Acoustic Emission Simulation on Coal Specimen Subjected to Cyclic Loading

Duan, Huiqiang; Ma, Depeng

doi:https://doi.org/10.1155/2020/3798292

Advances in Civil Engineering

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Research Article | Open Access

Volume 2020 | Article ID 3798292 | https://doi.org/10.1155/2020/3798292

Acoustic Emission Simulation on Coal Specimen Subjected to Cyclic Loading

Huiqiang Duan¹and Depeng Ma²

Academic Editor: Chunshun Zhang

Received06 Nov 2019

Revised13 May 2020

Accepted23 May 2020

Published29 Jun 2020

Abstract

The damage and failure state of the loaded coal and rock masses is indirectly reflected by its acoustic emission (AE) characteristics. Therefore, it is of great significance to study the AE evolution of loaded coal and rock masses for the evaluation of damage degree and prediction of collapse. The paper mainly represents a numerical simulation investigation of the AE characteristics of coal specimen subjected to cyclic loading under three confining pressures, loading-unloading rates, and valley stresses. From the numerical simulation tests, the following conclusions can be drawn: (1) The final cycle number of coal specimen subjected to cyclic loading is significantly influenced by the confining pressure, followed the valley stress. With the increase in confining pressure or valley stress, the cycle number tends to increase. However, the loading-unloading rate has a little influence on it. (2) The AE counts of coal specimen subjected to cyclic loading are greatly influenced by the confining pressure and the valley stress. With the increase in the confining pressure, the cumulative AE counts at the 1st cycle tend to increase but decrease at a cycle before failure; with the decrease in the valley stress, the cumulative AE counts per cycle increase in the relatively quiet phase. However, the loading-unloading rate has a little influence on it. (3) The failure mode of coal specimen subjected to cyclic loading is significantly influenced by the confining pressure. Under the uniaxial stress state, there is an inclined main fractured plane in the coal specimen, under the confining pressures of 5 and 10 MPa, the coal specimen represents dispersion failure. The loading-unloading rate and valley stress have little influence on it. (4) The AE ratio is proposed, and its evolution can better reflect the different stages of coal specimen failure under cyclic loading. (5) The influence of confining pressure on the broken degree of coal specimen subjected to cyclic loading is analyzed, and the higher the confining pressure, the more broken the failed coal specimen.

1. Introduction

In underground coal mining, many types of coal pillars need to be set. In addition to the static loading, these pillars have also been subjected to the repeated stress induced by mining and excavation. Under these stresses, the damage of coal pillars increases and the strength decreases, eventually very likely leading to collapse. Especially in deep mine, the failure of coal pillars often occurs in the form of rock burst [1–3]. Therefore, it is of great significance to study the precursory characteristics of coal mass failure for the safe production of coal mine. According to the research of the German scholar Kaiser, the loaded rock or materials release strain energy in the form of elastic wave, and this phenomenon is called acoustic emission (AE) [4–8]. The AE signals have been proved to be an important manifestation form and feedback of rock deformation and fracture [9–13]. Since the AE signals contain abundant precursory information of rock damage, the internal state and damage degree of rock can be predicted and evaluated by analyzing the characteristics of AE signals [14–17]. Therefore, to research the AE evolution law of coal mass from damage to failure under repeated stress is an important means to prevent coal mine from disasters and accidents.

Now, many research achievements have shown that there are two AE effects, namely, Kaiser and Felicity effects. Both effects are an indirect reflection to the damage and failure state of the loaded rock and closely related to the rock structure and loading conditions [18–20]. Besides, the rock types and test conditions have a significant influence on the AE characteristics. For example, Liu et al. [21] studied the AE characteristics of muddy sandstone under one full freeze-thaw loading cycle through triaxial seepage tests. The variation of rock permeability corresponds well to AE amplitude. AE signals are not active in the initial loading stage under higher confining pressure; on the contrary, the maximum values of AE energy and amplitude increase during the whole test. Su et al. [22] investigated the AE evolution of granite rock specimens in true triaxial rock-burst tests. On the eve of the rock burst, the “quiescent period” could be observed in the evolution of the AE hits, the time-dependent fractal dimensions of the AE hits continuously decrease, and the main frequency of the AE showed decreasing trends. Thus, the evolution of AE signals can be used as key information for rock-burst prediction. Tian et al. [23] researched the AE properties of sedimentary rocks subjected to the high-velocity waterjet impingement loading. They found that there are obvious differences in AE signal frequencies between the fluid dynamics and the rock failure. The main frequencies of the rock failure are within the range of 100–200 kHz, while the frequencies of the fluid dynamics are below 50 kHz. Wang et al. [24] studied the AE characteristics in karst limestone failure under uniaxial and triaxial compression. The AE activity of rock under triaxial compression differs from that under uniaxial compression. In the uniaxial compression test, the peak AE activities occur near the peak stress of the rock. In the triaxial compression test, the AE activities of the rock samples first decreased and then increased with an increase in the confining pressure, and the AE activity exhibited a certain lag, the AE peak appears at a sharp stress decrease and rock macroscopic failure. Zhang et al. [25] studied the acoustic emission characteristics of salt rock under uniaxial conventional compression and cyclic loading. Compared with conventional compression, the cyclic loading weakens the AE events of rock. The Kaiser effect is mainly dependent on rock properties and loading condition. Fan et al. [26] studied the AEs from salt in conventional fatigue tests (CFTs) and discontinuous cyclic loading tests with the zero loading stress intervals (ZLIs). In the CFTs, the AE counting rate decreased gradually and reached a plateau before a rapid increase prior to the failure. In the ZLI tests, the AE activity evolution with time is very strongly dependent on the ZLI length and increases with its growth. Some other scholars have also carried out abundant research on the AE characteristics of different types of rocks under varying loading conditions [15, 27–33].

Through analysis of existing literatures, many achievements have been obtained on the AE characteristics of high-strength rocks subjected to cyclic loading. Because there are abundant microdefects in coal mass, it is difficult to process it into a standard specimen, and so the cyclic loading test on a coal specimen is relatively deficient. As is known to all, lab tests do be the main method to study the AE characteristics of rock materials. But, in lab tests, the specimen can be used for only one destructive test without the repeatability, which leads to the poor accuracy of the test results. As for coal specimens with great discreteness in mechanical properties, the accuracy of lab tests is even worse. Besides, the lab tests are also limited by the test conditions and costs, and sometimes difficult to carry out. Thus, the numerical simulation method has gradually become a popular way in solving the problems on rock mechanics for its repeatability, easy implementation, high efficiency, and low cost [34]. Based on the above, in this paper, first, the AE characteristics of coal specimen subjected to cyclic loading are studied by using Particle Flow Code (PFC), and then, the AE characteristics and damage evolution of coal specimens are explored.

2. Establishment of the Model and Calibration of Meso-Parameters

2.1. Introduction of PFC

PFC is computing software developed by Itasca Company, USA. It has been widely used in the study of basic mechanical properties of rock materials, medium fracture, and crack development. The basic principle of PFC comes from the molecular dynamics, which studies the mechanical properties and behavior of the medium from the point of view of micro-structure [35].

There are two basic units in PFC, namely, particle and wall. The particles are used to form the research object. The walls are as a constraint to control the movement of particles. There are two contact models in PFC: linear model and linearpbond model. In the linear model, the contact between two particles is abstracted as an infinitesimal-sized plane, and the mechanical behavior of the contact plane is described by using spring elements and damper elements, which are parallel to each other. The spring element describes the linear elasticity of the contact plane, and the damper element describes the viscous properties. Because the contact plane is infinitely small sized, it can only transmit force. The linearpbond model adds bonding property on the basis of the linear model. Because the bonding element is in parallel with the spring element, this bond is also called a parallel bond. The parallel bond can be abstracted as a bonding material with constant stiffness and certain strength between two particles. The strength properties of parallel bond conform to the Mohr-Coulomb criterion. When the bond is destroyed, the linearpbond model changes from the bonding state to unbonding state, and the properties of nonbonding linearpbond model is identical with the linear model. Because the contact plane of the linearpbond model has a certain size, it can transfer force and moment.

2.2. Establishment of the Numerical Model

In this paper, the PFC 2D software is employed and the bonded particle model (BPM) is used to simulate the AE properties of coal specimens. The established model height is 100 mm, with a width of 50 mm. In the simulation test, the smaller the particle size, the more accurate the simulation results, but this also significantly reduces the computing efficiency. If the particle size is too large, the reliability of simulation results is worse and difficult to reflect the real mechanical properties of specimens. Therefore, in the numerical simulation, it is necessary to make a trade-off between computing accuracy and efficiency to determine the reasonable number and size range of particles.

The research achievements show that when the average particle size is less than 2.5% of the model minimum length, the better simulation results can be achieved [36]. In addition, the critical time-step of the model can be expressed as follows [35]:where m is the mass; k^tran and k^rot represent the translational and rotational stiffness, respectively; and I is the moment of inertia of the particle.

The model components in PFC are conceptualized as a collection of discrete bodies (composed of disk shaped balls/pebbles in 2D; spherical balls/pebbles in 3D) and springs. Each body may have a different mass, and each spring may have a different stiffness. A critical time-step is found for each body by applying equation (1) separately to each degree of freedom, assuming that the degrees of freedom are uncoupled. The stiffness is estimated by summing the contribution from all contacts using only the diagonal terms of the contact stiffness matrix. The final critical time-step is taken to be the minimum of all critical time-steps computed for all degrees of freedom of all bodies [35].

Equation (1) shows that if there is a large difference in particle size, the computing efficiency of numerical simulation will be greatly reduced.

Through repeated debugging and considering the time cost, the size range of particles in the model was determined to be from 0.35 mm to 0.55 mm. There generated 6945 particles in all. The linearpbond contact model is used between particles. The established model is shown in Figure 1. Four walls are generated around the model; the top and bottom are loaded walls, and the left and right are servo walls (deleted in uniaxial simulation). The linear contact model is used between walls and particles. In order to eliminate the end-restraint, the friction coefficient is set to 0.

2.3. Lab Test and Meso-Parameters Calibration

2.3.1. Lab Test

The big block of coal samples were from No. 16 upper coal seam of Yangcun Mine’s No. 10602 coal face in Shandong, China. Each sample was processed into several standard cylindrical specimens with a diameter of 50 mm and a height of 100 mm, which is suggested by the International Society for Rock Mechanics (ISRM). Conventional compression tests were conducted using the MTS815.02 rock-mechanics test system (MTS Systems Corporation, Eden Prairie, MN, USA) from the China University of Mining and Technology, and the test was employed using the displacement control mode with a loading rate of 0.003 mm/s.

2.3.2. Meso-Parameters Calibration

There is no clear criterion for the calibration of meso-parameters in numerical simulation. Generally, when using the same set of meso-mechanical parameters, if the simulation stress-strain curves under different confining pressures are in good coincidence with the lab test curves, the model can be considered reliable [37, 38]. However, this set of meso-parameters should be determined by trial-error method.

There is a sensitiveness of loading rate in the strength and deformation characteristics of rock. So, the conventional compression test with different loading rates is required in numerical simulation tests to obtain the whole process curve of static stress-strain corresponding to lab tests. Taking the conventional uniaxial compression test as an example, the axial stress-strain curves of coal specimen under different loading rates are shown in Figure 2. When the loading rate is less than or equal to 0.02 m/s, the peak strength and peak strain of coal specimen in the conventional compression simulation test tend to be steady. So, for the model in this paper, the loading less than or equal to this rate is regarded as the static.

Through repeated debugging, under the confining pressure of 0, 5, and 10 MPa, the conventional compression stress-strain curves of the simulation test and lab test are obtained, shown in Figure 3. The detailed meso-parameters are shown in Table 1. The comparison of peak strength and strain at stress peak point in the two tests is shown in Table 2, and the error between them is less than 6%. This shows that the numerical model after meso-parameter calibration can accurately reflect the mechanical properties of coal specimen.

3. Simulation Test of Coal Specimen Subjected to Cyclic Loading

In the lab test, when the friction-type AE signals are very strong, the AE monitoring system will record it. It is no doubt that these strong friction-type AE signals will decrease AE system reliability in monitoring material damage and failure. In the numerical simulation test, the bond breakage is continuously monitored by the FISH program of PFC, and the counting number of bond breakage according to the same time interval can be approximately equivalent to the measurement of AE activities [37]. This not only visualizes the study of AE characteristics through numerical simulation method but also eliminates the influence of friction-type acoustic emission. Since the purpose of numerical simulation is to study the basic mechanical properties of coal specimen subjected to cyclic loading, the peak stress of cyclic loading can be set at a higher level. This can accelerate the failure process of coal specimen and improve the computing efficiency. In this paper, cyclic loading is loaded according to the triangular waveform.

3.1. Influence of the Confining Pressure on Coal Specimen Subjected to Cyclic Loading

3.1.1. Stress-Strain Characteristics

In order to study the influence of confining pressure on the mechanical properties of coal specimen subjected to cyclic loading, the peak and valley stress of cyclic loading are fixed in the simulation test. The detailed test conditions and results are shown in Table 3, and the stress-strain curves and failure modes of coal specimen are shown in Figure 4.

(a)

(b)

(c)

Under the uniaxial stress state, the coal specimen was destroyed at the 4th cycle, and 656,539 time-steps were spent. Under the confining pressure of 5 MPa, the coal specimen was destroyed at the 20th cycle, and 4,219,657 time-steps were spent. Under the confining pressure of 10 MPa, the coal specimen was destroyed at the 38th cycle, and 11,715,047 time-steps were spent. The above part shows that when the peak and valley stress levels of cyclic loading are fixed, the higher the confining pressure, the more the cycle number and the testing time-step number. So, the confining pressure has a significant influence on the failure process of coal specimen subjected to cyclic loading; and with the increase in confining pressure, the cycle number and time-step number significantly increases.

3.1.2. Failure Mode

From Figure 4, the failure mode of cyclically loaded coal specimen under uniaxial stress state is significantly different from that under the confining pressures of 5 and 10 MPa. However, under the latter two confining pressures, there is little difference in the failure mode. Under uniaxial stress state, the main fractured plane of coal specimen is singly inclined, caused by the shear stress; besides, there are several tensile failures parallel to the axial direction of coal specimen near the main fractured plane. In other words, under uniaxial cyclic loading, the shear failure plays a dominant role in the final failure of coal specimen, and the tensile failure is only auxiliary. But, under the confining pressure of 5 and 10 MPa, the coal specimens are both in the form of dispersion failure, and there is no main fractured plane. So, the confining pressure is an important factor influencing the failure mode of coal specimen subjected to cyclic loading.

3.1.3. AE Characteristics

Figure 5 shows the AE counts and axial stress versus time-step curves of coal specimen subjected to cyclic loading under the confining pressure of 0, 5, and 10 MPa, respectively. And count the AE activities every 10,000 time-steps. From Figure 5(a), the AE activities are very obvious in each loading-unloading cycle. Besides, there are few AE activities in the unloading phases of cycles 1 and 2, but a large number of AE activities occur in the unloading phase of the 3rd cycle, and then the coal specimen was destroyed in the 4th cycle. The above shows that when a large number of AE activities occur during the unloading stage in some cycle, it indicates that the coal specimen is about to be destroyed. From Figures 5(b) and 5(c), when the coal specimen is destroyed after many cycles, the AE activity is very little at each cycle before failure and presents a three-phase evolution law, namely, initial, relatively quiet, and active phases. In the initial phase, the AE activities decrease with the increase in cycle number. In the relatively quiet phase, the AE activities remain at a low level with the increase in cycle number. In the active phase, the AE activities become more and more intense with the cycle number and reach the maximum when the coal specimen is destroyed. Moreover, Figure 5 also shows that a large number of AE activities mainly occur at the high-stress stage of cyclic loading, and there are almost no AE activities at the low-stress stage (except when the coal specimen is about to be destroyed).

(a)

(b)

(c)

Figure 6shows the cumulative AE count curves per cycle before specimen failure under the confining pressure of 0, 5, and 10 MPa, respectively. In the 1st cycle, the cumulative AE counts are 255, 833, and 1456, respectively. The above shows that under the same stress level, the higher the confining pressure, the greater the cumulative AE counts at the 1st cycle. That is, the higher the confining pressure, the more the fractures occurred in the coal specimen at the 1st cycle. However, at a cycle before coal specimen failure, the cumulative AE counts are 870, 255, and 112, respectively. This shows that the lower the confining pressure, the greater the precursory cyclic cumulative AE counts of coal specimen failure. On the whole, with the increase in the confining pressure, the cumulative AE counts at the 1st cycle tend to increase and the cumulative AE counts at a cycle before failure tend to decrease. In addition, with the increase in confining pressure, the final cycle number is obviously different. So, the confining pressure has a significant influence on the cyclic cumulative AE counts and the final cycle number of coal specimen subjected to cyclic loading.

In order to study the evolution law of AE counts with the cycle number, the ratio of the maximum AE counts in some cycle to the loudest AE counts in the 1st cycle is defined as the AE ratio, K. The equation is as follows:where A₁ is the maximum AE counts in the 1st cycle, and A_i is the peak AE counts in the i-th cycle.

Figure 7 shows the AE ratio versus the cycle number curves under the confining pressures of 0, 5, and 10 MPa, respectively. At the same stress level, the AE ratio tends to decrease with the increase in confining pressure.

3.2. Influence of the Loading-Unloading Rate of Cyclic Loading on Coal Specimen

3.2.1. Stress-Strain Characteristics

Taking uniaxial condition as an example, the influence of cyclic loading-unloading rate on coal specimen failure is studied, and the loading-unloading rates are 0.02, 0.03, and 0.04 m/s, respectively. The peak stress of cyclic loading is set to 18.18 MPa (92.5% of the conventional compression strength of coal specimen), and the valley stress is set to 10 MPa. Table 4 lists the test conditions and results. Figure 8 shows the stress-strain curves and failure modes of coal specimen subjected to cyclic loading with the three loading-unloading rates.

(a)

(b)

(c)

From Table 4 and Figure 8, under the loading-unloading rate of 0.02 m/s, the coal specimen was destroyed at the 12th cycle, and the 2,624,379 time-steps were spent; under the loading-unloading rate of 0.03 m/s, the coal specimen was also destroyed at the 12th cycle, and the 1,837,979 time-steps were spent; under the loading-unloading rate of 0.04 m/s, the coal specimen was destroyed at the 13th cycle, and the 1,534,179 time-steps were spent. This shows that the loading-unloading rate of cyclic loading has some influence on the failure process of coal specimen. Although the coal specimen was destroyed at the 12th cycle under both the loading-unloading rates of 0.02 and 0.03 m/s, the peak stress of coal specimen in the failure cycle is higher under the latter loading-unloading rate. The above shows that when other conditions are the same, the faster the loading-unloading rate, the fewer the failure time-steps; however, with the increase in the loading-unloading rate, the cycle number tends to increase slowly.

3.2.2. Failure Mode

From Figure 8, under the uniaxial cyclic loading-unloading rates of 0.02, 0.03, and 0.04 m/s, respectively, the failure mode of coal specimen has little difference. The main fractured plane of coal specimen is singly inclined, caused by the shear stress; besides, there are several tensile failures parallel to the axial direction of coal specimen near the main fractured plane. That is, the shear failure plays a dominant role in the final failure of coal specimen, and the tensile failure is only auxiliary. So, under uniaxial stress state, the cyclic loading-unloading rate has little influence on the failure mode of coal specimen.

3.2.3. AE Characteristics

Figure 9 shows the AE counts and axial stress versus time-step curves of coal specimen subjected to cyclic loading in the loading-unloading rate of 0.02, 0.03, and 0.04 m/s, respectively. The AE counts present a three-phase evolution law, namely, initial, relatively quiet, and active phases. The AE activities are most frequent in the failure cycle. However, there are almost no AE activities at the unloading or low-stress stage before coal specimen failure. In addition, in several cycles before the failure of coal specimen, the AE activities increase gradually with the cycle number, which can be used as a precursor of coal specimen failure.

(a)

(b)

(c)

Figure 10 shows the cumulative AE count curves per cycle before specimen failure under the loading-unloading rates of 0.02, 0.03, and 0.04 m/s, respectively. At the same stress level, the loading-unloading rate has some influence on the cyclic cumulative AE counts, but not obvious. Especially, at the first four cycles, the cumulative AE counts per cycle have little difference under the three loading-unloading rates. Then, with the increase in the cycle number, the cumulative AE counts per cycle are gradually different. Besides, with the increase in the difference of loading-unloading rate, the cumulative AE counts per cycle and the final cycle number are also gradually different. The above shows that the cyclic loading-unloading rates with a little difference have little influence on the cyclic cumulative AE counts and the final cycle number.

Figure 11 shows the AE ratio versus the cycle number curves under the loading-unloading rates of 0.02, 0.03, and 0.04 m/s, respectively, and these curves clearly reflect the three-phase evolution characteristics of AE activities. Each micro-fracture in the coal specimen is defined as an AE event and corresponds to a certain irreversible strain as well, so the evolution of AE ratio can also better reflect the different phases of coal specimen failure subjected to cyclic loading. When the AE ratio decreases with the cycle number, it indicates that the coal specimen is in the initial phase of the failure. When the AE ratio keeps stable with the cycle number, the coal specimen is in the constant phase of the failure. When the AE ratio increases with the cycle number, the coal specimen is in the acceleration phase of the failure.

3.3. Influence of the Valley Stress of Cyclic Loading on Coal Specimen

3.3.1. Stress-Strain Characteristics

Under the loading-unloading rate of 0.03 m/s, the influence of cyclic loading valley stress on coal specimen failure is studied. The valley stresses of cyclic loading are 6, 8, and 10 MPa, respectively, and the peak stress is set to 18.18 MPa (92.5% of the conventional compression strength of coal specimen). Table 5 lists the test conditions and results. Figure 12 shows the stress-strain curves and failure modes of coal specimen subjected to cyclic loading with the three valley stresses.

(a)

(b)

(c)

From Table 5 and Figure 12, when the valley stress of cyclic loading is 6 MPa, the coal specimen was destroyed at the 7th cycle, and the 1,573,079 time-steps were spent; when the valley stress of cyclic loading is 8 MPa, the coal specimen was destroyed at the 10th cycle, and the 1,897,379 time-steps were spent; when the valley stress of cyclic loading is 10 MPa, the coal specimen was destroyed at the 12th cycle, and the 1,837,979 time-steps were spent. The above shows that when the peak stress of uniaxial cyclic loading are fixed, with the decrease in the valley stress, the cycle number of coal specimen failure gradually reduces; that is, the damage increases in each cycle.

3.3.2. Failure Mode

From Figure 12, under the uniaxial cyclic loading with the valley stresses of 6, 8, and 10 MPa, respectively, the failure mode of coal specimen has little difference. The main fractured plane of coal specimen is singly inclined, caused by the shear stress; besides, there are several tensile failures parallel to the axial direction of coal specimen near the main fractured plane. That is, the shear failure plays a dominant role in the final failure of coal specimen, and the tensile failure is only auxiliary. So, under uniaxial stress state, the valley stress of cyclic loading has little influence on the failure mode of coal specimen.

3.3.3. AE Characteristics

Figure 13 shows the AE counts and axial stress versus time-step curves of coal specimen subjected to cyclic loading with the three valley stresses. The AE counts present a three-phase evolution law, namely, initial, relatively quiet, and active phases. The AE activities are most frequent in the failure cycle. In addition, there are almost no AE activities at the unloading or low-stress stage of cyclic loading before coal specimen failure.

(a)

(b)

(c)

Figure 14 shows the cumulative AE count curves per cycle before specimen failure under the valley stresses of 6, 8, and 10 MPa, respectively. At the same loading-unloading rate, in the 1st cycle, the cyclic cumulative AE counts have a little difference under the three valley stresses. With increase in the number of cycles, the difference of cumulative AE counts per cycle increases. Besides, with the increase in the difference of valley stresses, the final cycle number is also obviously different. Especially, in the relatively quiet phase, the lower the valley stress, the greater the cumulative AE counts per cycle. That is, the lower the valley stress, the more the fractures occurred in the coal specimen in the relatively quiet phase. The above shows that the valley stress of cyclic loading has little influence on the cumulative AE counts in the 1st cycle but has a relatively significant influence on the cumulative AE counts in the subsequent cycles and the final cycle number.

Figure 15 shows the AE ratio versus the cycle number curves in the three valley stresses. The curve clearly reflects the three-phase evolution characteristics of AE activities and different stages of coal specimen failure subjected to cyclic loading.

4. Damage Evolution of Coal Specimen Subjected to Cyclic Loading

Damage refers to the progressive weakening of internal cohesion caused by the development of material micro-defects subjected to monotonic or repeated loading and finally leads to the failure of volume units [39]. Damage can change many properties of materials, such as the decrease of elastic modulus, ultrasonic velocity, and density. For damage, we must give a quantitative calculation method. Reasonable damage variables should have a clear physical meaning and easy to be measured and used in engineering. In this paper, the cumulative AE counting method is used to calculate the damage of coal specimen subjected to cyclic loading.

Xiao et al. [40] proposed a very concise equation for damage calculation. The equation is as follows:where N is the cumulative AE counts at the end of some cycle and N_m is the cumulative AE counts at the specimen failure.

Because equation (3) cannot express the damage at some time-step in a cycle, the calculating damage is discontinuous by this method. In order to obtain the continuous damage value, here, the parameter “N” is defined as the cumulative AE counts at some time-step.

Taking coal specimens subjected to cyclic loading with the confining pressures of 0, 5, and 10 MPa as an example. Figure 16 shows the continuous damage evolution process of coal specimen subjected to cyclic loading. Figure 17 shows the damage curves of coal specimen subjected to cyclic loading at each cycle. Table 6 shows the number of fractured and unbroken contacts and their ratio at the peak stress point of specimen failure cycle under the three confining pressures.

(a)

(b)

(c)

From Figures 16 and 17, under the confining pressures of 0, 5, and 10 MPa, the damages at the 1st cycle are 0.1634, 0.4623, and 0.5659, respectively. This shows that the damage at the 1st cycle increases with the increase in confining pressure. On further analysis, the following conclusions can be obtained. Under the uniaxial stress state, coal specimen is destroyed only at the 4th cycle, and the damage almost linearly increases; under the confining pressures of 5 and 10 MPa, coal specimen is respectively destroyed at the 20th and 38th cycle, the damage presents the three-phase evolution law, namely, initial, steady, and accelerating phases. So, the confining pressure has a great influence on the damage evolution process of coal specimen subjected to cyclic loading. More importantly, the damage of coal specimen subjected to cyclic loading increases rapidly before forthcoming failure, so it is of great significance to use the AE monitoring technology to explore the precursory characteristics of coal specimen failure.

From Table 6, under the confining pressures of 0, 5, and 10 MPa, the ratio of fractured contacts to unbroken contacts are 9.86, 10.51, and 14.13 percent, respectively. A general trend is that this rate rises with the increase in the confining pressure. That is, the higher the confining pressure, the more broken the failed coal specimen subjected to cyclic loading. The above shows that the confining pressure has a large influence on the broken degree of coal specimen subjected to cyclic loading.

5. Discussion

At present, the AE characteristics of rock under cyclic loading have been widely studied, and many rich research results have also been obtained [5, 7, 15, 26, 30–33]. However, most of these achievements are based on the lab test and do not consider the discreteness of specimen and not fully study the failure mode of specimen. So, this paper studies the AE characteristics and failure mode of coal specimen under different confining pressures, loading-unloading rates, and valley stresses by numerical simulation.

In this paper, the numerical simulation results show that with the increase in confining pressure, the cycle number of coal specimen failure increases significantly; with the increase in the loading-unloading rate, the cycle number of coal specimen failure tends to increase slowly; the lower the valley stress, the less the cycle number of coal specimen failure. These results are consistent with that of the lab tests. Therefore, for some problems of rock mechanics subjected to cyclic loading difficult to be studied by the lab test, the numerical simulation method is a way to solve them. In addition, the numerical simulation results also show that the AE activities of coal specimen subjected to cyclic loading present a three-phase evolution law, namely, initial, relatively quiet, and active phases. The AE ratio proposed in this paper can well reflect these three phases. Because there are little or no AE activities in the relatively quiet phase, the Kaiser effect can be considered to play a leading role. Because AE activities become more and more intense in the active phase, the Felicity effect can be considered to play a dominant role. So, the failure of cyclically loaded coal specimen is the combined result of the two AE effects. Meanwhile, the appearance of Felicity effect can be used as a precursory index of specimen failure. For the failure mode and degree of coal specimen, the effect of confining pressure is very significant. Under uniaxial stress state, there is an inclined main fractured plane in coal specimen; however, under the confining pressures of 5 and 10 MPa, the coal specimen represents dispersion failure. Besides, under these three confining pressures, the ratios of fractured contacts to unbroken contacts are 9.86, 10.51, and 14.13 percent, respectively. It can be concluded that with the increase in confining pressure, the coal sample tends to be more broken.

In fact, the in situ rock masses generally consist of many types of rock; therefore, to study the AE characteristics of rock combination body subjected to cyclic loading is more helpful to solve the in situ rock engineering problems. In addition, in most cases, the in situ rock masses are subjected to noncyclic loading, sometimes dynamic loading; therefore, the rock engineering problems subjected to the two loadings also need to be further studied in the future. More importantly, to study the AE characteristics of rock subjected to cyclic loading is aimed at providing the reliable precursory indicator for predicting its damage and failure. So, it is more meaningful to study the nonlinear prediction method of rock failure based on the three-phase evolution law of AE activities under cyclic loading through the nonlinear theory. For example, the AE waveform signals obtained in the lab test are analyzed through the methods of wavelet and spectrum analysis and then to study the evolution law of discrete wavelet coefficient and main frequency in the loading process. If the mutation characteristics of the discrete wavelet coefficient and the main frequency at specimen failure can be determined, then the two indexes can be used as the precursory information to predict the specimen failure.

6. Conclusions

In this paper, the influence of confining pressure, loading-unloading rate, and valley stress on the AE characteristics and failure process of coal specimen subjected to cyclic loading is studied by using the PFC simulation software. The main conclusions are as follows:(1)The cycle number of failed coal specimen subjected to cyclic loading is significantly influenced by the confining pressure, followed by the valley stress, and finally the loading-unloading rate. With the increase in confining pressure, the cycle number significantly increases; with the decrease in valley stress, the cycle number gradually reduces; and with the increase in loading-unloading rate, the cycle number tends to increase slowly.(2)The failure mode of coal specimen subjected to cyclic loading is significantly influenced by the confining pressure. Under uniaxial stress state, the main fractured plane of coal specimen is singly inclined, caused by the shear stress; besides, there are several tensile failures parallel to the axial direction of coal specimen near the main fractured plane. Under the confining pressures of 5 and 10 MPa, the coal specimens are both in the form of dispersion failure and there is no main fractured plane. However, the loading-unloading rate and valley stress of cyclic loading has little influence on it.(3)The AE counts of coal specimen subjected to cyclic loading is greatly influenced by the confining pressure and the valley stress. With the increase in the confining pressure, the cumulative AE counts at the 1st cycle tend to increase but decrease at a cycle before failure; with the decrease in the valley stress, the cumulative AE counts per cycle increase in the relatively quiet phase. However, the loading-unloading rate has a little influence on it.(4)A large number of AE activities mainly occur at the high-stress stage of cyclic loading, and there are almost no AE activities at the low-stress stage before forthcoming failure of coal specimen. If a large number of AE activities occur during the unloading stage in some cycle, it indicates that the coal specimen is about to be destroyed.(5)When the coal specimen is destroyed after many cycles, the AE activities present a three-phase evolution law, namely, initial, relatively quiet, and active phases. The AE ratio is proposed, and it is defined as the ratio of the maximum AE counts in some cycle to the loudest AE counts in the 1st cycle. The evolution of AE ratio can better reflect the different stages of coal specimen failure under cyclic loading.(6)Under different confining pressures, the continuous damage evolution curves of coal specimen subjected to cyclic loading are obtained. Meanwhile, the influence of confining pressure on the broken degree of coal specimen subjected to cyclic loading is analyzed through the ratio of fractured contacts to unbroken contacts and shows that the higher the confining pressure, the more broken the failed coal specimen subjected to cyclic loading.

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 they have no conflicts of interest.

Acknowledgments

This research was supported by the National Natural Science Foundation of China (Grant no. 51574156) and the Natural Science Innovation Foundation of Inner Mongolia University of Science and Technology (Grant no. 2019QDL-B25).

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Copyright © 2020 Huiqiang Duan and Depeng Ma. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.

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