Editorial Feature

The Piezoelectric Effect and Ignition Properties of Coal Mine Gob Roof Explosion

In many countries, coal is the primary source of energy. Although the safety situation in coal mines around the world has substantially improved over the years, serious accidents in coal mines still occur regularly, and the coal mine safety case remains critical.

coal mining, mining safety

Image Credit: King Ropes Access/Shutterstock.com

In China, 55 significant coal mine thermal accidents occurred between 2010 and 2021, resulting in 1074 fatalities, including 27 incidents (49.09%) in the gob and working face, resulting in 508 fatalities (47.3%).

Due to the obvious geological complexity of underground mining, avoiding gas explosions in coal mines has long been a priority and a challenge.

To effectively prevent gas explosions in the coal mining business, more research into the ignition sources in gobs is required.

After mining, a gob is a unique place formed by the collapse and accumulation of rock on the surface of a coal seam. The level of filling is determined by a variety of criteria, such as the height of the rockfall down (seam thickness or mining height), the kind of roof rock, and rock strength features, as well as the distance from the front coal working surface and the depth of mining exploitation.

Previous scholars have looked at the electrodynamic effects of rocks in precise detail. These investigations, however, have mostly targeted the luminescence of rocks in the air and have not taken into account the methane atmosphere.

Electrical ignition properties generated by load crack discharge during coal roof mining are poorly known.

As a result, a paper, published in ACS Omega, investigates the piezoelectric effect of roof deformation and fracture sparking the methane qualities to provide accurate ideas for the prevention and management of gas explosions in the gob. This will be critical for disclosing the process of gas explosions in the stope.


The rock samples were taken from the Renlou coal mine’s roof. To eliminate moisture from the pores, the rock samples were put in a drying cabinet at 80 °C for 12 hours.

Figure 1 depicts the experimental setup. The uniaxial compression experiments were carried out on a hydraulic universal testing machine with loading rates of 0.5 and 5 kN/s.

Schematic diagram of the rock sample discharge experiment system.

Figure 1. Schematic diagram of the rock sample discharge experiment system. Image Credit: Wang, et al., 2022

Results and Discussion

As shown in Figure 2, the quartz source of the Renlou mine sandstone is elevated, accounting for 63.7%, with feldspar (Na2O-Al2O3-6SiO2) source accounting for 28.2%, generating the standard skeletal structure of the sandstone.

XRD results of roof sandstone in the Renlou coal mine.

Figure 2. XRD results of roof sandstone in the Renlou coal mine. Image Credit: Wang, et al., 2022

Figure 3 shows the SEM findings of the rock sample at various magnifications. On the surface of the quartz sample, there are numerous uneven, columnar, or granular bright white spots. It possesses sedimentary rock properties, such as fine grains and small angles, and the grains are tightly bonded to the cementation, resulting in high compressive strength.

This well-developed lamellar structure implies that these rocks are substantially anisotropic and capable of producing piezoelectric effects at both the microscopic and macroscopic levels.

SEM images of the rock samples at different magnifications.

Figure 3. SEM images of the rock samples at different magnifications. Image Credit: Wang, et al., 2022

Figure 4 depicts the discharge patterns of Renlou mine sandstones at 0.5 and 5 kN/s loading rates. Table 1 presents the maximum voltage, loading duration, and peak pressure of the Renlou mine sandstone during the destruction phase at various loading rates.

Discharge patterns of Renlou mine sandstones at two loading rates of 0.5 and 5 kN/s.

Figure 4. Discharge patterns of Renlou mine sandstones at two loading rates of 0.5 and 5 kN/s. Image Credit: Wang, et al., 2022

Table 1. Peak Voltage, Loading Time, and Peak Pressure during the Damage Phase of the Renlou Mine Sandstone at Different Loading Rates. Source: Wang, et al., 2022

Loading rates
Specimen V1max
0.5 1 1.1 0.52 582.5 148.4
2 1.3 0.7 610.3 155.4
3 1.21 0.59 570.2 145.2
5 1 1.78 0.826 70.3 178
2 1.91 0.891 74.1 187.7
3 1.83 0.89 75 189.9


The polarization distribution of charges during the first 3 phases of compression and distortion of the rock can be simplified to a parallel plate capacitor, as illustrated in Figure 5, if the entire rock is treated as a whole during the process of compression.

The faster the rate of pressure exerted, the quicker the electric field varies, the stronger the magnetic field produced, the stronger the energy collected, and the higher the number of charges discharged at the point of fracture, as shown in Figure 4a, b.

Polarization distribution of charges.

Figure 5. Polarization distribution of charges. Image Credit: Wang, et al., 2022

Figure 6 depicts the typical spurting sparks produced by the sandstone as a result of the electron avalanche event.

Spark produced by the roof sandstone.

Figure 6. Spark produced by the roof sandstone. Image Credit: Wang, et al., 2022

Figure 7 depicts the destruction of positive and negative electrons into photons.

Photon emission process.

Figure 7. Photon emission process. Image Credit: Wang, et al., 2022

The thermal concept of ignition and the electrical concept of ignition are two widely accepted hypotheses for the process of electrical spark ignition. The gas mixture burns as a result of the chain reaction.

In conclusion, the researchers note that in the process of gas igniting by the piezoelectric effect of rock, two mechanisms operate simultaneously.

Figure 8 depicts the time scales of particle reactions.

Time scale of particle reactions.

Figure 8. Time scale of particle reactions. Image Credit: Wang, et al., 2022

Three persons were killed in a methane explosion in the Renlou coal mine in 2014. The methane explosion happened unexpectedly. Following the disaster, mine technicians tried several steps to prevent the gob’s coal from self-igniting, but four gas explosions occurred in quick succession.

Figure 9 depicts the accident site of the gas explosion. Table 2 shows the actual explosion times.

Gas explosion accident area.

Figure 9. Gas explosion accident area. Image Credit: Wang, et al., 2022

Table 2.  Exact Explosion Times of the II7322 Gob. Source: Wang, et al., 2022

Explosion Date Time
1st explosion 12 March 15:09
2nd explosion 15 March 18:28
3rd explosion 15 March 20:18
4th explosion 15 March 22:09
5th explosion 17 March 17:11


There was no definite determination concerning the ignition source after the disaster. Some analysts assume the gas-air mixture was ignited by the leftover coal in the II7322 gob self-igniting.

Figure10a depicts the trend of data collected by the CO concentration sensor at the II7322 air return way’s airtight partition wall.

Figure 10b illustrates the CO sensor data variation trend in the II2 mining area’s major return airway. Figure 10c exhibits the CO sensor data variation trend in the II8222 air return way’s outer part.

Variation trend of CO sensor data. (a) Airtight partition wall of the II7322 air return way; (b) main return airway of the II2 mining area.; (c) outer section of the II8222 air return way.

Figure 10. Variation trend of CO sensor data. (a) Airtight partition wall of the II7322 air return way; (b) main return airway of the II2 mining area.; (c) outer section of the II8222 air return way. Image Credit: Wang, et al., 2022

Three individuals were killed by the shock wave while transferring material for the II8222 machine tunnel’s outer section outside the airtight partition wall, whereas the II7322 air return way’s airtight partition walls were uninjured, as illustrated in Figure 9.

The DF48 fault is intersected by the II7222 machine tunnel, II7322 machine tunnel, and II8222 outer section machine tunnel, as depicted in Figure 11.

DF48 fault location map.

Figure 11. DF48 fault location map. Image Credit: Wang, et al., 2022


An experimental system was built and an explosive accident study was undertaken in this work, based on micro-mechanical examination of sandstone samples from the Renlou mine, to examine the probability of a piezoelectric effect igniting methane in the gob, with the following primary conclusions:

(1) The piezoelectric effect and compressive strength are important elements in the collecting of free charges before sandstone fracture.

(2) The rock tip holds a large number of charges at the time of sandstone fracture, generating a “point-surface” effect that causes the electron avalanche.

(3) The spark is orange-yellow and lasts for 22 milliseconds during the electron avalanche, significantly exceeding the ionization energy and ignition induction duration of methane.

(4) The root causes of the creation of electrical discharges and ignition of the gas explosion in the Renlou coal mine II7322 gob are the piezoelectric action and compressive strength of the sandstone.

Journal Reference:

Wang, Y.-N., Wang, D.-M., Xin, H.-H., Zhu, Y.-F., Hou, Z., Zhang, W., Li, M. (2021) Piezoelectric effect and ignition characteristics of coal mine gob roof collapse. ACS Omega, 6(43), pp. 28936–28945. Available Online: https://pubs.acs.org/doi/10.1021/acsomega.1c03987?ref=pdf&.

References and Further Reading

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Laura Thomson

Written by

Laura Thomson

Laura Thomson graduated from Manchester Metropolitan University with an English and Sociology degree. During her studies, Laura worked as a Proofreader and went on to do this full time until moving on to work as a Website Editor for a leading analytics and media company. In her spare time, Laura enjoys reading a range of books and writing historical fiction. She also loves to see new places in the world and spends many weekends looking after dogs.


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