2. Mitigating Risks in Coal Mining
The Cuncaota II Mine is located in the Yijinhuoluo Banner, Ordos City, within the Inner Mongolia Autonomous Region. The coal seams extracted from this mine are Type I, which makes them prone to spontaneous combustion. They have a significant mining height and long working faces, with relatively fewer collapses in the upper and lower triangular areas. However, there is a considerable amount of residual coal near the two roadways in the goaf, posing a significant risk of spontaneous combustion. Classified as a low-gas mine, the risk of surpassing gas pressure limits is relatively low. The main safety concern affecting mine production is the spontaneous combustion of residual coal in the goaf due to air leakage. Therefore, immediate measures are necessary to mitigate the likelihood of spontaneous combustion in the goaf and ensure the safety of mine production.
The 22,122 working face is located in the No. 1 mining area, spanning 835.5 m in length and 340.9 m in width, covering a total area of 284,821.95 m2. The coal seam varies in thickness from 2.14 m to 4.81 m, with an average thickness of 2.93 m. The roof of the working face consists mainly of sandy mudstone and siltstone, followed by mudstone and medium-grained sandstone, with localized occurrences of fine-grained sandstone and coarse-grained sandstone. The floor primarily consists of siltstone and fine-grained sandstone. The stratigraphic column of the working face is shown in Figure 1. In the auxiliary haulage roadway of the 22,122 area, the roof consists mainly of continuous medium-grained sandstone, with good rock layer integrity and reduced susceptibility to collapse during mining operations. However, there is a significant issue of air leakage at the two corners of the working face. Currently, measures such as wind curtains and cement bag walls are primarily used to mitigate air leakage. The 22 coal seam is characterized by its overall black coloration with black-brown streaks. The primary constituents of the coal rock include dark coal, bright coal, and some occurrences of cannel coal and vitrinite. The coal exhibits an asphalt luster, featuring a uniform and banded structure, blocky texture, extensive crack development, semi-hardness, and a propensity for spontaneous combustion. The coal seam has a natural ignition period of 42 days, with flame lengths exceeding 400 mm, and the coal dust within the seam possesses explosive properties.
Figure 1. Stratigraphic column of the 22,122 working face.
To fully grasp the impact of corner filling on changes in the gas concentration in the goaf, the oxygen concentration in the goaf is monitored using a 260 m long 2-inch seamless steel pipe. This pipe is positioned in the direction of the main withdrawal channel, starting from the end position of the inlet and return air lane of the 22,122 working face. By employing the oxygen concentration method, the approximate range of the oxidation zone in the goaf is determined. This method relies on measuring the oxygen concentration at various distances from the goaf to the working face. Areas with an oxygen concentration greater than 15% are classified as heat dissipation zones. Areas with an oxygen concentration between 15% and 5% are considered oxidation spontaneous combustion zones. Lastly, areas with an oxygen concentration below 5% are identified as asphyxiation zones. Sampling probes are strategically placed at 25 m intervals, starting from the corner of the working face. Each intake and return airway has three probes, labeled as “Inlet 1,” “Inlet 2,” “Inlet 2,” “Return 1,” “Return 2,” and “Return 3”. To protect the probes from damage, probe protection devices are utilized, and seamless steel pipes are connected using flange plates to ensure strong connections. Through sampling and an analysis of gas concentration data, it is observed that, on the intake side of the 22,122 working face, the oxygen concentration decreases to below 15% at a distance of 134 m from the working face, indicating entry into the oxidation zone. At a distance of 229 m, the oxygen concentration further decreases to below 5%, signifying entry into the asphyxiation zone. The oxidation zone is approximately 95 m wide. On the return side of the goaf, the oxygen concentration decreases to below 15% at a distance of 42 m from the working face, entering the oxidation zone. At a distance of 185 m, the oxygen concentration drops below 5%, indicating entry into the asphyxiation zone. The oxidation zone on the return side has a width of around 141 m. Figure 2 illustrates the situation of the 22,122 working face and the distribution diagram of the “three zones” of spontaneous combustion in the goaf.
Figure 2. Conditions of 22,122 working face and distribution diagram of goaf oxidation zone 3 experimental analysis of mountain sand paste filling material.
Based on the above analysis, it is evident that there is a significant issue of air leakage at the corners of the 22,122 working face. The current sealing techniques are not effective, resulting in a considerable amount of airflow entering the goaf. Additionally, in the goaf of the 22,122 working face, particularly on the return side, the width of the oxidation zone is excessively large, leading to a heightened risk of spontaneous combustion in the goaf. It is essential to implement effective sealing methods at the corners of the working face to minimize air leakage into the goaf, decrease the width of the oxidation zone, and ensure safe mining operations.