Geohazard Risk Reduction Technologies in Geotechnical Engineering
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Hong Zhang, Wei Liao, Junbo Lin, Bang Zhang, Haoran Feng, "Correlation Analysis of Macroscopic and Microscopic Parameters of Coal Measure Soil Based on Discrete Element Method", Advances in Civil Engineering, vol. 2019, Article ID 1302682, 14 pages, 2019. https://doi.org/10.1155/2019/1302682
Correlation Analysis of Macroscopic and Microscopic Parameters of Coal Measure Soil Based on Discrete Element Method
Abstract
Numerical simulation of the triaxial test of coal measure expansive soil distributed along the highways in Pingxiang District, Jiangxi, was carried out by means of discrete particle flow, during which the macromechanical properties and the formation and developmental patterns of shear displacement field of the coal measure expansive soil were studied from a mesoscopic perspective. The result showed that the macroscopic stress and strain of test specimens can be significantly influenced by the interparticle friction coefficient of the coal measure expansive soil. Peak value of the deviatoric stress of test specimens increased with increasing friction coefficient, and before reaching the deviatoric stress peak value, the stressstrain relationship of the soil body basically presented a linear variation trend; the soil interparticle contact stiffness varied hyperbolically with the deviatoric stress peak value of test specimens, and the increasing contact stiffness ratio led to a gradual decrease of the deviatoric stress peak value but had only a small impact on the residual strength of test specimens; confining pressure was found to have remarkable influence on both the deviatoric stress peak value and the residual strength of test specimens; when the experimental confining pressure increased from 0.2 MPa to 1.2 MPa, the deviatoric stress peak value and the residual strength of test specimens increased by 2.14 times and 5.11 times, respectively. This paper reveals the macroinstability and failure mechanism of coal measure expansive soil from a microperspective.
1. Introduction
Coal measure soil mostly appears ash black in appearance, while the soil mass exposed is greyish with weak interlayer bonding and loose structure. Since coal measure soil is easily weathered and disintegrated with poor water stability after excavation, large gullies are likely to be caused by water and soil loss during heavy rain. Therefore, an urgent problem which should be solved currently is how to handle and utilize engineering with coal measure soil. Some researchers at home and abroad have researched problems and reinforcement measures for engineering with coal measure soil [1–3]. Nevertheless, characteristics of engineering with coal measure soil and causes of the abovementioned problems are rarely documented. Focusing on the coal measure soil along the GuangzhouWuzhou expressway, Hu et al. [4] determined the shear strength of coal measure soil under different water contents and its influence law with the routine straight shear test. Zhu et al. [5] established a mathematical model regarding the stability of the slope infiltrated by rainfall and analyzed the influence of cracks and weathered layers on slope stability using the limit equilibrium method together with the shear strength theory of unsaturated soil. Zhang et al. [6] simulated and analyzed the slope stability of coal measure soil with different cracks and weathering degrees under rainfall infiltration using the transient unsaturated seepage software based on some secondary slope of DaqingGuangzhou expressway in Jiangxi. Li and Liu [7] took the red clay and powdered coal measure soil in hilly and mountainous areas of southwestern China as the objects of study to investigate the influencing rule of different water contents on parameters such as the cohesion, internal friction angle, and shear strength using the common straight shear test. Yang and Zheng [8] determined the soilwater characteristic curve for samples of remolded unsaturated coal measure soil with different dry densities using a soil moisture characteristic curve meter, and they fit the data measured with the VG model. Most of the abovementioned documents tend to research from the perspective of macromechanics. However, macromechanical property is a symbol of parameter changes in the microstructure of soil mass. In that case, the slope of coal measure soil can be considered as a system comprised of soil particles in different sizes. Those soil particles in the system are discrete, and the interaction between the particles is characterized by nonlinear dissipation. To be specific, it is the micromechanical behavior of particles inside the system that determines many macromechanical properties of the slope. Hence, microscopic analysis must be performed on the composition of particle structure of the slope soil and distribution characteristics of contact force chain and movement characteristics of particles, so as to disclose the mechanism of macroscopic static and dynamic features shown by the granular system of the slope of coal measure soil [9–14].
In 1979, Cundall and Strack [15, 16] proposed the distinct element method (DEM), which has gradually become an effective tool to study the microstructures of granular systems. Many scholars modeled typical soil mechanics experiments (e.g., biaxial compression and direct shear tests) using the discrete element method [17–23]. The unloading of silos is a typical bulk flow process. After the appearance of the discrete element method, Langston et al. [24–29] used DEM to study hopper unloading. In the field of complex soil dynamics or machinesoil dynamics, some scholars use the discrete element method to simulate the excavation, drilling, shoveling, penetration, and pipeline laying processes [30–36].
A large amount of coal measure strata containing montmorillonite and illite are distributed along the PingxiangLianhua expressway in Jiangxi. As a result, expansive soil can be found in coal measures. Nonetheless, few researches on mechanical properties of the expansive coal measure soil have been reported currently. In this paper, the discrete element method (DEM) is employed to have a 3D numerical simulation of the triaxial test on the expansive coal measure soil, to probe into the influencing rule of parameter changes of the micromechanic structure of the soil mass particles on macromechanical characteristics of the expansive coal measure soil, and to discuss the formation and development law of the shear displacement field of the expansive coal measure soil. The research findings can provide theoretical references for the protective slope design and construction of the expansive coal measure soil.
2. Principles of Discrete Element Method
2.1. Physical Equations
The discrete element method (DEM) is to consider objects of research as an integral whole consisting of a finite number of discrete particles, in which each particle is idealized as a rigid body and deemed as a discrete calculating unit. The particles are independent of each other with contact and friction. Assuming that the normal contact forces between two contact solid elements are directly proportional to the normal relative displacement between them, the following algebraic relation can be obtained [37]:where is the normal stiffness of the distinct element; is the normal displacement of the distinct element; and is the unit normal vector over the contact surface.
The tangential contact force between granular particles is defined as the shear force whose size is closely related to the movement track of the particles and their loading history. In this paper, the shear force between granular particles is expressed in the form of increment. When a contact is formed between granular particles, the total tangential contact force between the particles is assumed to be initialized to zero. And the increment of the tangential contact force resulting from the relative displacement between the particles is accumulated in each cycle of calculating time steps. The calculating relationship can be expressed as follows:where is the shear stress increment between distinct elements in each calculation step; is the tangential contact stiffness of the distinct element; and is the increment of the tangential relative displacement of the distinct element.
2.2. Equations of Motion
Based on equation (2), the resultant force and the resultant moment imposed on granular particles after the accumulation of each calculation of time steps are calculated. After that, the acceleration and the rotational angular velocity of granular particles are calculated according to Newton’s second law. Thus, physical quantities such as velocity, linear displacement, and angular displacement of the granular particles in the calculation period can be known. If the resultant shearing force acting on the granular particles in the direction of at the moment of is assumed as , the motion of granular particles can be expressed by the following two equations:where is the average acceleration of granular particles at the moment of in the direction of ; is the rotational acceleration of granular particles at the moment of in the direction of ; is the mass of granular particles; is the bending moment of the resultant force acting on the granular particles; and is the rotational inertia of granular particles.
2.3. Particle Contact Constitutive Model
Since many coal particles are contained in expansive coal measure soil, especially that in the weathering layer of the slope is loose, it results in weak cohesive force between the soils. The shear strength is formed primarily by the internal friction between soil particles. Therefore, a contact sliding model can be utilized to describe the constitutive relationship between the normal force and the tangential shear force interacting between particles. The normal tension between particles is neglected in the contact sliding model. The sliding motion between particles only occurs under set conditions, that is, the shearing force actually generated between particles should be greater than the preset threshold; also, the sliding between particles must be performed within a certain range of shear strength. Assuming that the displacement overlapping between two particles is less than or equal to zero, it can be considered that the two particles have no contact or their contact force is zero. In this way, their constitutive behavior can be described aswhere is the friction coefficient between particles. If so, then the particles will slide. Meanwhile, in the next cycle step, will be
3. Numerical Simulation of Particle Flow of Expansive Coal Measure Soil
A particle flow calculation model is firstly established in this paper according to the actual particle size range of the soil mass by assuming that particles of the soil mass are rigid materials. Meanwhile, the above contact sliding model is used to indicate the particle interaction. After simulating the stressstrain relationship of test pieces in the triaxial test by changing microscomic parameters of particles, the results obtained are compared with those from the laboratory triaxial test. Finally, microscomic parameters of the soil particles that can reflect macromechanical properties of the soil mass are determined through numerous trial calculations and analyses. Furthermore, the calculation model is taken as a basic model for analyzing the influencing law of changes of particle microscopic parameters on macroscopic characteristics of the expansive coal measure soil.
3.1. Principles of Numerical Calculation of the Triaxial Test
The key to the calculation principle of numerical simulation in the triaxial test is to calculate the stress state of the test piece in the loading process along with stress control. While the test piece is loaded by controlling the movement velocity of the bottom plate and the top plate of the model constraint boundary in the triaxial test that is simulated with the discrete particle flow program [38]. The stress of the test piece can be obtained by dividing the resultant force of all the forces acting on the test piece by the area of the corresponding test piece. The strain of the test piece in the directions of and can be obtained as follows:where is the current length of the test piece in the corresponding direction and is the original length of the test piece in that direction. Concerning the cylindrical test piece, the axial strain and the radial strain can be expressed as follows:
Servo functions can be called in the cycle of calculating the time steps to reduce the difference between the monitoring stress and the preset stress in the calculation of numerical simulation. The numerical servo functions are adopted to adjust the velocity of conducting lateral restraint against the wall of the test piece, so that the restraint stress can be inclined to a certain constant. The numerical servo functions are achieved by the following algorithms; the velocity of boundary restraint can be expressed as follows:where is the velocity of laterally restraining the wall and is an “incremental” parameter obtained through the following method.
Assuming that the increment of the binding force generated in the movement of lateral wall restraining within a calculated step can be expressed as follows:where is the number of contact surfaces on the constraint boundary and is the average stiffness of these contact surfaces. Therefore, the average increment of restraint stress iswhere is the area of regions involved in the constraint boundary. In order to achieve stable test loading in the numerical simulation of the triaxial test, the absolute value of the variable of restraint stress must be smaller than the difference between the monitored value and the preset value. Amplification of coefficients is adopted in the simulation of actual numerical simulation. is assumed as an amplification coefficient. To guarantee the loading stability, we may havewhich leads towhere , , , and ; thus,
Eliminate by taking and , we can obtain
The following equation can be obtained by transposing the inequation:
Therefore, the increment can be determined by the following equation:
In general, is taken in actual simulated calculations.
3.2. Test Materials and Laboratory Triaxial Test
The test soil samples source from the slope of original coal measures at K12 + 110 in A2 section of WanzaiYichun expressway in Jiangxi. Natural physical and mechanical indexes of the samples are as follows: the average density of soil particles is 2230 kg/m^{3}; the average natural density is 1680 kg/m^{3}; the natural porosity is 0.32; and the moisture content W of the test pieces is 18.2%. The distribution of particle contents in different particle size ranges of the expansive coal measure soil can be obtained by conducting particle grading test on the samples with the sieving method and the mixed method, as shown in Table 1. Soil particles mainly range from 0.25 to 10 mm, accounting for 85.41%; with d_{10} = 0.129, d_{30} = 0.58, and d_{60} = 1.27; the nonuniform coefficient C_{u} is 9.84; and the curvature coefficient C_{c} is 2.08. The SLB1 triaxial shear permeameter manufactured by the Nanjing Soil Instrument Factory is used in the test which takes unconsolidatedundrained (UU) shearing. The test pieces are 40 mm in diameter and 80 mm in height. The triaxial shear test is conducted under the ambient pressure of 0.1 MPa, 0.3 MPa, and 0.6 MPa, respectively.

3.3. Numerical Modeling of Triaxial Test and Determination of Microscopic Parameters
Sizes of numerical modeling and particle simulation are magnified to save time for calculation and improve the efficiency of analysis. The numerical model of the triaxial test is 2 meters in height and 0.8 meters in diameter. As can be known from the results of the laboratory particle grading test for expansive coal measure soil in Table 1, the particle size ranges from 0.25 to 10 mm. The particle diameter should be set within this range in modeling. And a total of 3,058 solid particles can be generated in the form of uniform distribution. The calculation model is shown in Figure 1.
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The walls on the top and at the bottom of the particle flow soil samples are driven to conduct relative movement via the numerical servo system under consolidated and ambient pressure of 0.1 MPa, 0.3 MPa, and 0.6 MPa, so as to unload the test pieces. At the same time, the ambient pressure of the test pieces can be guaranteed unchanged through adjustment of the side wall displacement before the end of loading. Numerical calculation results are approximated to the results of the laboratory triaxial test via repeated trial calculation by changing microscopic parameters of the particles. The final calibrated results of microscopic parameters of the particles are obtained, as shown in Table 2. Threeaxis simulation results calculated by DEM are compared with the laboratory test results, as shown in Figure 2. It can be seen from the figure that the peak value of the deviatoric stress calculated by numerical simulation of the triaxial test is relatively close to the laboratory triaxial test results with consistent change trends of the stressstrain curve. Thus, it indicates that the microscopic parameters calibrated finally can relatively approach the real model.

4. Correlation Analysis of Microscopic Parameters and Macroscopic Mechanics of Coal Measure Soil
4.1. Relationship between Friction Coefficients and StressStrain
The friction coefficient between particles is set as 0.1, 0.3, 0.5, 0.7, and 0.9 for numerical simulation in order to discuss the influence of friction coefficients on the macroscopic stress and strain of the expansive coal measure soil. Microscopic parameters of other particles in the calculation model can have assignment according to Table 1. The influencing relationship curve of different friction coefficients on stressstrain of expansive coal measure soil is shown in Figure 3.
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According to the deviatoric stressaxial strain curve in Figure 3(b), as the friction coefficient between the particles grows, the peak value of the deviatoric stress of the test piece will also increase continuously. The stressstrain relationship of the soil mass tends to be in linear change before the test piece reaches the peak. The soil mass enters the strain softening stage right after that. As can be seen from Figure 3(a), strain softening of the soil is apparent. As the friction coefficient increases, a growth of the interaction force between soil particles can be observed; and the force for overcoming the sliding between particles is also improved. Thus, there is an increase of the modulus of deformation of the soil. Certain enhancement of the residual strength of the soil can be seen with the friction coefficient after the test piece is loaded and unloaded, which, however, is insignificant. Moreover, the residual strength of the soil increases insignificantly when the friction coefficient is large.
Figure 4 presents the relationship curve between the volumetric strain and the axial strain of the test piece under different friction coefficients, indicating that the volumetric strain decreases with the increase of axial strain at the initial stage of loading, whereas particle deformation changes into tangential sliding from normal compression and overlapping between particles. Consequently, the volume of the test piece becomes smaller, macroscopically resulting in shrinkage. The volumetric strain increases with the axial strain at the later stage of loading. The test piece is slid tangentially with the increase in volume, macroscopically leading to dilatancy. The volumetric strain of the test piece is enlarged with the increase of friction coefficients.
4.2. Relationship between Contact Stiffness and StressStrain of Particles
Based on the original calculation model, the ambient pressure is 0.3 MPa; and the contact stiffness is 1 GPa, 3 GPa, 5 GPa, 7 GPa, 9 GPa, and 12 GPa, respectively. Other parameters are constant. Numerical simulation of the triaxial test specific to the test piece is conducted in 6 working conditions. The stressstrain relationships of the test piece with different contact stiffness are shown in Figures 5 and 6.
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As can be seen from Figure 5, the deviatoric stress peak of the test piece decreases with the increase of the contact stiffness of the particles. When the contact stiffness increases from 1 GPa to 3 GPa, the decline of the deviatoric stress peak of the test piece is significant; when the contact stiffness increases from 5 GPa to 12 GPa, the deviatoric stress peak of the test piece is slow; when the contact stiffness is large, the residual strength of the test piece tends to be the same value (as shown in Figure 5(a)). According to the test results of numerical simulation, with the increase of the contact stiffness between particles of the test piece, the macroscopic initial tangential modulus of the test piece will also experience an increase, while the deviatoric stress peak and the axial strain corresponding to the strength reaching the peak value become smaller, suggesting that the contact stiffness has little influence on the residual strength of the test piece.
It can be observed from Figure 6 that the deformation of the test piece is constituted primarily by normal particle compression and overlapping as the volumetric strain decreases with the increase of the axial strain at the initial stage of loading. As a result, the test piece is shrunk. The influence of the contact stiffness of particles on the shrinkage of the test piece is not obvious at the early stage. As the test piece is further loaded, its volumetric strain becomes positive and increases with the axial strain, whereas particle deformation changes into tangential sliding from normal compression and overlapping between particles and causes volume expansion, which is macroscopically manifested as dilatancy. The volumetric strain of the test piece rises with the contact stiffness of the test piece. Such increase, however, is unapparent at the later stage.
As can be seen from Figure 7 that presents calculation results of the stiffness ratio between different particles, the initial tangential modulus of the test piece at the early stage is decreased and the strength of the peak value of the deviatoric stress gradually decreases with the increase of the particle stiffness ratio, exerting little influence on the residual strength of the test piece. Furthermore, the stiffness ratio has an invisible influence on characteristics such as shrinkage and dilatancy of the test piece.
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4.3. StressStrain Relationship under Different Ambient Pressures
The stress state around the test piece in the triaxial test is changed to explore the changing law of deviatoric stress and axial strain under different ambient pressures. Ambient pressures calculated are valued as 0.2 MPa, 0.4 MPa, 0.6 MPa, 0.8 MPa, 1.0 MPa, and 1.2 MPa, while other microscopic parameters remain constant. The calculation results are shown in Figures 8 and 9.
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From Figure 8, the initial tangential modulus of the test piece is growing (the slope of the curve increases gradually) before the softening of the curve strain with the increase of the ambient pressure. In the meantime, the deviatoric stress peak and the residual strength of the test piece are also improved constantly to realize linear change. As a result, ambient pressure has appreciable influence on the residual strength of the test piece.
The relationship curve of the volumetric strain and the axial strain under different ambient pressures of the test piece is shown in Figure 9. It can be observed that the volumetric strain of the test piece is negative at the early loading stage. As the axial strain increases, the test piece is shrunk gradually, which becomes increasingly obvious with the increase of the ambient pressure. When the ambient pressure is small, the test piece is diverted to dilatancy from shrinkage. It can also be observed that the volumetric strain of the test piece constantly decreases with the increase of the ambient pressure. When the ambient pressure is small, the declining range is significant; when the ambient pressure is large, the declining range of the volumetric strain is insignificant.
4.4. Analysis of the Influence of Porosity on Shear Strength Parameters
Based on the original calculation model, the ambient pressure is set as 0.8 MPa; and the porosity of the test piece is set as 0.3, 0.35, 0.4, 0.45, and, 0.5, respectively, while other parameters maintain constant, thus to analyze the stressstrain relationships of the test piece under different porosity conditions. The simulated calculation results are shown in Figure 10. As can be seen from Figure 10(a), the porosity has certain influence on the deviatoric stress peak of the test piece. The deviatoric stress peak of the test piece is large when the porosity is small; that is, the larger the porosity is, the smaller the deviatoric stress peak of the test piece will be. Nonetheless, the porosity has an insignificant influence on the residual strength of the test piece.
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The relationship curve of volumetric strain and axial strain under different porosity conditions of the test piece is shown in Figure 10(b). It can be observed when the test piece with low porosity (samples are dense) is sheared, a shrinkage will be witnessed for the test piece with the decreased volume at the early loading stage. After that, the volume of the test piece will rapidly increase, macroscopically manifesting as dilatancy in an obvious manner, as the particles in the test piece are sheared and moved. When the test piece with high porosity (samples are loose) is sheared, its volume will decrease before the subsequent rebound, mainly manifesting shrinkage. Moreover, the volume increase of the test piece gradually decreases with the increase of porosity.
4.5. Discussion on the Evolution Law of Shear Displacement Field of Expansive Coal Measure Soil
The displacement and velocity change paths of particles in the test piece can be monitored and tracked in real time in the loading process of numerically simulating the triaxial test with the particle flow code. Moreover, the formation of the shear displacement field and the change law of the stress field of the test piece can be analyzed through elaboration of the displacement vector. Figure 11 shows the vector diagram presenting the formation and evolution of the shear displacement field of the test piece under different axial strains (calculation of time steps) when the ambient pressure is 0.6 MPa. To be specific, Figures 11(a) and 11(b) show the formation of the shear displacement vector at the initial loading stage of the test piece. It can be seen from Figure 11(a) that particles in the test piece are moved towards the central section at this time with the insignificant shape of the shear zone, indicating that the test piece is at the early stage of dilatancy. It can be observed from Figure 11(b) that the shear zone of the test piece is formed initially as loading continues. At this time, the motion of particle displacement vector approaches the direction of 45°. Whereas Figures 11(c) and 11(d) show the evolution of the shear displacement vector after the deviatoric stress of the test piece reaches the peak. Since particle motion changes from the low potential energy to the high potential energy, the directional trend of the shear displacement field becomes significant with the increase of the axial strain of the test piece. Meanwhile, the thickness of the shear zone is getting smaller in the state of instability.
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Distribution of the shear displacement field of the test piece under different ambient pressures is presented in Figure 12. It can be observed that the width of the shear displacement belt of particles is gradually narrowed as the ambient pressure increases. Analyzing the microscopic mechanism shows that it is mainly because the resistance of particle motion in the restrained test piece increases with the ambient pressure of the test piece. That is to say, the difficulty of displacing the relative sliding of the particle has also increased, which is further manifested by the enhanced deviatoric stress peak of the test piece from the macroperspective.
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5. Macroinstability of Coal Measure Soil and Micromechanism Analysis of Shear Band Localization
Cundall and Strack [39] as well as Bardet and Proubet [40] studied the localization of shear strain with the PFC discrete element analysis software. Vardoulakis and Aifantis [41] and Chambon et al. [42] theoretically explored the mechanism of production of shear zones based on the second gradient. In this paper, the author analyzed the mesoscopic mechanism of localization of shear zones with the volume fraction of particles, coordination number, and other mesoscopic parameters. The gradation of test samples in the triaxial test originated from the undisturbed coalbearing soil samples on the side slope at mark K12 + 110 of section A2 on the WanzaiYichun expressway in Yichun, Jiangxi. The gradation is shown in Table 1. The numerical model in the triaxial test was 2.0 m in height and 0.8 m in diameter; the average soil particle density was determined as 2230 kg·m^{−3}, and the natural porosity was 0.32. The values of mesoscopic parameters of the test samples were in accordance with the calibrated values in Table 2. To track the parametric variation in the particle system, a measuring sphere (MS1) outside the shear zone and one (MS2) inside the shear zone were selected to highlight the variation of volume fraction, coordination number, and other parameters within and outside the shear zone.
5.1. Macroscopic Instability of Coal Measure Soil
The results of deviator stress and volumetric strain of the test samples simulated by the triaxial test are shown in Figure 13. Figure 13(a) shows the complete process of elastoplasticity, which the particle system underwent. When the axial strain was ε < 2.0%, the deviator stress and axial strain exhibited a linear change at the macrolevel, and the particle system exhibited elastic properties. When increased, the particle system entered the plastic stage. When the axial strain was 2% ≤ ε ≤ 3.5%, the deviator stress of the test samples underwent violent fluctuations and peaked at the axial strain value of 2.4%. Later, the deviator stress gradually decreased; during this process, the test samples hardened. When the axial strain was ε > 3.5%, the particle system entered the softening stage, where the deviator stress considerably decreased, which indicated the presence of internal damage to the system. According to Figure 13(b), when the particle system was under pressure, the volumetric strain decreased to a negative value; when the particle volume fraction n increased, the stress in the system increased. When the axial strain was ε < 2.0%, the system was in an elastic strain. When the axial strain was ε = 3.2%, the volumetric strain was ε_{v} = −1.8% while the system achieved its highest density and maximum volume fraction. When the axial strain was ε > 3.2%, the volumetric strain increased and the particle system entered the plastic stage. When the axial strain was ε = 5.3%, the volumetric strain became = 0, which indicated that the volumetric strain of the system returned to the initial state. When ε > 5.3%, the volume fraction of the particle system gradually decreased while the volumetric strain experienced slight fluctuations. At the same time, the change in slope remained constant. The system experienced a dilative shear failure.
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5.2. Mesomechanism Analysis of Shear Band Localization of Coal Measure Soil
Figure 14 illustrates the relationship curve between the axial strain and volume fraction, which were measured using the measuring spheres. Figure 14 shows that the volume fraction n of both MS1 and MS2 gradually increased at first, while the particle system remained at the elastic stage, which was represented as shrinkage. When the axial strain was 2% ≤ ε ≤ 3.2%, the volume fraction at the shear zone (MS2) remained the same at 65.38%, with the system shifting to the hardening stage. When ε = 3.2%, the MS2 volume fraction n exhibited a slight decrease with a small range of variation and the particle system may have internally developed small cracks. The MS2 volume fraction n exhibited only minor changes before ε < 4.5%. When ε = 4.5%, the MS2 volume fraction n progressed in a sustained decline and the system entered the critical state, which indicated the growth of the dominant shear zone. When the axial strain increased, the inshear zone (MS2) volume fraction n exhibited an overall downward trend with occasional small upward and downward deviations, which implies that the dilatancy of the particle system was primarily caused by the loose arrangement of particles within the shear zone. The varying pattern of the outershear zone (MS1) volume fraction was similar to that of MS2.
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Figure 15 shows the variation curve of the coordination number and axial strain. It is observed that when the axial strain was ε < 2%, as the loading process of the entire particle system continued, the coordination number Z gradually increased. When 2% ≤ ε ≤ 4.5%, the coordination number Z of MS1 and MS2 exhibited small oscillations, and the maximum coordination number of MS1 was 5.5 and that of MS2 was 5.84. When ε = 4.5%, the coordination number Z of MS1 and MS2 clearly decreased, which indicates the increase in porosity in the central area of the particle system. Meanwhile, the volumetric strain gradually increased from the minimum, which indicates a clear dilatancy of the entire particle system during the softening stage. When the axial strain was ε = 5.8%, the coordination number of the particle system increased again. Therefore, it was concluded that the dilative shear failure of the particles included slippage between the particles and angular displacement, which was generated by particle rotation. When the axial strain was 7.5%, the coordination number of the particle system remained practically unchanged and the coordination numbers of MS1 and MS2 were 4.7 and 5.1, respectively.
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6. Conclusions
Based on the theory of discrete element method (DEM), this paper performed numerical calculations on the triaxial test of expansive coal measure soil as well as simulated the macromechanical properties of the coal measure soil as well as the formation and development of the shear displacement field from the perspective of particle microscopic parameters, from which, results similar to the laboratory test can be obtained. By analyzing microscopic parameters of the particles and the influencing law of the macroscopic stressstrain curve of the expansive coal measure soil, the following conclusions can be made.(1)The friction coefficient between soil particles exerts a significant influence on the macroscopic stress and strain of the test piece. As the friction coefficient between particles grows, the deviatoric stress peak of the test piece also increases continuously. The stressstrain relationship of the soil mass tends to be in linear change before the test piece reaches the peak. The soil mass enters the strain softening stage immediately after reaching the peak, whereas the increase in the residual strength of soil mass is not obvious when the friction coefficient is large.(2)The contact stiffness between particles increases, whereas the deviatoric stress peak of the test piece decreases, basically presenting a hyperbolic change. When the contact stiffness ratio increases, the deviatoric stress peak of the test piece will decrease gradually with nearly no effect on the residual strength of the test piece. Meanwhile, the stiffness ratio has insignificant effect on characteristics such as shrinkage and dilatancy of the test piece.(3)The deviatoric stress peak and the residual strength are significantly affected by the ambient pressure in the test. By analyzing from the microscopic mechanism, it is mainly a result of the resistance increase of particle motion in the restrained test piece with the ambient pressure of the test piece. That is to say, the difficulty of displacing the relative sliding of the particle has also increased, which is further manifested by the enhanced deviatoric stress peak of the test piece from the macroperspective.(4)The monitoring of volume fraction and coordination number in shear band shows that the volume fraction in shear band of coal measure soil decreased with the increase of axial strain when the granular system was in the softening stage, which indicated that the dilatancy behavior of the granular system was basically caused by the loose distribution of particles in the shear band. At the same time, the coordination number began to decrease significantly, indicating that the porosity in the central region of the particle system began to increase, and the dilatancy failure behavior of the particles included not only the slip between the particles but also the angular displacement caused by the rotation of the particles.
Data Availability
The data used to support the findings of this study are available from the corresponding author upon request.
Conflicts of Interest
The authors declare that there are no conflicts of interest regarding the publication of this paper.
Acknowledgments
This study was supported by the National Natural Science Foundation of China (Grant no. 51609114), the Science and Technology Project of Jiangxi Education Department (Grant no. GJ161101), and the Superiority Science and Technology Innovation Team Project of Nanchang City (Grant no. 2017CXTD012).
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