Abstract

The physical simulation system is an important means to study the mechanism of coal and gas outburst. The small- and medium-sized coal and gas outbursts account for the largest proportion in China. So, the paper focuses on small- and medium-sized coal and gas outbursts based on key physical rules and their statistical characteristics. According to the geometric parameters statistical data of more than 100 caverns, the proportion of outburst caverns whose depth is less than 5 m is 80%, and whose depth is more than 6 m is 13%. The ratio of depth and cavern outlet’s diameter is 2.58–7.31. There are statistical relationship of 2 times between coal’s and cavern’s volume, and between gas emission volume per ton and gas content in seam. Then, the cavern of coal and gas outburst is simplified as an ellipsoid, and the shape of cavern outlet is simplified as a circle. The cavern’s and the prototype’s geometrical parameters of small and medium coal and gas outbursts were deduced. The depth of cavern is 5 m, width is 4 m, and diameter of cavern outlet is 0.68–1.94 m. The depth of coal and outburst prototype is 12.3 m, width is 6.5 m, and diameter of cavern outlet is 0.68 m. In order to guarantee the movement similarity, according to the relationships among statistical data of outburst coal particle’s size, cavern outlet’s size, and height of tunnel, the minimum cavern outlet’s size was calculated. Select 10 times the coal particle’s size (5 mm) as the smallest size. Then, maximum geometric similarity ratio of coal and gas outburst was deduced, and it is 13.6. The minimum geometrical parameters of coal and outburst similar model were obtained. Its depth is 0.9 m, width is 0.48 m, and diameter of cavern outlet is 50 mm. According to the results, the physical simulation system was developed. The results provide support to carry out physical simulation experiment of coal and gas outburst.

1. Introduction

Since the first recorded coal and gas outburst that occurred in Loire mining areas of France in March 22, 1834, more than 20 countries and regions have experienced coal and gas outburst [1, 2]. China’s first coal and gas outburst occurred in west pit coal roadway face of Fuguo Coal Mining Liaoyuan Coal Mining Bureau in April 20, 1950. Today, according to the statistics, the number of coal and gas outbursts in China accounts for 1/3 of the global total [3]. China has become one of the most affected countries by coal and gas outburst.

At present, comprehensive hypothesis of coal and gas outburst mechanism has been accepted by global scholars. Then, it is considered that the coal and gas outburst is caused by the combined action of gas pressure, in situ stress, and physical and mechanical properties of coal. Based on the “comprehensive hypothesis theory,” the global scholars carried out a great deal of studies and build many theories. The physical simulation experiments are an important means to study the mechanism and prevention technology of coal and gas outburst, in which the similar material and physical simulation system are the key factors. Many researchers studied the mechanical characteristics of rock, coal, and similar materials [46]. Meanwhile, various physical simulation systems are developed to carry out physical experiments. Xодот et al. had done the one-dimension outburst simulation test firstly. The geometric dimension of the molding model is 0.2 m × 0.6 m × 1.4 m. The hydraulic press can provide a vertical loading pressure of 10 MPa, and the sealing pressure can reach 1–2.5 MPa. The experiments were carried out with briquette and CO2, and the results have shown that coal and gas outburst will occur only under high gas pressure gradient [7]. Kravchenko used coal samples of 0.2 m × 0.04 m 0.04 m and CO2 to carry out experiments with gas pressure of 2–5 MPa. The failure wave velocity of coal samples was measured by an oscilloscope [8]. Yartsev carried out the experiments with coal samples with a diameter of 56 mm and a height of 100 mm and pressure of 0.5–4.0 MPa [9]. Kuroiwa and Tashiro used a cylindrical device with a volume of 120 cm3 to simulate the coal and gas outburst tests with briquette coal samples and CH4 [10]. Alekseev et al. developed a triaxial stress test equipment. The maximum pressure of the device is 600 MPa, the adsorption equilibrium pressure is 15 MPa, and the coal sample size is 60 mm × 60 mm × 60 mm [11]. Bodziony et al. carried out experiments with a cylindrical device. Its diameter is 97.4 mm and length is 281 mm. Deng Quanfeng, Luan Yongcai, and Wang Youan developed a one-dimensional outburst simulation test system. The vertical and lateral pressures are provided by 100t and 500t material testing machines. The coal sample container of the system is a cylinder with an inner diameter of 200 mm, and the mouth is a circle with a diameter of 20 mm. Through 12 outburst tests using the system, it was concluded that the minimum gas pressure of outburst increases linearly with the increasing of coal strength [12]. Zhou and He developed a three-dimensional loading rheological test system, in which the coal sample container is a cylinder with an inner diameter of 50 mm and a length of 100 mm, and the loading is provided by a creep press [13]. Nelieki and Topolnicki developed a test device with a diameter of 96.4 mm and a length of 300 mm. The outburst test of briquette samples made from 0.2 mm pulverized coal and adsorbed gas of N2 or CO2 was simulated [14]. Jiang Chenglin and Yu Qixiang developed a one-dimensional outburst simulation test system. The vertical pressure of the system is provided by a 500t testing machine. The coal sample container is a cylinder with an inner diameter of 442 mm, and its outlet is an adjustable round shape with a maximum diameter of 200 mm. The coal and gas outburst tests were carried out with the system, and the hypothesis of spherical shell instability was obtained [15]. Cai carried out three-dimensional simulation test of coal and gas outburst. The size of outburst simulation module (length × width × height) is 225 mm × 225 mm × 187.5 mm, and the factors influencing outburst strength are obtained [16]. Norbert Skoczylas developed a two-dimensional loading outburst simulation test equipment. The coal sample chamber is cylindrical, with an inner diameter of 48 mm, a length of 110 mm, and a protrusion size of 0.78 mm2–21.84 mm2. The experiments were carried out with uniaxial compressive strength of 1.8–17.2 MPa and gas pressure of 1.4–31.7 MPa. The relationships between uniaxial compressive strength, gas pressure, and outburst were obtained [3]. In addition, the research teams of Anhui University of Science & Technology and Chongqing University developed three-dimensional coal and gas outburst model test systems and carried out plenty of experiments with different conditions. These researches’ results improved the prevention and treatment level of the disaster. The former physical simulation systems have the variety of dimensions of similar models. Because of less study on the similar model, this results in the decline of similar degree.

Aimed at the shortages of physical simulation systems, the paper puts forward a geometric model for physical simulation system through studying the similar model’s dimension of small and medium coal and gas outbursts according to their characteristics of outburst cavern, gas emission, and coal particle size based on dominant physical law in coal and gas outburst. The study focuses on prototype geometric parameter of coal and gas outburst and development of physical similar simulation system, including depth and width, and diameter of cavern outlet. The results can provide a high similar degree system to study the mechanical processes for coal and gas outburst.

2. Mechanical Mechanism of Coal and Gas Outburst

2.1. Evolution Process of Coal and Gas Outburst

Mechanical mechanism theory of coal and gas outburst is derived from the “comprehensive hypothesis theory.” The views of the theory are that there exist four stages of preparation, initiation, development, and termination in the process of coal and gas outburst. And under certain conditions, there also exist several pauses and re-initiation process in the stage of development [1719]. The evolution processes of coal and gas outburst are shown in Figure 1, in which the thick solid line expresses the inevitable phenomenon and the thick dashed line expresses the possible phenomena.

In the stage of preparation, balance of original in situ stress in working face is destroyed by mining activity. It causes rebalancing of the situ stress. During the process, coal and rock mass around the working face are destroyed. So, there forms in situ stress concentration area and bearing pressure limited equilibrium area appears in front of the working face’s coal wall. The quasi-static deformation and damage of coal and rock provide mechanical failure conditions for initiation of coal and gas outburst.

In the stage of initiation, accumulation of deformation and fracture of coal or rock mass is achieved to certain critical conditions or there exists outside disturbing load suddenly; coal and rock are destroyed and lose their bearing capacity. During the process of destruction, elastic potential energy and gas internal energy stored in coal and rock are released rapidly and lead to the destroyed coal and rock being thrown out. Then, there forms the initial outburst cavern.

In the stage of development, the coal and rock mass with high in situ stress and gas pressure around the outburst cavern is suddenly exposed after initiating of coal and gas outburst. Stress loaded in coal wall of outburst cavern is suddenly removed and then gas rapidly desorbs and flows into the cavern. It forms benefit condition for coal mass’s failure. Under the composited action of in situ stress and gas pressure, coal seam is broken and thrown out rapidly. Meanwhile, the outburst cavern is gradually expanded.

In the stage of pause and re-initiation, after the development stage there is no condition to meet the coal destruction, so coal destruction pauses. The reason why coal destruction is paused is that there forms support action in cavern wall caused by accumulation of coal and gas, and unloading effect is weakened, caused by slow damage of cavern wall. Then, the coal and rock mass around the outburst cavern will continue quasi-static deformation and emit gas into cavern. When the gas pressure in the cavern increases to a certain value, the fractured coal and rock will be thrown out again, and the coal and rock of cavern wall will be destroyed continuously. It results in a new occurrence of coal and gas outburst.

In the stage of termination, if there is not enough gas pressure to throw out the fractured coal and rock again after the stage of development, the re-initiation of coal and gas outburst cannot appear also. The outburst cavern becomes stable and the coal and gas outburst is terminated.

2.2. Dominant Physics Laws in Coal and Gas Outburst

The views of mechanical mechanism theory of coal and gas outburst are that coal and gas outburst are of continuous or alternating appearances of three dominant phenomena as follows [17]:(1)Static deformation and destruction of coal seam in the stage of preparation.The in situ stress balance of original formation is destroyed in the process of mining in workface. There forms support pressure area in front of workface, and part of coal seam is destroyed. It is the stage of preparation of coal and gas outburst. The deformation and destruction processes are quasi-static.(2)Fracture of gassy coal seam in the stages of initiation and development.The main phenomenon is the rapid broken gassy coal seam in the stage of development. It is caused by the sudden changing of in situ stress and sudden exposing of gassy coal seam to high pressure. The essence of the broken seam is that the tensile stress concentration results in fissure expansion. And the tensile stress concentration caused in situ stress and gas pressure in caverns and cracks tip of coal seam.(3)Movement of broken coal and gas flow in mining space.During the outburst, there forms separation phenomenon where coal particle sizes distribute large to small with the near to far distance from outburst cavern because of outburst broken coal and gas flow’s movement and deposition in mining space. Also, there appear damaging shock waves in the initial of the outburst.

3. Statistical Characteristics of Coal and Gas Outburst

3.1. Shape and Geometric Parameters of Coal and Gas Outburst Cavern

After the coal and gas outburst, there is a cavern in coal and rock mass along with coal, and rock and gas are thrown into mining space. According to statistical research, cavern of coal and gas outburst general has a small opening and a big cavity. Shapes of caverns are pear-shaped, tongue-shaped, bottle inversion-shaped, bifurcation-shaped, and so on [18, 20, 21]. Caverns of coal and gas outburst have different geometric parameters. The caverns’ characteristics geometric parameters of more than 100 coal and gas outbursts that occurred during tunnel excavating in Chongqing district are shown in Table 1.

Depth of outburst cavern along the strike is the important parameter. In Table 1, it is shown that the proportion of outburst caverns whose depth is less than 5 m is 80%, and whose depth is more than 6 m is 13%, in Chongqing area.

Typical coal and gas outburst has the characteristics of small opening and big cavity. The statistical geometric parameters of small and medium coal and gas outburst’ cavern are shown in Table 2.

3.2. Gas Emission Quantity

Plenty of gas is emitted in the process of coal and gas outburst. The gas concentration will exceed normal state in coal mine for several days because the stacked coal continually desorbs large amounts of gas. The gas emission quantity depends on outburst scale and gas content of coal seam. According to standard, coal and gas outburst has the characteristic where unit gas emission quantity of outburst coal is greater than or equal to 30 m³/t, or more than twice the content of local coal seam.

3.3. Volume Relationship between Outburst Coal Quantity and Cavern

The volume of outburst cavern is always smaller than that of outburst coal and rock. According to the statistics, volume of outburst cavern is half of outburst coal volume normally. But the volume ratio is 1/10 in some special coal and gas outbursts [18, 22].

3.4. Size of Outburst Coal Particle

The outburst coal particle has the form of block or is granular with some size. Statistical size data of outburst coal out of the outburst cavern is shown in Table 3.

4. Geometric Parameter of Coal and Gas Outburst Similar Model

Generally, most of the coal and gas outbursts are small and medium. So, the data about similar model in this paper is derived from the statistics of small and medium coal and gas outbursts.

4.1. Geometric Parameter of Coal and Gas Outburst Cavern

Outlet of coal and gas outburst cavern is simplified to a circle in this paper. The outburst cavern is described by height, width, and depth. According to the data in Table 1, it is analyzed that depth of the coal and gas outburst that happened in China is less than 5 m, and the width is less than 4 m [17].

Height of outburst cavern has relation to thickness and dip angle of coal seam. The height of similar model is decided by the coal seam. In China, coal mining is mostly in medium thickness coal seam. So, the thickness is less than 3.5 m normally.

According to the statistical data of outburst cavern’s outlet in Table 2, size of outburst cavern’s outlet varies with the outburst scales. Among the lager coal and gas outbursts, outlet size of outburst cavern that occurred in coal roadway heading face is limited by the height of coal seam thickness, but there is no limit to the width of coal seam. So, there forms the outburst cavern of its width larger than height. As seen in Table 2, the ratio of depth and cavern outlet’s diameter is 2.58∼7.31. When the depth of coal and gas outburst is 5 m, cavern outlet’s diameter is 0.68–1.94 m. It is fit to the thickness (1.3∼3.5 m) of the main mining coal seam in China.

Analyzing the above, the geometric parameters of typical small and medium coal and gas outburst are shown in Table 4 and Figure 2.

Height of coal and gas outburst is depended on thickness of coal seam. So, the height of outburst cavern is not considered in Table 4.

4.2. Prototype Geometric Parameter of Coal and Gas Outburst

Geometric parameter of outburst cavern is different from coal and gas outburst prototype’s because outburst cavern is produced by coal and gas outburst. In the process of coal and gas outburst, there is coal and rock mass of big area participating in the outburst and not only that of the outburst cavern area. So the coal and outburst prototype contains coal and rock mass of cavern area and the surrounding influenced area.(1)Prototype geometric parameters deduced by the volume relation between outburst cavern and outburst broken coal.Volume of outburst cavern is always smaller than that of outburst broken coal. According to statistic data of more than 30 outburst caverns that occurred in Zhong Liangshan Coal Ming, Yu Tianbao Coal Ming, and Donglin Coal Ming located in Chongqing district, the volume ratio of outburst cavern and outburst broken coal is 1/2 [18, 22]. The outburst cavern is equivalent to an elliptic cylinder whose major axis is 5 m and minor axis is 4 m. The prototype of coal and gas outburst is considered as an elliptic cylinder too. When the coal gas outburst occurs in small and medium thick coal seam, the height h is assumed to be the thickness of the coal seam. Analyzing the statistics in Table 2, ratio of cavern’s depth and width becomes larger with the increase of cavern’s depth. The ratio is 1.44–2.13, and the average ratio is 1.89. In this paper, the volume ratio of outburst cavern and outburst broken coal is 1/2, so the ratio of prototype’s major and minor axis is 1.89 : 1. It is calculated that the participating coal and rock mass is in the area of length 8.7 m, width 4.6 m, and height h.(2)Prototype geometric parameters deduced by the relation between gas emission quantity of unit mass coal and gas content of coal seam.

According to statistics, gas emission quantity of unit mass coal is more than twice gas content of coal seam in most coal and gas outbursts because of the gassy coal seam surrounding outburst cavern desorbs and is emitted to the roadway [17]. According to standard, coal and gas outburst has the characteristic where unit gas emission quantity of outburst coal is greater than or equal to 30 m3/t, or more than twice the content of local coal seam. In order to keep similar gas emission, the gas quantity derived from the influenced coal seam should be taken into account. In order to simplify calculation, the ratio of gas emission quantity of unit mass and gas content of coal seam is determined to be 2 times in this paper. It is assumed that gassy coal of influenced area desorbs all gas in the occurrence process or later in coal and gas outburst. So, the influenced area of coal seam is twice the outburst cavern area. Based on the above condition, the ratio of prototype’s major axis and minor axis is 1.89 : 1. So the participating coal and rock mass is in the area of length 12.3 m and width 6.5 m.

So, the minor prototype geometric parameters of typical small and medium coal and gas outburst are shown in Table 5.

4.3. Geometric Parameters of Coal and Gas Outburst Physical Similar System

For the convenience of test, the size of physical similar system is usually smaller than that of the prototype. But, size of outburst cavern outlet should fit the size of outburst coal particles. If the size of outburst coal particles is close to or larger than the size of outburst cavern outlet, the coal particles will block outburst cavern outlet and will result in the failure of occurrence of test. From Table 3, the mass proportion of coal particles size of 5 mm is more than 64%. The similar material which is used to carry out similar simulation test in laboratory has the characteristics of better uniformity, lower strength, and smaller coal particles than coal seam, and the proportion of coal particles of size 5 mm would be larger than 64%. So, the size of 10 times 5 mm is chosen as the minor size of outburst cavern outlet. Then, the minor size of outburst cavern outlet is 50 mm. It is calculated that the maximum geometric similarity ratio of the physical similar simulation model is 13.6.

In order to keep the similar movement of coal particles in roadway, the size of similar simulation roadway should be greater than the size of outburst coal particles. So, the size of 10 times 5 mm is chosen as the size of similar simulation roadway. According to the rule of height of road way in “Mine Safety Regulations” of China, the height of roadway is chosen as 2.0 m. It is calculated that the maximum geometric similarity ratio of the physical similar simulation model is 20.

So, the maximum geometric similarity ratio of the physical similar simulation model is 13.6. The minimum geometric parameters of similar simulation model are shown in Table 6.

5. Development of Physical Similar Simulation System

5.1. Sealed Cabin

The sealed cabin is used to make gassy coal seam model. It has the size of 1.5 × 0.8 × 0.8 m (length × width × height) which is developed according to the geometric similarity ratio 8. And the maximum size of outburst cavern outlet is 300 mm. At present, within the mining depth of 1000 m, the gas pressure of coal seam is less than 6 MPa normally. So, the pressure of working pressure is designed to be 6 MPa [23]. The opening method of outburst cavern outlet is positive-pressure blasting using rupture disc. The similar simulation system can carry out simulation test of different sizes through changing the sizes of model and outburst cavern outlet. The sealed cabin is shown in Figure 3.

At present, the structural form of roadway is trapezoid and arch usually in coal mine. And its height is about 2.5 m. For ease of manufacture, section of simulated roadway is simplified to a square. The geometric similarity ratio is chosen as 8. So, the size of the simulated roadway section is 300 mm. It is fit to the size of outburst cavern outlet.

5.2. Simulated Roadway

The simulated roadway is consisted by straight pipes (length of 1 m and 1.5 m), bending pipes (turning angles of 10°, 20°, and 90°), and three-way pipes. So, the different combination methods of pipes can simulate different forms of roadways. The pipes are shown in Figure 4.

5.3. Mechanical Loading System

Most of the coal mining depth is less than 1000 m in China. The rock mass average density is 2.5 × 103 kg/m³. So, it is calculated that the in situ stress is about 25 MPa in the depth of 1000 m. Because the bearing area is 1.2 m2 (1.5 m ∗ 0.8 m), the mechanical loading system is designed such that the vertical loading is 3 × 106 kg and the horizontally symmetrical loading is 2 × 106 kg. And the structural form of loading system is of frame type.

To prevent the impact of test system during the test, the system rigidity is designed to be more than 3 × 1010 N · m−1.

Mechanical loading system is shown in Figure 5.

5.4. Data Acquisition System

Monitoring equipment uses NI PXI data acquisition system and phantom v210 high-speed camera. Based on NI PXI data acquisition system, the data acquisition software is developed. The system can collect such parameters of coal and gas outburst as in situ stress, gas pressure, temperature, velocity of stress wave, shock wave, wind speed, oxygen concentration, carbon dioxide concentration, and image of the cavern process. Data acquisition system is shown in Figure 6.

5.5. Dust Collector

The dust collector is comprised of air inlet, dust cleaning window, multi-stage vibration bag dust collecting device, and air outlet. The dust collector is shown in Figure 7. It is used for clearing dust produced in test and keeping the environmental protection.

6. Conclusion

Based on the statistical data of small and medium coal and gas outbursts, the geometric sizes of the prototype and similar model of medium and small coal and gas outburst are theoretically deduced. Then, the physical simulation system is developed. Conclusions are obtained as follows:(1)The cavern of small and medium coal and gas outburst is equivalent to an elliptic cylinder. The cavern’s major axis is 5 m and minor axis is 4 m. Height depends on the thickness of the coal seam. Diameter of the cavern outlet is 0.68–1.94 m.(2)With the relations between outburst broken coal and rock volume, gas emission quantity of unit mass, and gas content of coal seam, the minimum geometric size of coal and gas outburst prototype is deduced. The depth is 12.3 m, width is 6.5 m, and diameter of cavern outlet is 0.68 m.(3)According to the size relations between coal particle and outburst cavern outlet, and between coal particle and roadway, the maximum geometry similarity ratio of prototype and model is 13.6. The minimum geometry depth is 0.90 m, width is 0.48 m, and diameter of cavern outlet is 0.05 m.(4)The physical simulation system is developed. Geometry size of sealed cabin is 1.5 × 0.8 × 0.8 m (length × width × height). Its gas bearing capacity is 6 MPa, and maximum diameter of outburst cavern outlet is 0.3 m. The section of simulated roadway is square and its edge length is 0.3 m. The vertical loading is 3 × 106 kg, and the horizontally symmetrical loading is 2 × 106 kg. The system rigidity is more than 3 × 1010 N · m−1.

7. Discussion

Coal and gas outburst is the result of comprehensive action of in situ stress (including tectonic stress) and gas and coal physical and mechanical properties. The occurrence mechanism is complex. The existing research methods of coal and gas outburst mechanism are mainly divided into three types. In the early stage, scholars analyzed the phenomenon of coal and gas outburst and deduced the outburst mechanism and put forward the hypothesis of gas leading role and in situ stress leading role hypothesis. With the deepening of understanding of coal and outburst, scholars have carried out research on outburst mechanism by means of energy theory, mechanical theory, and numerical simulation, which promotes the understanding of disasters and the improvement of prevention and control technology. At present, due to the need of safety production, the mechanism of outburst has been studied qualitatively and quantitatively. Because it is difficult to achieve the field test, the similar material simulation test has become an effective method to study the outburst criterion quantitatively. However, most of the similar coal seam models in the former test system are cylindrical, and the mechanical loading is mainly one-dimensional. Although some tests were carried out with three-dimensional simulation system, the size of coal sample is small. So, most of the similar experiments have low degree of similarity.

On the basis of previous studies, the geometry size of outburst simulation test system is obtained, and the test system is developed based on the analysis of coal and gas outburst data in the paper. The results improve the similarity of simulation system and promote the progress of physical similar simulation experiment. However, due to the limited amount of data, the geometric size of the similar model proposed in this paper does not fit all conditions, and the effect of tectonic stress is not considered alone. In the following research, scholars will continue to improve the present simulation test system and strive to restore the real coal and gas outburst process.

Data Availability

The data used to support the findings of this study are available from the corresponding author upon request.

Disclosure

The authors would like to declare on behalf of their coauthors that the work described was original research that has not been published previously and not under consideration for publication elsewhere, in whole or in part. All the authors listed have approved the manuscript that is enclosed. Meanwhile, the founding sponsors had no role in the design of the study; in the collection, analyses, or interpretation of data; in the writing of the manuscript; and in the decision to publish the results.

Conflicts of Interest

The authors declare no conflicts of interest, and the manuscript is approved by all authors for publication.

Acknowledgments

This research was supported by Key R&D Program of Shandong Province, China (Grant no. 2019GSF111051), Shandong Provincial Natural Science Foundation, China (Grant no. ZR2018LE009), and the PhD Start-up Fund of Shandong Jiaotong University, China.