sandstone and shale based on their analysis [
25]. Mueller proposed a modeling method for proppant embedment based on the size distribution and density of various proppants, utilizing surface-formed indentation hardness to calculate the degree of embedding [
26]. Li developed a rhombohedral model to calculate the flow capacity of sand-containing fractures by integrating the principles of elastoplastic ball contact, capillary bundle model, and Karman Kozeny equation. Their model factors in parameters such as rock and proppant deformation, particle size, proppant layers, and closure pressure, allowing for the calculation of width and permeability changes in sand-containing fractures during compression [
27]. Chen proposed a model of proppant embedding as a function of effective stress by combining the Hertz contact model with a power-law model, similar to the Oliver–Pharr model. This approach enables flexible simulation of different curvature shapes or trends of the embedding curve by adjusting the power exponent λ [
28]. Shi used the Hertz contact model to calculate the width of supporting fractures and studied the size effect of proppants, focusing on proppant deformation and embedding. They identified the particle size of proppants as the most sensitive influencing factor, followed by proppant concentration, proppant pumping rate, proppant elastic modulus, and proppant pumping method. They noted that compared to other factors, the influence of formation elastic modulus and Poisson’s ratio can be disregarded [
29]. After reviewing a series of previous studies, it was found that both individual experiments and theoretical simulations are insufficient for directly observing the dynamic embedment process of proppants within hydraulic fractures. This limits our ability to unveil the underlying micro-mechanisms of proppant embedment. Therefore, it is necessary to combine numerical simulation methods with experimental approaches for a comprehensive investigation.
Currently, while numerical simulation studies on proppant embedment are ongoing, there are certain limitations in these studies regarding the mechanisms by which proppant embedment affects fracture width. Fan combined three-dimensional continuum–discrete mechanics with the lattice Boltzmann (LB) method to systematically simulate the effects of fracture axial and confining stresses, number of proppant layers, proppant size, spatial distribution of proppants, and proppant breakage [
30]. Zheng established a three-dimensional discrete element model for proppant breakage and its impact on fracture conductivity. Although they discussed various factors affecting conductivity, they did not thoroughly analyze the influence of proppant embedment on fracture width [
14]. Liu utilized computational fluid dynamics (CFD) in conjunction with COMSOL Multiphysics to calculate the variations in permeability, concluding that both permeability and porosity decrease with increased proppant embedment, with the most significant reduction (nearly half) occurring within the first 20% of embedment [
31]. Deng used the three-dimensional discrete element method (3D DEM) to simulate the interaction between shale and proppants in hydraulic fracturing and to assess the average fracture width under different proppant sizes, Young’s modulus, and pressure levels. However, their analysis did not include a statistical examination of changes before and after fracture surface closure and the key control mechanisms that contributed to these changes [
32]. Meanwhile, Bolintineanu utilized the discrete element method (DEM) for simplified simulations, focusing solely on the generation of static proppant filling structures to analyze proppant filling height and evaluate the proppant diversion effect based on the final fracture width, without considering the interaction process between the proppant and the fracture surface [
33]. Zhang employed a combination of elastic–plastic theory and the material point method to develop a numerical model for the embedding of proppants in a coalbed reservoir. This approach addressed the issue in experiments where neglecting coal particle detachment led to underestimation of proppant embedding depth [
34]. Lu established a numerical model to simulate the elastic–plastic deformation of proppants embedded into rough fracture surfaces. They analyzed the embedding process of proppants in coarse fractures under closing stresses and identified factors affecting the width of the propped fracture [
35]. Ahamed proposed a simplified material model based on the Drucker–Prager failure criterion to describe proppant embedding behavior in hydraulic fracturing. They suggested that modifying the elastic modulus to account for surface changes due to pore fluid saturation may provide an underestimation for proppant embedment measurements in coal [
36]. However, their work did not quantitatively evaluate the impact of proppant embedding on the propped fracture width. Presently, there is limited numerical simulation research focused on the quantitative evaluation of proppant embedment behavior. Most studies primarily discuss the factors affecting embedment in relation to fracture conductivity. While some researchers have examined how the average fracture width varies with different parameters after closure, they have not systematically analyzed the dynamic changes in fracture width before and after closure to explore the underlying mechanisms of embedment influence.
In response to the aforementioned challenges, this study implements the discrete element flow method to construct a numerical simulation model for proppant embedding in coal seam reservoirs. The model simulates the dynamic process of proppant embedding in fracture surfaces during closure, calibrated with laboratory experiments. Subsequently, the study develops key methodologies for characterizing fracture width and proppant embedding depth. Lastly, the influence of factors such as proppant size, number of placement layers, and closure stress on fracture width is investigated. The research aims to identify optimal proppant parameters, offering theoretical support to optimize hydraulic fracturing operations in coal seam reservoirs.
2. Establishment and Validation of the Model
2.1. Principles of Discrete Element Particle Flow Code
The Discrete Element Particle Flow Code (PFC) operates by discretizing rock–soil into disk particles or spherical particles. Particle movement is governed by their interactions through contact with one another and is not entirely unconstrained. The principles governing particle motion are depicted in
Figure 1, wherein the constitutive relationship based on the contact model uses the force–displacement law to calculate contact forces and displacement changes between particles. Subsequently, Newton’s second law of motion is used to update particle positions and identify contact points and stacking distances. These processes are iteratively refined until system equilibrium is achieved or failure occurs in the rock–soil, as illustrated in
Figure 1.
First, the discrete element particle flow simulation adheres to the force–displacement law. Based on the constitutive relations of the contact model, the forces and torques between particles are calculated according to the force–displacement law. As shown in
Figure 2, in a two-dimensional model, the contact point of the particle element is located in the ‘overlap’ region of the two solid elements. When particles come into contact, the normal direction of the contact plane aligns with the line connecting their centers. When a particle contacts a wall, this normal direction is defined as the direction of the shortest distance from the particle’s center to the wall.
The unit normal vector
ni of the contact plane between two particles, as well as the
ni of the contact plane between a particle and a wall, can be calculated using the following formula:
In Equation (1),
xAi,
xBi, and
xCi represent the positions of the centers of particles A, B, and C, respectively.
xWi represents the intersection point of the unit normal vector
ni with the wall.
d represents the distance between the centers of particles or the distance from a particle center to the wall. The formula for calculating this distance
d is as follows:
The equation for determining the position
xδi of the contact point across various contact modes is presented as follows:
In Equation (3), RA represents the radius of particle A, RB represents the radius of particle B, and RC represents the radius of particle C. Additionally, Un represents the extent of overlap between particles or between particles and the wall.
The contact force vector
Fi acting between two interacting bodies can be resolved into a normal component and a tangential component:
The formula for calculating the normal component,
Fin, is as follows:
In Equation (5), Kn represents the normal stiffness at the contact point.
Second, the discrete element particle flow simulation follows the laws of motion. Based on the resultant force and torque acting on the particles, combined with Newton’s Second Law of Motion, the motion state of the particles can be determined. This manifests in two forms: translation and rotation. The basic equations of motion are as follows:
Equation (6) delineates the translational equation, represents acceleration. m represents the mass of the particle unit. gi represents the vector of volumetric force acceleration, such as gravitational load. Equation (7) articulates the rotational equation. represents angular acceleration. Mi represents the resultant moment acting on the particles. I indicates the principal moment of inertia.
Finally, there are various contact models in the discrete element method for particles, and this study primarily focuses on the linear parallel bond model (
Figure 3). The linear parallel bond model includes both parallel bonding and linear contact. The linear contact only acts under compression, with a mechanism similar to the linear model. The mechanical model of the parallel bond model can be described as follows:
The mathematical expressions for the contact force
and moment
within the linear parallel bonding model are as follows:
In Equation (8),
represents the linear force;
represents the damping force; and
represents the parallel bonding force. In Equation (9),
represents the parallel bonding moment. The formulae for calculating both the parallel bonding force and moment are presented as follows:
In Equation (10), represents the normal parallel bonding force; represents the tangential parallel bonding force; and represents the normal component of the unit direction vector. In Equation (11), represents the rotational torque, which is consistently equal to zero in the two-dimensional model presented in this article, and represents the bending moment.
A parallel bond is capable of simultaneously transmitting both forces and torques. If the maximum normal or shear force on the parallel bond exceeds its normal or shear strength, the failure of the bond will occur.
2.2. Establishment of Proppant Embedding Model
This study employs PFC2D software (version 6.0), which utilizes a two-dimensional simulation. Two-dimensional modeling offers key advantages over three-dimensional modeling, including faster computation due to fewer degrees of freedom and easier result analysis and visualization. Therefore, two-dimensional simulations are often preferred. However, it acknowledges inherent limitations in representing three-dimensional phenomena. Despite this, the manual encourages using simplified two-dimensional models throughout the modeling process to validate hypotheses and algorithms whenever possible [
37].
Research by David et al. [
38] also shows that in the stress–strain relationship, both two-dimensional (2D) and three-dimensional (3D) systems exhibit linear elastic behavior during the initial small deformation stage, with scaled deviatoric stress values being highly consistent. As deformation increases, the stress reaches a peak and then gradually decreases to a critical flow state. In this process, stress decreases more rapidly in 2D and more gently in 3D. Additionally, the peak isotropic stress is higher in 2D than in 3D, while the peak deviatoric stress is lower in 2D than in 3D. At the critical state, the isotropic stress levels are similar in both 2D and 3D, but the critical deviatoric stress value is slightly higher in 3D.
A script was written based on the particle flow code (PFC 2D) to meet the requirements of the numerical simulation. Within the numerical rock sample model, after the calibration of micro-parameters, a hydraulic fracture with specific dimensions (0.04 m in length and 0.005 m in width) was preset. Numerical proppants were then arranged inside the hydraulic fracture at a specific packing density, as depicted in
Figure 4. In the
Figure 4, black disks represent rock particles, brown disks represent proppant particles, blue disks signify fracture surface particles, and green lines illustrate the connections between rock particles. The surface particles of the fractures and the rock particles are classified into different groups so as to track and monitor the relative position changes in the surface particles of the fractures during the fracture closure process. A servo mechanism is used to apply the minimum horizontal principal stress to the numerical rock sample model. Subsequently, the embedding process of numerical proppants within hydraulic fractures is simulated and studied under different conditions. In conjunction with laboratory physical experiments, the accuracy of the numerical model was calibrated, systematically and comprehensively revealing the influence of proppant parameters and geostress parameters on the proppant embedment mechanism [
39].
2.3. Calibration of Parameters for Numerical Rock Samples
A core sample was taken from Well A at a depth of 2260 m in the Yichuan–Huanglong coal reservoir. The core was processed into standard samples with a height of 50 mm and a diameter of 25 mm. Using a triaxial rock mechanics servo testing system, a uniaxial compression test was conducted under a confining pressure of 0 MPa. The mechanical parameters, including elastic modulus, Poisson’s ratio, and compressive strength, were measured, as shown in
Table 1.
To ensure consistency between the numerical simulation and actual physical phenomena, we conducted a uniaxial compression numerical simulation to select appropriate micro-parameters for the numerical rock sample model. Using the uniaxial compression test as an example, a script was developed in the particle flow software (PFC) to generate a rectangular wall with a height of 50 mm (the height of the core) and a width of 25 mm (the core diameter). Inside the wall, circular particles of specific sizes and quantities were arranged in a certain pattern. The linear parallel bond model was used to bond the particles together, and internal unbalanced forces were eliminated. Stress was then applied to the upper and lower walls (green lines) to replicate the uniaxial compression rock mechanics experiment. During the application of stress, the internal contact bonds in the numerical rock sample break, generating a fracture (represented by red short lines). A script was used to monitor the stress–strain curve and calculate macroscopic mechanical parameters such as Young’s modulus, Poisson’s ratio, and compressive strength.
Before conducting parameter calibration, it is first necessary to discuss the influence of the main mesoscopic parameters in the model on mechanical parameters such as the compressive strength, Young’s modulus, and Poisson’s ratio of the numerical core. Based on the established numerical core model, with other parameters fixed, adjust the values of main mesoscopic parameters (including tensile strength of contact bonding pb-ten, cohesive force of contact bonding pb-coh, stiffness ratio kratio, and Effective Modulus emod), respectively, to explore the sensitivity of the mesoscopic parameters. The main microscopic parameters of the model are shown in
Table 1, and the results are presented in
Figure 5,
Figure 6,
Figure 7 and
Figure 8, respectively.
When using experimentally measured mechanical parameters such as compressive strength, Young’s modulus, and Poisson’s ratio as fitting parameters to calibrate the mesoscopic parameters of numerical cores, the results that fully match the experimentally measured rock mechanical parameters are not necessarily unique. Therefore, it is necessary to compare the internal crack morphology generated during uniaxial compression of numerical cores with that of actual cores to determine the uniqueness of the fitting parameters. The fracture patterns from the uniaxial compression experiments in the laboratory and the numerical simulation were then compared and analyzed, as shown in
Figure 9. The rock sample predominantly exhibited diagonal fractures, with the red line segments in the figure delineating the regions where fracture and failure occur within the rock model. The fracture patterns observed in the numerical rock sample align closely with those induced by uniaxial compression during laboratory experiments.
Table 2 presents the final calibration results of the numerical rock sample, encompassing both macroscopic and microscopic parameters. Notably, among the simulated elastic modulus, Poisson’s ratio, and compressive strength, the macroscopic parameters derived from simulations are within 5% of experimental findings, suggesting that this numerical rock sample model can accurately represent a real reservoir rock sample. Future investigations will utilize these microscopic parameters as a benchmark to establish a particle-embedding numerical simulation model aimed at exploring how particle embedding influences fracture width within targeted blocks.
2.4. Model Scale Effect
In the particle discrete element numerical simulation method, the size of the sample model has a certain impact on the test results. The base model size is 0.05 × 0.1 m, and the particle size ranges from 0.0000332 to 0.00002. Based on the model with completed parameter calibration, the sample was scaled down by 2.5 times, 5 times, 10 times, 15 times, and 20 times, respectively, and the particles were also scaled down by the same respective factors to investigate the influence of size effect on the mechanical parameters of the model. The results are shown in
Figure 10,
Figure 11 and
Figure 12.
The results show that when the size was scaled down by 2.5 times, the compressive strength of the model was 25.90 MPa, Young’s modulus was 2.45 GPa, and Poisson’s ratio was 0.082. When scaled down by 5 times, the compressive strength was 27.20 MPa, Young’s modulus was 2.51 GPa, and Poisson’s ratio was 0.056. When scaled down by 10 times, the compressive strength was 29.42 MPa, Young’s modulus was 2.61 GPa, and Poisson’s ratio was 0.045. When scaled down by 15 times, the compressive strength was 32.11 MPa, Young’s modulus was 2.68 GPa, and Poisson’s ratio was 0.039. When scaled down by 20 times, the compressive strength was 35.46 MPa, Young’s modulus was 2.76 GPa, and Poisson’s ratio was 0.037. As the scaling-down factor increased, the compressive strength and Young’s modulus increased to a certain extent, while Poisson’s ratio decreased to a certain extent. Based on the scale effect analysis, the particle size used in calibration should also be used in subsequent model establishment.
2.5. Verification of Proppant Embedded Particle Flow Model
A total of 220 proppant particles (20–40 mesh) were placed in a 0.04 mm long fracture, achieving a proppant concentration of approximately 3 kg/m2. Using a script to create a FISH function, the placement of the proppants and the changes in fracture width during the closure process were monitored under closure stresses of 15 MPa, 20 MPa, 25 MPa, 30 MPa, and 35 MPa, respectively. The conditions were simulated for both steel and rock plates, and the average fracture width under different conditions was calculated.
To validate the accuracy of the model, this study used a displacement sensor in a conductivity experimental device to measure the width of fractures at different closure pressures in experiments involving 20–40 mesh ceramsite. Full-diameter coal core samples were taken from Well X at a depth of 2260 m, and 10 rock slabs were machined with dimensions of 177 mm in length, 37 mm in width, and rounded ends with a diameter of 37 mm. Proppant embedment was verified by placing 20–40 mesh coated ceramite with a sand laying strength of 3 kg/m2 and a steel plate or rock slab into the API conductivity experimental device and applying a closing stress of 15–35 MPa.
As shown in
Figure 13, panels (a) and (b) illustrate the tests for proppant embedment in rock and steel plates, while panels (c) and (d) depict the simulation of proppant embedment in steel and rock plates.
Figure 14 depicts the curves of average fracture width obtained from laboratory experiments, alongside the simulated average fracture width as a function of closure pressure. The data in the figure indicate a close alignment between the experimental results and those from the numerical simulations, with an error margin of less than 5%. The average difference between the steel plate experiments and the simulated fracture width is approximately 0.00006 m, while the average difference between the rock plate experiments and the simulated fracture width is approximately 0.00005 m. This consistency serves to validate the correctness of the model. Building on this validation, subsequent research will use this model for numerical simulations concerning proppant embedding.
In practical scenarios, proppant injected into fractures exhibits uneven placement, with higher concentrations in some areas and lower concentrations in others, and this can be approximately classified into single-layer and multi-layer placement patterns. Additionally, fractures in real-world applications are relatively large, allowing observation of the proppant placement effect, which is characterized by a gradual reduction in the number of layers, from the near-wellbore region to the far-wellbore zone. This enables a comprehensive assessment of how proppant distribution at all positions within actual fractures influences proppant embedment.
However, experimental and simulation studies simplify the problem by focusing on an arbitrary segment along the fracture length, thereby neglecting variations in proppant distribution across the entire fracture length. Consequently, the results from these studies only reflect the impact of local conditions and cannot fully capture the influence of proppant distribution within actual fractures on proppant embedment.
2.6. Calculation of Fracture Width and Embedding Depth
During the investigation of proppant embedment, while calculating the average fracture width provides a qualitative assessment of whether proppants are embedded in the fracture surface, it does not clarify the underlying embedment mechanisms. Therefore, this article establishes key technical methods for characterizing fracture width and embedding depth to observe changes across the entire fracture surface during the closure process under different proppant filling schemes.
Figure 15a illustrates the theoretical model of rock plate embedment, while
Figure 15b represents the theoretical model for steel plate simulation. In these illustrations, the blue disk symbolizes the fracture surface particles, the gray disk represents the proppant particles, and the blue straight line denotes the steel plate.
The formula for calculating fracture width in simulations of rock plates and steel plates is presented as follows.
In Equation (12), represents the width of the fracture at any position on the rock plate simulation, in meters; represents the vertical coordinate of any rock particle on the upper fracture surface along the fracture length, in meters; represents the vertical coordinate of any rock particle on the lower fracture surface along the fracture length, in meters; represents the radius of any rock particle on the upper fracture surface along the fracture length, in meters; and represents the radius of any rock particle on the lower fracture surface along the fracture length, in meters.
In Equation (13), represents the average fracture width of the rock plate simulation, in meters, while L represents the length selected for the model along the fracture length, also in meters.
In Equation (14), represents the average fracture width of the steel plate simulation, in meters; represents the fracture width at any position along the surface of the steel plate simulation, in meters; represents the vertical coordinate at any point along the length of the fracture on the upper surface of the steel plate, with a constant denoted as C1, in meters; and represents the vertical coordinate at any position along the length of the fracture on the lower surface of the steel plate, with a constant represented as C2, in meters.
The formulae for calculating the embedding depth
and the average embedding depth
of the proppant at any position along the fracture length direction is presented as follows.
The formula for calculating the embedding degree
is as follows.
Based on this, a length of 0.04 m along the fracture direction is selected as the research object. Using a single-layer particle embedding model as an example, a PFC script file is developed to track and monitor the changes in particle positions on the fracture surface. This enables the dynamic monitoring of the fracture surface during the closure process. The functional relationships between the fracture length, propped fracture width, and embedding depth are illustrated in
Figure 16 and
Figure 17 below. In
Figure 16, the orange curve represents the trajectory of the upper fracture surface, while the black dashed line indicates the trajectory of the upper steel plate. The blue curve depicts the lower fracture surface, and the green dashed line represents the trajectory of the lower steel plate. The difference between the orange curve and the blue curve in
Figure 16 is the simulated fracture width of the core, corresponding to the purple curve in
Figure 17. The difference between the black dashed line and the green dashed line in
Figure 16 represents the simulated fracture width of the steel plates, corresponding to the red dashed line in
Figure 17. Additionally, the difference between the red dashed line and the purple curve in
Figure 17 represents the embedding depth of the proppant into the fracture surface. Subsequently, this method will be used to study the dynamic changes in fracture width and proppant embedding depth during the fracture closure process, providing a foundation for understanding the embedding mechanism of proppants.