Abstract
Better understanding of the storage and transportation characteristics of methane in coal seams is important to further develop and utilize the methane resources in the coalbed. This study is devoted to investigating the relationship between methane adsorption performance and pore structure by analyzing twelve coal samples derived from the typical methane-rich coalbeds in China. To eliminate the influence of inorganic components such as ash in different coal samples, a specific fixed-bed reactor with internals was employed for the coal treatment. Based on N2/CO2 adsorption analysis at low-pressure condition, the pores in coal were classified into three types in this study: ultra-micropore (pore width < 1 nm), micropore (1 nm < pore width < 2 nm) and mesopores (2 nm < pore width < 50 nm). According to the Langmuir equation, the Langmuir volume (VL) and Langmuir pressure (PL) were calculated to characterize the high-pressure adsorption of methane, and the influence of methane adsorption associated parameters was evaluated. The results indicate that N2-pore size distributions (1–50 nm) varied a lot among samples, suggesting the significant heterogeneity of pore structure among samples. Estimated by the FHH model, pore surface fractal dimension (D1) and spatial geometry fractal dimension (D2) were, respectively, ranging in 2.059–2.808 and 2.649–2.852, which indicated that the more irregular surface, namely more inhomogeneous pore structures, resulted in the more surface area and stronger adsorption capability. By grey relational analysis (GRA), the importance of the pore structure factors on methane adsorption was identified, as an order from the most important to the least: ultra-micropore volume (0.9085) > ultra-micropore surface area (0.8976) > fractal dimension D1 (0.8862) > N2-BET surface area (0.7915) > micropore volume (0.5035) > micropore surface area (0.5006). This study shows the influence of parameters of pore structure on methane adsorption of coal and clarifies the order importance of these parameters by the GRA method.
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Introduction
Methane is the main component of coal bed methane (CBM), accounting for 95–98% of its volume. Its absorbability and flowability in CBM system are closely related to the pore structure of coal (Zhang et al. 2019b; Fan et al. 2020). Thus, it is of great significance to investigate the pore structure of coal, which is related to methane adsorption capacity. Coal is found to be a natural polymeric material with anisotropic porous structures (Gorbaty et al. 1986; Liu et al. 2019). It is generally believed that pores in coal have a wide size distribution and formed an interconnected network (Everett 1972). The pore size distribution of coal usually includes micropores (pore width < 2 nm), mesopores (2 nm < pore width < 50 nm) and macropores (pore width > 50 nm), according to the International Union of Pure and Applied Chemistry (IUPAC) classification standard (Everett 1972; Macuda et al. 2020).
Different methods with varied purposes and accuracies have been adopted to investigate the pore structure of coal, such as nuclear magnetic resonance spectroscopy (NMR) (Genty et al. 2007; Yao et al. 2014), small-angle X-ray scattering (SAXS) (Zhao et al. 2014), small-angle neutron scattering (SANS) (Mastalerz et al. 2012), high-resolution transmission electron microscopy (HRTEM) (Harris and Yust 1976), Mercury intrusion porosimetry (MIP) (Clarkson and Marc Bustin 1996; Zhang et al. 2019a) and N2/CO2 gas adsorption analyses (Nguyen and Bhatia 2007). Each of these widely used techniques detects only a specific aperture range, but they cannot be used independently to describe the overall porosity or pore size distribution of samples. Among all the techniques, N2/CO2 gas adsorption analyses have been used widely to describe pore size distribution (Okolo et al. 2015). Okolo et al. (2015) used CO2 gas adsorption techniques combined with the Horvath–Kawazoe (H–K) method and could only detect pores within the range of 0.3–0.65 nm. Mastalerz et al. (2008, 2012) stated an upper limit of 0.85 nm. N2 analysis was believed to be able to detect the pores in the range from 1.7 to 300 nm. CO2 gas adsorption is capable of measuring ultrafine micropore, while N2 adsorption can provide a deep insight into the mesopore size distribution (Mahajan 1991; Walker and Mahajan 1993). Previous studies showed that most ranges of pore size distributions can be described by combining these two techniques. The properties of micropore sizes in the range of 0.85–1.7 nm are unclear and need further study (Okolo et al. 2015).
Based on the study of coal structure, further studies provided useful information about pore structure and methane adsorption capacity with N2 and CO2 adsorption. Experimental evidence shows that micropores play a dominant role in the adsorption of methane by coal (Hao et al. 2013). Yao et al. (2008) found that higher fractal dimension D1 correlated with surfaces with higher irregularity, which provided more adsorption sites for methane. Higher fractal dimension D2 was accompanied by higher heterogeneity of pore structure and higher liquid/gas surface tension that reduced CH4 adsorption capacity (Yao et al. 2008; Li et al. 2018). Cai et al. (2013) found that adsorption-pore (pore size < 100 nm) controlled gas adsorption/diffusion, while seepage-pore (pore size > 100 nm) had obvious effects on and gas flow in coal seam. However, few studies had focused on quantitative analysis of influence degree related to these parameters. Analyzing the methane adsorption associated with the pore parameters independently and qualitatively needs further systematic and quantitative mathematical comprehensive investigation.
In this work, an indirectly heated fixed-bed with internals was employed for the treatment of coal samples, which made the modified samples with the same ash composition but different pore structures. This new reactor has been devised to enhance the heat transfer and pyrolysis performance, significantly increasing the coal tar yield and the transformation of char morphology structure (Hu et al. 2017). Besides, we adopted grey relational analysis (GRA), which is a useful method to evaluate the influence of various parameters without knowing their complex relationships (Zuo et al. 2016). The GRA method has been applied widely in various fields such as engineering technology, medicine, agriculture, petroleum industry and biology. However, the application of the GRA method to methane adsorption has not been reported to our limited knowledge. Therefore, this work aimed to: (1) describe the full range of micro-/mesopore size distribution; (2) define the pore structure parameters associated with methane adsorption capacity by linear fitting; and (3) study the influence degree of structure parameters, and try to find the sequence of degrees by GRA method.
Methodology
Samples and Thermal Conversion Procedure
Six typical different coal samples with different coal ranks were collected from active underground coal seams in China. All samples were crushed into 40–80 mesh size particles and were sealed and evacuated at 80 °C for 24 h before heat treatment. The heat treatment experiments adopted a fixed-bed reactor made of 304-type stainless steel (Fig. 1). The reactor was 400 mm in height and 30 mm in inner diameter. A screen plate was welded in the right middle of the reactor to support the coal samples. Above the screen plate, there were four metal plates attached to the wall of the reactor at the angles of 90° with their width of 10 mm, height of 100 mm and thickness of 3 mm. The reactor was electrically heated externally with its temperature controlled by a proportional integral and differential controller connecting with a thermocouple. Nitrogen was adopted as the carrier gas with a flow of 100 ml/min and purity of 99.99%. 30 g coal sample was added to the reactor and heated to the preset temperature under nitrogen atmosphere. Nitrogen flow was not terminated into the reactor until its temperature dropped to room temperature. Then, modified coal samples were named in the form of “coal seam—treatment temperature (°C)—treatment time (hour)”. The proximate and ultimate analysis data are shown in Table 1, according to the ASTMD7582 method (Xu et al. 2018b, 2019).
N2/CO2 Adsorption Characterization
Nitrogen and CO2 adsorption characterization was performed via a physisorption apparatus (Quantachrome autosorb-6b/3B). The adsorption curves of nitrogen were measured at − 196°C under relative pressures (the gas pressure/the saturated vapor pressure, P/P0) ranging from 0.001 to 0.995. The adsorption curves of CO2 were measured under 0 °C within the standard atmospheric pressure range (0–0.101325 MPa). All samples were dried under vacuum at 80 °C for 10 h prior to the adsorption tests (Jagiello et al. 2015). The parameters of the pore were calculated by means of density functional theory (DFT) and automatically by the software of the physisorption apparatus (Nie et al. 2015).
High-Pressure Adsorption
Adsorption isotherms of methane under high pressure (up to 16 MPa) were obtained by static volumetric adsorption method (MTT752-1997, China standard). Approximately 15 g of the sample was used for each measurement. The void volume of the sample tube was measured by helium at the test temperature and then degassed at 80 °C for 10 h under vacuum. The methane adsorption capacity was measured with its peak pressure approached 16 MPa. The adsorption isotherm was analyzed to obtain adsorption parameters with the Langmuir model as (Langmuir 1918):
where VL, the Langmuir volume, is the maximum adsorption capacity of the material, while PL, the Langmuir pressure, is the corresponding adsorption pressure when the adsorption volume (V) reaches half of VL.
Grey Rational Analysis Calculation
GRA was used to calculate and compare the influence degree of pore parameters. The adsorption capacity, VL, was expressed as V = {x10, x20,…, xm0}.The adsorption parameters schemes were expressed as F = {F1, F2,…, Fn}. Factor i of the sample j was expressed as xij. Due to different dimensions and units, the numerical values of different factors varied significantly. The different factors were standardized and transformed to compare after dividing by the average of the series. The standardized treatment of different factors was calculated as:
After standardization, the evaluation factors were converted into Rj = (r1j, r2j,… rmj)T, while the optimal factor was converted into R0 = (r10, r20,… rm0). The multidimensional grey relational coefficient was calculated as:
where ρ was applied to prevent the effect of maxi|ri0 − rij| from becoming too large, thus controlling the amplifying effect of different relation coefficient. In this study, ρ was set to 0.5, the recommended value, which ensured both moderate distinguishing effects and good stability of outcomes (Nelabhotla et al. 2016).
The multidimensional grey relational matrix U was calculated from the matrix Rn (m factors of n samples) and Eq. (5), thus:
Finally, grey relational grade (γi) was calculated as:
Results and Discussion
Quantitative Analyses of Pore Structure
Nitrogen adsorption analysis is used widely to characterize pore distribution in coal. Figure 2 demonstrates that the adsorption lines vary between different coal and modified coal with different treatments. The hysteresis lines of samples belong to H3 type according to IUPAC, because of capillary condensation of slit-shaped mesopores (Thommes 2010). Isotherm hysteresis still occurred at low relative pressures indicating the existence of intercalation, a solid swelling because of layered structures in materials (Cai et al. 2013; Xu et al. 2018a). The low-rank coals have more obvious adsorption hysteresis effect compared with high-rank anthracite (WYM), indicating that mesopores collapse during coalification. Similar results can be found between raw coal and modified coal after heat treatment of SM and XJ. Coalification has some similarity with heat treatment, especially the heat treatment under low temperature for a longtime (Landais 1991; Behar and Hatcher 1995). Generally, diagenesis has transformed organic matter at higher thermal maturity, generating more microporosity and reducing heterogeneity of pore surface (Levy et al. 1997). This process often occurred in high-rank coal with high adsorption capacity (Bustin and Clarkson 1998). Therefore, the SM, XJ raw coals and modified coals can be regarded as a series of coals with varied coalification degrees. Moreover, it reduces the influence of inorganic matter when comparing the influence of pore characterization on methane adsorption.
The pore parameters estimated with N2 adsorption are listed in Table 2. Sample SM-400-80 has the smallest average pore size but has the largest BET surface area. Sample XJ has the largest average pore size and the largest BJH mesopores volume. The results indicate that pores with smaller size contribute more to surface area, while those with larger size dominate over pore volume (Wang et al. 2016).
Density functional theory (DFT) and molecular simulation can be adopted to analyze accurately the pore size distribution (PSD) over the complete micropore–mesopore size range within a single method (Thommes 2010). The DFT-PSDs of all samples are shown in Figure 3, which can be divided into four categories according to their distinctions. Category I has the most intensive peak below 2 nm and dispersive peaks above 2 nm, including XJ-400-40, SM-400-40 and SM-400-80. Category II has intensity peak below 2 nm and intensive peaks in the range above 2 nm, including SX and SM. Categories III and IV have little or no peak below 2 nm. Category III has dispersive peaks above 2 nm, including WYM, XJ-400-80, SM-300-40 and SM-300-80, while category IV has intensive peaks above 2 nm, including HN, HLJ and XJ. These pore size distributions in different categories influenced the fractal analysis of samples as discussed below.
It is hard to analyze ultrafine pores with nitrogen due to its low diffusion rate under low temperature. However, CO2 is recognized as a good alternative, primarily because of higher operating temperatures (usually 0 °C) (De Jonge and Mittelmeijer-Hazeleger 1996). Figure 4 shows the CO2 adsorption isotherms. It can be confirmed that all samples are microporous materials owning to their Type I isotherms.
Both CO2-DFT pore volume and surface area are listed in Table 2. The DFT-PSDs of 12 samples show their major peaks ranging from 0.35 to 1 nm (Fig. 5). There were no pores above 1 nm because of the high test temperature (0 °C). The higher the temperature is, the larger the fugacity of CO2 molecule gets, and the higher the adsorption equilibrium pressure becomes. However, the maximum analysis pressure was standard atmospheric pressure. In this condition, CO2 can only be used to analyze pores less than 1 nm.
Fractal geometry is a powerful method for the quantitative study of pore structure and surface irregularity that directly affects pore adsorption and diffusion behavior. The FHH model had the high universality of many rock types, including coals. All FHH plots are displayed in Figure 6. Each picture had two obvious straight fitting-lines in the P/P0 ranges below and above 0.5. The coefficients of determination of all fitting-lines were higher than 0.92 (Table 3). The results indicate that there are two different adsorption mechanisms of the tested coal samples.
Methane Adsorption Capacity
Figure 7 displays the isotherms of excess methane adsorption measured by the volumetric method. Based on IUPAC classification, all the isotherms belong to Type I (Fig. 7), indicating that the Langmuir adsorption mode is suitable to analyze them quantitatively. All calculated results are shown in Table 2. The adsorption capacities of the samples were in the ranges of 11.27–27.06 and 21.36–39.26 ml/g, respectively.
Influence of Fractal Dimensions on Methane Adsorption
Methane adsorption character varies with not only temperature and pressure but also the physical properties of adsorbent (Yang and Saunders 1985). Among several physical properties, few attempts have been made on the effects of the fractal characteristics of coal pores on methane adsorption (Liu and Nie 2016). Each sample had two fractal dimensions, D1 and D2, which had different impacts on methane adsorption.
D1 was calculated using the data with P/P0 of ≤ 0.5. The van der Waals forces between adsorbate and surface of adsorbent dominate the adsorption process, resulting in monolayer adsorption on the surface. Consequently, D1 reflects the surface roughness of the pore structure. D2 was calculated using the data with P/P0 of > 0.5. The adsorption mechanism transits from monolayer adsorption with P/P0 of ≤ 0.5 to multidimensional and pore-filling adsorption with P/P0 of > 0.5. Therefore, D2 can be used to define the irregularity of pore structure (Yao et al. 2008; Sun et al. 2015). It is interesting to find that samples with N2-PSD of category I (XJ-400-40, SM-400-40 and SM-400-80) have larger D1 than the others. It could be comprehended that the surface of material with micropore and disorder mesopores is rougher than that with uniform pores.
The two fractal dimensions, D1 and D2, have significantly different effects on VL and PL of samples (Fig. 8). VL has a positive liner relationship with D1 because rougher surface adsorbents with higher values of D1 have more active sites for methane adsorption (Wang et al. 2016). However, similar to previous reports (Cai et al. 2013; Wang et al. 2016), there is no obvious relationship between D2 and VL, or between D1/D2 and PL. It is deduced that adsorbents with higher D1 have more micropores and more irregular and rougher coal surfaces, which can offer more sites for methane adsorption, resulting in their higher VL values.
Influence of Pore Structures on Methane Adsorption
The adsorption capacity of coal samples is associated closely with micro-/mesopore characteristics. Therefore, it is of great significance to analyze the full range micro-/mesopore size distribution (0.3–50 nm). We quantified the full range micro-/mesopore (0.3–50 nm) by combining the N2/CO2 adsorption results (Figs. 3 and 5).
Figure 9 shows the relationship of pore structures and methane adsorption. Methane adsorption capacity is positively related to pore volume and surface area of pores with pore diameter less than 2 nm (0.3–1 nm from CO2 data, 1–2 nm from N2 data). However, in correspondence with previous results (Liu and He 2017), mesopore (2–50 nm) did not significantly influence methane adsorption (Fig. 9a, b and e). A linear relation can be found between BET surface area and VL mainly because the former is dominated by micropore (Thommes 2010).
PL shows a linear increase with the increase in average mesopores size (Fig. 10a). The reason for this phenomenon might be that the interaction energy between adsorbent and adsorbate in the center of pore decreases with rising pore size (Thommes 2010). Thus, the larger the pore size is, the larger the fugacity of methane molecule gets; consequently, the higher the adsorption equilibrium pressure becomes.
Grey Relational Analysis of Influence Factors
As discussed above, methane adsorption is a complex process influenced by several factors such as the fractal dimension D1, micropore volume, micropore surface area, N2 BET surface area, ultra-micropore volume and ultra-micropore surface area. In order to analyze the influence degree of different factors on adsorption performance, the GRA method was adopted. Based on the GRA method and the above experimental data, the reference and comparison sequences were first constructed as follows.
The reference sequence was:
The reference sequence after standardized treatment was:
The comparison sequence was:
The comparison sequence after standardized treatment was:
The multidimensional grey relational matrix U was calculated by the matrix Rn, thus:
Finally, from the coefficient matrix [U], the grey relational grades between coal structure parameters and the methane adsorption capacity were calculated, thus: γ1 = 0.9218 (D1), γ2 = 0.7994 (N2 BET surfaces area), γ3 = 0.5446 (micropore surface area), γ4 = 0.5486 (micropore volume), γ5 = 0.9261 (ultra-micropore surface area) and γ6 = 0.9312 (ultra-micropore volume). In conclusion, the order of influence degree of coal structure parameters on methane adsorption capacity was γ6 > γ5 > γ1 > γ2 > γ4 > γ3.
In the GRA, grey relational grade (γi) is correlated to the performance of different factors in a complex process. The higher γi one factor achieves, the more important it performs in such a process (Xu et al. 2011). The six influence factors of the methane adsorption process are listed by their performances as follows: ultra-micropore volume > ultra-micropore surface area > D1 > N2 BET surfaces area > micropore volume > micropore surface area. Generally, the grey relational grade represents different influence degree of varied factors, with γi > 0.9, γi > 0.8, γi > 0.7, γi < 0.6 representing marked influence, relatively marked influence, noticeable influence, and negligible influence, respectively. Ultra-micropore has stronger influence on methane adsorption capacity than micropore (Shen et al. 2015). Besides, ultra-micropore contains a large proportion of micropores whose pore size is believed to be the optimum dimension for methane adsorption, around 0.8 nm (Matranga et al. 1992). The grey relational grade of the pore volume is always higher than that of surface area, not only for micropores but also for ultra-micropores. Because of high-pressure adsorption, there was a solid swelling phenomenon in the coal sample, which increases the methane adsorption capacity of the sample. This phenomenon was more closely related to the pore volume than surface area. Therefore, compared with surface area, pore volume is a more important factor in gas sorption of coal, which is consistent with previous studies (Mastalerz et al. 2004; Clarkson et al. 2013; Hao et al. 2013).
Conclusions
The pore structure of all samples was characterized by N2/CO2 adsorption, and their high-pressure methane adsorption capacity was measured. By means of linear fitting, several coal structure parameters were found to influence methane adsorption capacity. Furthermore, the influence degree afforded by different structure parameters was evaluated by GRA method. The major conclusions of this study are as follows:
-
(1)
A full range micro-/mesopore size distribution was characterized by combining CO2 and N2 adsorption (0.3–1 nm by CO2 adsorption and 1–50 nm by N2 adsorption). Comprehensively analyzed from the pore structure and methane adsorption data, it could be found that both surface area and volume of pore with its width below 2 nm had significant influence on Langmuir volume (VL), while average mesopore size is closely related to Langmuir pressure (PL).
-
(2)
Four categories PSDs were observed for all the samples. Category I, which had most intensive peak during 1–2 nm and dispersive peaks during 2–50 nm, had obviously larger D1 than the other samples.
-
(3)
Based on the N2 adsorption data, two different fractal dimensions, D1 and D2, were obtained. D1 ranged from 2.059 to 2.808, and D2 ranged from 2.649 to 2.852. The higher pore surface fractal dimension (D1) represented rougher surface, on which more active adsorption sites were available for methane, whereas D2 did not influence the gas storage capacity.
-
(4)
The grey relational grades of six factors (fractal dimension D1, micropore volume, micropore surface area, N2 BET surface area, ultra-micropore volume and ultra-micropore surface area) were 0.8862, 0.5035, 0.5006, 0.7915, 0.9085 and 0.8976, respectively. Therefore, the influence of the six factors were ranked by the importance from the most to the least as ultra-micropore volume, ultra-micropore surface area, fractal dimension D1, N2 BET surface area, micropore volume and micropore surface area. This study showed that GRA is a promising statistical method that can be used successfully for comparing influence of different pore parameters on methane adsorption.
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Acknowledgments
The study was financially supported by National Science and Technology Major Project of China (2016ZX05040-003). We thank Doctor Nie Fan for his linguistic assistance during the revise of this manuscript.
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Xu, S., Hu, E., Li, X. et al. Quantitative Analysis of Pore Structure and Its Impact on Methane Adsorption Capacity of Coal. Nat Resour Res 30, 605–620 (2021). https://doi.org/10.1007/s11053-020-09723-2
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DOI: https://doi.org/10.1007/s11053-020-09723-2