Study on Pore and Fissure Structure Characteristics of Deep Soft Coal Rock

The microscopic pore and fissure structure is the key factor affecting the exploitation, storage, and migration of coalbed methane and coal spontaneous combustion tendency. For further research of the microstructure of deep soft coal rock, such as pores and fissures, the coal samples from the Yangdong mining area were qualitatively and quantitatively analyzed in terms of morphological characteristics, pore shape, pore specific surface area, pore volume, and pore diameter by a scanning electron microscope (SEM) and a low-temperature liquid nitrogen adsorption experiment. The results show that there are three major categories and five minor categories of pores with different genetic types, including metamorphic pore, exogenous pore, and mineral pore, and there are endogenous fissures, exogenous tensile fissures, and exogenous shear fissures developed in the coal body. According to the results of the low-temperature liquid nitrogen adsorption experiment, the hysteresis curves of coal samples can be divided into two types. The I type curve produces a loop. There is a “hysteresis loop” which is obvious, and there is an inflection point that is not obvious. The pore system is mainly composed of open pores. The II type curve has no adsorption back line and no obvious inflection point. The pore structure is mainly composed of an impermeable hole closed at one end. The BET specific surface area of coal samples ranges from 0.2810 to 4.7569m/g, with an average of 1.27984m/g. The BJH pore volume ranges from 0.002864 to 0.007377 cm/g, with an average of 0.0041246 cm/g. The average BJH pore diameter of coal samples ranges from 4.3935 to 20.1501 nm, with an average of 16.0313 nm. The pore specific surface area of coal is mainly contributed by micropores, and the transition pores contribute the most to pore volume. The distribution of pore volume in each pore section of a coal sample has the rule that the transition pore is larger than the micropore, and the micropore is larger than the mesopore, and the maximum ratio is 66.2%. The distribution of pore specific surface area has the rule that the micropore is larger than the transition pore, and the transition pore is larger than the mesopore. The maximum ratio is 91.2%.


Introduction
Coal is a kind of porous medium material, and its microscopic pore structure determines the adsorption, desorption, diffusion, seepage, and mechanical properties of coal. [1,2] The pore and fissure structure of a coal body has a significant influence on the exploitation, storage, migration, and spontaneous combustion tendency of coal, and it is also a key factor affecting the extractability of coalbed methane [3,4]. As early as the 1960s, domestic and foreign scholars have begun to study the micropore structure of coal. Gan et al. believes that with the demand for energy and the development and utilization of coal and coalbed methane, people pay more and more attention to the study of coal pore structure [5]. The research methods of domestic and foreign scholars on the distribution characteristics of coal's microstructure and morphological development, pore and fracture types, and pore volume and specific surface area mainly include observation description and physical tests [6]. The observation description method mainly includes macrodescription and imaging of coal samples with an optical microscope, while common physical test methods include the densitometer algorithm, the mercury injection method (MIP), the low-temperature nitrogen or CO 2 adsorption method, the scanning electron microscope (SEM), the nuclear magnetic resonance method, and the microscopic CT scanning method [7][8][9].
Li et al. [10] studied the relationship between the pore structure characteristics and structural deformation of tectonic coal in the Hancheng mining area using the microscopic CT test, and the study showed that cataclastic coal had the best pore connectivity and permeability, while mylonite coal had the worst. Meng et al. [11] studied Dongqu coking coal by using the microscopic CT and mercury injection test, and they obtained its pore diameter and morphology and other characteristics and believed that micropores were the main cause of poor permeability and connectivity. Thompson et al. and Kueper et al. [12,13] first studied the porous material and calculated its fractal dimension. Wang et al. [14] studied the influence of coalification on the pore structure of the middle and high rank coal, and they found that micropores and transition pores accounted for the largest proportion of volume and specific surface area in middle and high rank coal. With the increase of coal rank, the fractal dimension of micropores gradually increased. Nie et al. [15] labeled the pore types in SEM images of coals with different metamorphic degrees. According to Mahamud's research [16], when the pressure of mercury injection is greater than 10 Mpa, the coal sample will produce a compression effect and destroy the coal's primary pore system. Cai et al. [17] used a small-angled ray combined with a scanning electron microscope to study and find out if the coal pores are mostly spheroid in low coal rank and ellipsoid in high coal rank. Klimenko et al. [18] used the conditional moment model to study the fractal characteristics of transportation, storage, and adsorption processes in the pores of CO 2 porous media. Li et al. [19] adopted SEM, lowtemperature liquid nitrogen adsorption methods, and CO 2 adsorption methods for 8 kinds of coals with different metamorphic degrees to analyze parameters such as pore volume, pore diameter, specific surface area, and pore shape, and they obtained the heterogeneity of the pore morphology of coals with different ranks. Jiang et al. [20] studied the pore characteristics of structural coal and divided the lowtemperature liquid nitrogen adsorption loop lines of coal samples into three categories. It is considered that there are four kinds of pores in coal: cylindrical pores with openings at both ends, cylindrical pores with openings at one end, ink bottle pores, and slit flat pores. Sun, Li and Wang, and Li et al. [21][22][23] also conducted low-temperature liquid nitrogen adsorption experiments under different metamorphic coals, different temperatures, different coal body structures, and different coal mines, so as to study the pore structure, pore volume and pore diameter distribution, and adsorption characteristics of coals under different conditions.
The pore-fissure structure of coal rock is closely related to coal seam mining and gas extraction, and it has a certain influence on coal spontaneous combustion. The pore-fissure structure in deep soft coal rock is extremely complex, and the pore size distribution varies from millimeter to nanometer. The different pore sizes control the adsorption, apportionment, diffusion, and seepage of coalbed methane. The traditional scanning electron microscope method only qualitatively studies the pore and crack parameters on the polished surface of a coal sample, but it cannot deeply study the internal pore structure of coal, which has limitations. In this paper, the method of SEM and low-temperature liquid nitrogen adsorption experiment is adopted. It is of great significance to the coalbed methane resource evaluation, exploration, and development for a qualitative and quantitative characterization of the innovative ways of combining different scales of deep soft coal rock micropore structure research and analysis of the changing rule of the specific surface area and pore volume of coal and the pore size distribution of laws and so on.

Experimental Samples and Methods
The coal sample in this experiment is taken from the Yangdong well field of the Fengfeng coalfield, which is located in the east wing of the middle part of the Fengfeng coalfield. The coal quality belongs to the section of coking coal, thin coal, and lean coal in the metamorphic zone of the Fengfeng coalfield. The industrial analysis of raw coal quality is shown in Table 1: According to the relevant standards of "GB/T482-2008 Coal Sample Method for Coal Seam" and "SY/T6154-1995 Determination of Static Nitrogen Adsorption Capacity by Rock Specific Surface and Pore Diameter Distribution," the no. 2 coal (large coal) of the Permian Shanxi Formation in Yangdong Mine was collected as experimental coal samples, and the collected coal samples were sealed and stored in sealed bags with labels and transported to the laboratory.

Scanning Electron Microscope Observation Method.
According to the test requirements of the samples in the laboratory, the collected large coal samples are cut at a slow speed. The size of the cut is generally about 1 cm × 1 cm × 1 cm, which is a relatively regular cube. If there is secondary damage to the coal in the cutting process, the sample will be scrapped. One side of the qualified small sample is ground and disassembled; that is, the gauze is used for smooth and slow grinding, respectively. The side after disassembling is selected as the observation surface, and its surface is purged for clean treatment, and then dried. Then, conductive treatment (the observation surface is plated with a conductive layer) is conducted for experimental observation. The experimental instrument utilized here was the JSM-5510LV scanning electron microscope from Japan Electron Optics Laboratory Co., Ltd., as shown in Figure 1. The instrument resolution was 3.2 nm, and the magnification was continuously adjustable from 18 to 300,000. The surface of the sample was observed by secondary electronic imaging, and the apparent morphology and pore-fissure structure of the sample were analyzed.

Low-Temperature Liquid Nitrogen Adsorption Method.
According to the requirements of the experimental test, the large coal samples collected were crushed with a crusher in the laboratory, and then the crushed coal samples with a particle size of 60 to 80 mesh were screened out by a standard sieve. The prepared coal samples were put into a 105°C electric heating blast drying oven to dry, and then they were bottled and sealed for storage for experimental use. The experimental instrument utilized here was the ASAP-2000 automatic specific surface and aperture analyzer produced by Micromeritics Instrument Co., Ltd., as shown in Figure 2. The test was carried out according to the national standard "Determination of specific surface area of solid substance by gas adsorption BET method" (GB/T19587-2017). The instrument has high testing accuracy, the specific surface area analysis range is from 0.0005 m 2 /g to none, the pore diameter analysis range is 0.5 to 500.0 nm, and the pore volume minimum can detect 0.0001 cm 3 /g. The nitrogen adsorption method is used to measure the pore structure distribution characteristics of the coal sample, such as the specific surface area, pore diameter, and pore volume. According to the scanning electron microscopy results of the coal samples in Figure 3, five types of pores are developed in the coal samples, including the granular pore, the breccia pore, the friction pore, the intergranular pore, and the air vent. The coal body as a whole is a collection of broken particles; the structure is loose, the whole coal body is flaky, the granular pore is attached to the surface of the coal body, and they have different shapes and sizes, irregular shapes, and relatively developed pore structures. Most of the pores are filled and stacked with minerals, including granular pores (Figure 3(a)), breccia pores (Figures 3(a) and 3(b)), and intergranular pores (Figure 3(c)). The coal body is damaged by the weak tectonic stress field or external factors, and it forms a sharp corner shape with a relatively regular shape. There is basically no displacement between the holes, and the connectivity is good. The holes formed between the breccia (i.e., the breccia holes) are exogenous holes. The pore diameter generally ranges from 2 μm to 10 μm, which is usually found in cataclastic coal. There are some clastic minerals filling in the pore, but it will not seriously block the pore fissure and has a certain permeability. A fragmentary hole is a kind of exogenous hole formed after being damaged by strong tectonic stress, and the shape of the crushed grain is mostly a sheet, block, or semicircle. It is small in volume and easy to accumulate. It is a displacement hole formed between the crushed grains and has good connectivity. The pore diameter range is generally 0.5 to 5 μm, and it is mostly found in cataclastic coal and crushed coal. Because severe fissures will block the pore and fissure, it has a certain influence on the permeability of a coal reservoir. Intergranular pore is the pore between the mineral grains, and it is a mineral pore. The pore diameter is generally micron sized, which is less developed in the coal body and has little influence on the permeability of a coal reservoir.
It can also be seen from the figure that the structure on the surface of the coal body is becoming denser, with fewer fissures and macropores. The pores are more elliptical and    developed. Under the action of compressive stress, and due to friction or the sliding movement between the coal face and the surface, there is the formation of grooves, round lines, and long triangular or linear holes (namely friction holes) that are exogenous holes. The pore diameters vary from 1 to 2 μm to dozens of microns. The pores are partially connected, which has a certain effect on the migration of (d) Air vent  5 Geofluids coalbed methane. The pores exist in cataclastic coal and crushed coal. The air vent is a kind of metamorphic pore, which is mostly round, oval and tubular with smooth edge and formed by "gas generation" and "gas accumulation" due to coalification in the coal-forming period. The common stomata size is 0.1 to 3 μm, the development is more concentrated, about 1 μm is more common, the stomata are independent of each other, the connectivity between the pores is not good, and the pores are developed in both primary coal and structural coal.

Analysis of Coal Fissure
Characteristics. The fissure in the coal body is due to the coal seam in the coal-forming period by the nature of various stresses, such as tectonic stress and geological stress, resulting in the coal body fissure, section opening or fissure, and other non-closed-state fissure phenomena. Research on coal microfissures began last century, but research progress is relatively slow. It was not until the 1960s, when Ammosov and Eremin [24], both scholars of the former Soviet Union, put forward their ideas in the book "Fissures in Coal." Since then, the research on coal body fissures gradually became mature. Later, the term "cleat" was proposed to describe endogenous fissures, and cleat can be divided into facet cleat and end cleat [25]. On the basis of previous research, this paper also divides the fissures in the coal into two types: endogenous and exogenous.
As can be seen from Figure 4, there are endogenous fissures and exogenous fissures developed in the coal samples, and their morphology, size, and genesis are different. In the endogenous fissure, coal is densely developed, with few fillings and no scratches on the surface, which are relatively flat and have tensile characteristics (as shown in Figure 4(a)). Fills in cleats are generally autogenic minerals and rarely fill broken coal particles. Under certain tectonic action, dislocation or extrusion occurs between coal bodies, resulting in fissures or openings, and exogenous tensile fissures and shear fissures can be seen (as shown in Figures 4(c) and 4(d)). Due to the effect of tensile stress, the exogenous tensile fissure has a large opening, appearing as a narrow and long opening (as shown in Figure 4(d)). There is no scratch on the surface, and some debris will be filled in the fissures, with cracks ranging from a few microns to dozens of microns. Exogenous shear fissures rupture due to the action of shear force, showing staggered small fissures and long extension. The fissure has a small opening and is basically closed (as shown in Figure 4(c)). Most fissures are imbricated or stepped, and some are also X-shaped, with good ductility and debris filling.

Analysis of Low-Temperature Liquid Nitrogen Adsorption Experiment Results
The pore structure of coal is complex, and the pore diameter distribution varies from millimeter to nanometer. Therefore, the study of the pore structure of coal not only needs qualitative characterization but also needs to be combined with quantitative calculation to be more accurate. The above SEM results are used to qualitatively characterize the morphological characteristics of pore fissures on the surface of a coal body. The observed coal body morphological characteristics were relatively rough. The characteristics of micron and millimeter pores and fractures in coal samples can be clearly observed, but the nanosized pores cannot be detected. Therefore, the low-temperature liquid nitrogen adsorption experiment can be used to characterize the finer pore structure and morphological characteristics in coal.

Isothermal Adsorption Curve Analysis.
Isotherma adsorption curve can well reflect the surface adsorption characteristics of coal samples, and pore morphology characteristics of experimental coal samples and pore diameter distribution which plays a major role in adsorption can be seen from the adsorption curve and desorption loop. The adsorption isotherm of each coal sample is shown in Figure 5.
The International Union of Pure and Applied Chemistry (IUPAC) classify the isotherm adsorption curve into six types [26]. Compared with the six adsorption isotherms, the nitrogen adsorption isotherm of coal samples tends to belong to the IV adsorption isotherm as a whole, but it is not the same as it. The overall adsorption curve shows an upward trend, and the adsorption curve is lower, while the desorption curve is higher. When the relative pressure is greater than 0.9, the curve rises steeply, and the adsorption volume increases sharply. The curves show that at the beginning, the single-layer adsorption transitions to multilayer adsorption at the low pressure stage. As the relative pressure continues to increase, multilayer adsorption begins to appear, and the adsorption amount gradually increases until the multilayer adsorption gradually forms, and the adsorption layer is infinite when the saturated vapor pressure is reached. In the middle and high pressure stage (the relative pressure is greater than 0.5), the separation phenomenon of the adsorption curve and the desorption curve gradually appears, and the hysteresis loop is produced, namely, the hysteresis loop. The appearance of the adsorption hysteresis ring is caused by capillary condensation on the surface of coal under high pressure (the relative pressure is greater than 0.9).
It can be seen from the hysteresis loop of the coal sample in this experiment that its hysteresis loop type does not strictly belong to the specific type divided by IUPAC. Each type of adsorption hysteresis loop represents different pore structures and reflects the adsorption capacity and air permeability of coal. Referring to the study of adsorption experiments on a large number of coal samples by Chen and Tang [27], the adsorption isothermal hysteresis curve characteristics of coal samples in this experiment were observed and compared, and the adsorption isothermal hysteresis curves were divided into two types: (1) I type: nos. 1, 2, 3, and 4 coal samples are representative, the normal type curve produces a loop, the desorption curve and the adsorption curve do not completely coincide, the curve "hysteresis loop" is obvious, and the inflection point is not obvious, indicating that there is no "ink bottle" like hole in the coal sample. The adsorption curve and desorption 6 Geofluids curve basically overlap at low and high relative pressure, and the inflection point occurs when the relative pressure is about 0.5. In the region of 0.45 to 0.95, the capillary condensation phenomenon occurs in the coal body, and the "hysteresis loop" is generated, which is because the pressure required for the capillary condensation of the coal body is less than that of evaporation. It shows that there are closed holes at one end in the low pressure and high pres-sure stages, which mainly include cylindrical holes, parallel plate holes, wedge-shaped holes, and tapered holes at one end. In the middle and high pressure stage, the pore system is mainly composed of open pores, including cylindrical pores at both ends and parallel plate pores at four sides, and part of slit pores. Such pore structure is conducive to the migration of coalbed methane, and has good permeability and connectivity  (2) II type: the no. 5 coal sample is representative, the normal type curve does not produce the adsorption back line, the desorption curve and the adsorption curve almost completely coincide, and the hysteresis phenomenon is not obvious, i.e., there is no obvious inflection point; this is because this kind of coal sample coal capillary condensation and evaporation required pressure that is basically equal. This shows that the pore structure of this kind of coal sample is mainly composed of impermeable pores with one end closed, including cylindrical holes, parallel plate holes, wedge-shaped holes, and tapered holes with one end closed. The pore connectivity is poor, which is not conducive to the exploitation and migration of coalbed methane. The poor connectivity between pores is not conducive to the exploitation and migration of coalbed methane 4.2. Specific Surface Area and Pore Volume Analysis. As a solid material of porous medium, coal's specific surface area is a powerful index to show the adsorption capacity of coal seam, and the adsorption capacity of coal presents a positive correlation with the change of the specific surface area. The specific surface area results obtained by different calculation models are also different. The specific surface area obtained by the BET calculation model is the most common method. In this experiment, the BET equation [28] based on the multimolecular layer adsorption theoretical model is used to characterize the specific surface area: where W is the weight of adsorbed gas at the relative pressure (P/P 0 ); W m is the weight of adsorbed gas covered by a single surface; P/P 0 is the adsorption relative pressure; P is the equilibrium partial pressure of adsorbed mass; P 0 is the saturated vapor pressure of the adsorbent; C is the BET constant, which is related to the adsorption energy of the first adsorption layer.
In physical adsorption, the adsorption between solid and gas is dependent on the intermolecular gravity and occurs. The molecules that have been adsorbed still have gravity; so, on top of the first layer of adsorption, they can also adsorb a second layer, a third layer …, that is, multimolecular layer adsorption. Pore volume (also called pore volume) mainly shows the total pore volume per unit mass. Table 2 shows the distribution characteristics of pore structure parameters of coal samples obtained under the lowtemperature liquid nitrogen adsorption experiment.
The results show that the BET specific surface area of coal samples ranges from 0.2810 to 4.7569 m 2 /g, with an average of 1.27984 m 2 /g. The specific surface area of BJH ranges from 0.5686 to 6.7164 m 2 /g, with an average of 1.9034 m 2 /g. The BJH specific surface area is larger than that of BET on the whole, but the changing trend remains consistent. The total pore volume of the single point method of a coal sample ranges from 0.002865 to 0.007375 cm 3 /g, with an average of 0.004132 cm 3 /g. BJH pore volume ranges from 0.002864 to 0.007377 cm 3 /g, with an average of 0.0041246 cm 3 /g. Generally speaking, the difference between the two is very small. The BJH average pore diameter of a coal sample varies greatly from 4.3935 nm to 20.1501 nm, with an average of 16.0313 nm. Figure 6 is the fitting curve of the relationship between specific surface area and pore volume. It can be seen that there is a positive correlation between specific surface area and pore volume, and both specific surface area and pore volume of coal samples in the mining area are small. Figure 7 shows the pore specific surface area and pore volume increment diagram under different pore diameters. The relation diagram of the pore specific surface area and pore diameter shows that the curve trends of coal samples 01, 02, 03, and 04 are similar, with peaks at about 3 to BET surface area (m 2 /g) Figure 6: BET specific surface area and BJH pore volume fitting curve.
8 Geofluids 4 nm and 20 to 40 nm, indicating that micropores and transition pores have a large contribution to the specific surface area of coal samples. However, the curve of coal sample 05 is different from the other four coal samples. As can be seen from the figure, the peak appears at the aperture of about 2 nm, and then it gradually decreases, but it still keeps a large value. After 10 nm, it becomes very low and flattens out, indicating that the micropores within the range of 2 to 10 nm make a great contribution to the specific surface area of coal samples. As can be seen from the diagram of the relationship between pore volume increment and pore diameter, the pore volume increment increases continuously with the increase of pore diameter. The peak value of coal samples 01, 02, 03, and 04 is mostly at the aperture of 30 nm and 100 nm, while the peak value of coal sample 05 is at 10 nm and 50 nm, indicating that the transition hole plays a major contribution to the pore volume of coal sample.

Analysis of Pore Diameter Distribution Characteristics.
The classification methods of apertures usually include the B.B. Hodot decimal division and the IUPAC classification. There are many calculation models for apertures, including BJH, D-H, HK, DFT, and NLDFT. [29] In this paper, the  9 Geofluids BJH theoretical model is used for pore diameter analysis of coal samples, and the B.B. Hodot decimal division method [30] is used for the coal pore type division system. According to the classification system, the pore diameters of coal can be divided into four types: macropore (>1000 nm), mesopore (100-1000 nm), transition pore (10-100 nm), and micropore (<10 nm). The pore diameter distribution range of each sample recorded by the instrument in this experiment is 1.7 nm to 300 nm. Figure 8 shows the pore diameter distribution characteristics of a coal sample obtained under the low-temperature liquid nitrogen adsorption experiment.
In Figure 8, dV/dD represents the differential of total pore volume to pore diameter, and it represents the distribution function of pore volume density. The peaks protruding from this curve represent the most concentrated pore diameter range in the measured coal sample. As shown in Figure 8, the pore diameter distribution of each coal sample in the region of 2 to 20 nm presents a single peak distribution phenomenon, which indicates that the pore diameter of a coal sample is mainly distributed in the region of 2 to 20 nm, and the main peak is mainly around 2 to 5 nm. Therefore, the micropores and transition pores larger than 2 nm contribute greatly to the pore volume. Generally speaking, pores with pore diameter less than 100 nm, especially micropores, are the main factors that determine gas adsorption, storage, and migration. Therefore, the distribution of micropore diameter in coal plays a leading role in gas storage and migration in coal seams.
According to the classification of coal samples according to the low-temperature liquid nitrogen adsorption isotherm above, the pore diameter distribution curve is also divided into two kinds. The peak value of coal samples 1 to 4 appears at around 4 nm, and both ends of the peak value plummet, indicating that the pore diameter distribution is most concentrated when the pore diameter is 4 nm. The curve has a flat trend in the range of 5 to 20 nm, indicating that there are a large number of micropores and transition pores in this range, and the pore diameter distribution is uniform, but there is no particularly concentrated distribution of pores. The peak value of coal sample 05 appears at 2 nm, indicating that the pore diameter distribution is most concentrated at the pore diameter of 2 nm. The curves at both ends of the peak value did not drop suddenly, but the peak value gradually decreased with the increase of pore diameter until 20 nm, indicating that the micropores and transition pores at 2 to 20 nm accounted for the majority of the coal sample 05. In general, micropores and transition pores play an absolute role in controlling the specific surface area and pore volume of coal samples, respectively. Table 3 shows the pore diameter distribution and proportion characteristics of coal samples obtained under the low-temperature liquid nitrogen adsorption experiment, and Figure 9 shows the specific surface area and pore volume proportion of each pore diameter segment. It can be seen that the percentage of pore volume in each pore diameter section of a coal sample is dominated by transition pores, and transition pores make the largest contribution to pore volume. Micropore volume accounts for 12.4% to 61.1% of the total pore volume, transition pore volume accounts for 25.8% to 66.2%, and middle pore volume accounts for 13.1% to 26.1%. The specific surface area of each pore section of a coal sample is dominated by the proportion of micropores, which contributes the most to the specific surface area. The proportion of micropores was 56.2% to 91.2%, the proportion of transitional pore specific surface area was 7.6% to 40.87%, and the proportion of middle pore specific surface area was 1.2% to 3.9%. The results of aperture ratio analysis are consistent with those in Figure 8. The distribution of pore volume in each pore section of a coal sample has the rule that the transition pore is larger than the micropore, and the micropore is larger than the mesopore, and the maximum proportion is 66.2%. The distribution of pore specific surface area show that the micropore is larger than the transition pore, and the transition pores are larger than the mesopores. The maximum ratio is 91.2%.

Discussions
By comparing the results of scanning electron microscopy of the coal samples in the study area, it can be found that there are metamorphic pores, exogenous pores, and mineral pores in the coal, and there are endogenous fractures, exogenous tensile fractures, and exogenous shear fractures in the coal. This is because the tectonic stress fields or external factors cause different degrees of damage to the coal body, resulting in different types of pore fractures. By comparing the isothermal adsorption curves of coal samples and referring to previous studies and distinguishing from their classification criteria, the analysis shows that the isothermal adsorption curves of coal samples in the study area can be divided into two types, and the pore structure system of coal samples is mainly composed of open pores and impermeable pores closed at one end. This condition is because different holes will produce different hysteretic curves. 10 Geofluids According to Figure 10, qualitative analysis was made on the variation of specific surface area and pore volume with pore diameter of coal samples in the study area. It can be seen from the overall trend of the relation curve between incremental pore area and pore diameter that there are different peaks in the range of the pore diameter of coal, especially in the range of a micropore, indicating that a micropore has a large contribution to the specific surface    area of a coal sample, accounting for the largest proportion. From the overall trend of the relation curve between incremental pore volume and pore diameter, it can be seen that the incremental pore volume increases with the increase of pore diameter and presents the characteristics of multipeak distribution. The most obvious peak value is mostly located within the range of the transition hole, indicating that the transition hole plays a major contribution to the pore volume of a coal sample and accounts for the largest proportion.
On the basis of qualitative analysis, quantitative analysis was carried out on the average proportion of specific surface area and pore volume of each pore section of coal sample. As can be seen from Figure 11, the micropores accounted for 23.56% of the total pore volume, the transition pores accounted for 21.80%, and the mesopores accounted for 54.64%. The specific surface area of micropores, transition pores, and mesopores accounted for 65.86%, 31.26%, and 2.88%, respectively. The results show that the distribution of pore volume in each pore section of a coal sample has the rule that the transition pore is larger than the micropore, and the micropore is larger than the mesopore. The distribution of the pore specific surface area has the rule that the micropore is larger than the transition pore, and the transition pore is larger than the mesopore. This is because micropores and transition pores make major contributions to the pore specific surface area and pore volume of coal samples, respectively, and the greater the contribution, the greater the proportion. The research results have certain practical significance for the design of gas extraction, coal seam mining, and migration in the study area.

Conclusion
(1) SEM results show that there are three types of pores, namely, metamorphic pores, exogenous pores, and mineral pores, and there are five subtypes of pores with different genetic types, such as air vent, granular hole, breccia pores, friction pores, and intergranular pores. The pore diameter is generally in the transition range from nanometer to micron. There are endogenous fractures, exogenous tensile fractures, and exogenous shear fractures developed in the coal body. The overall development is relatively compact and flat. The research on fractures is on the micron scale, generally ranging from a few to dozens of microns (2) The low-temperature liquid nitrogen adsorption experiments show that there are two main types of hysteresis curve. The I type curve produces a loop.
A "hysteresis loop" is obvious, and an inflection point appears, but it is not obvious. The II type curve does not produce an adsorption back line and has no obvious inflection point. The pores of coal samples are mainly composed of open pores and impermeable holes closed at one end. The average pore diameter is 16.0313 nm, and the pore specific surface area and total pore volume are small, averaging 1.27984 m 2 /g and 0.0041246 cm 3 /g, respectively (3) The pore specific surface area and pore volume of coal are mainly contributed by micropores and transition pores at 2 to 20 nm. The distribution of pore volume in each pore section of a coal sample has the rule that the transition pore is larger than the micropore, and the micropore is larger than the mesopore, and the maximum ratio is 66.2%. The distribution of specific surface area has the rule that the micropore is larger than the transition pore, and the transition pore is larger than the mesopore, and the maximum ratio is 91.2%.

Data Availability
The data used to support the findings of this study have not been made available because the original data relate to the intellectual property rights of the author, and all the original data cannot appear in the paper, and the experimental data that cannot appear is related to privacy.

Conflicts of Interest
All authors declare no conflict of interest.