Investigation of mechanism and kinetics of non-isothermal low temperature pyrolysis of perhydrous bituminous coal by in-situ FTIR
Introduction
Perhydrous coal is a type of coal that is enriched with hydrogen (4.6–5.6, wt.%) or has a higher atomic ratio of hydrogen and carbon (H/C) compared to other types of coal of similar rank [1]. The hydrogen enrichment gives rise to the modifications in the macromolecular structure of the coal, thus affecting the properties and behavior of the coal [2], [3], such as high calorific value [4], higher volatile matter content and enhancement of oil/tar potential [2]. Perhydrous coal was used as a good fuel source and applied in the field of hydrocarbon generation [5].
However, the complexity of coal composition and structure limits its utilization, and consumption of with large quantities of coal releases a high amount of pollutants such as SO2, CO2 and organic matter [6]. Thermal decomposition may be the initial step during the main processes of coal utilization including combustion and gasification [7]. Good understanding the mechanism of coal pyrolysis can help controlling the release of pollutants and enhance the conversion rate of coal, beneficial for clean and effective utilization of coal. Additionally, the decomposition reaction of can provide basic information concerning the structure of perhydrous coal molecules [8]. Furthermore, there is a similarity between the artificial pyrolysis and natural coalification, so that pyrolysis was often employed to study coalification process [9], [10].
In the past decades, many studies have addressed the pyrolysis of coal. General pyrolysis reactions and processes were established [11], [12], [13] and can be summarized as follows. At low temperature, some weak non-covalent bonds such as hydrogen bond are cracked and reduced. Compounds bonded by these weak bonds are slightly vaporized and released from solid coal. With rising temperature, bridge bonds begin to be cleaved, resulting in the formation of free radical groups and subsequent production of gas, tar and char. Finally, the solid residue undergoes further condensation reactions with the release of secondary gases (mainly CO and H2). Nevertheless, studies focusing on the detailed information about reactions and processes during pyrolysis have been limited, especially in the case of dynamic processes. Thermo gravity analysis (TGA) [14] was applied in investigation of the mechanism and kinetic characterization of coal pyrolysis. However, the results based on TGA are macroscopic and do not provide the information on the correlation between the coal structure and reactions. The coal pyrolysis model of Functional Group-Depolymerization Vaporization Crosslinking (FG-DVC) firstly proposed by Solomon established the correlation between coal structure and reactions and characterized the reaction of functional groups as the main processes of coal pyrolysis [12]. Nevertheless, this model is based on the evolution of the gas product by TGA-Fourier Transform Infrared Spectroscopy (TGA-FTIR) [15] and TGA-Mass Spectrum (TGA-MS) [16]. However, data obtained using these two characterization methods can not directly reflect the changes in solid coal during heating process, while in-situ transmission FTIR can determine the direct changes in the solid coal. Some reports on in-situ FTIR measurement have been published [17], [18], [19], [20]. Unlike ex-situ FTIR, the in-situ FTIR can reflect the online evolution of functional groups, and using ex-situ FTIR make the presence of secondary reactions inevitable during the coal processing [21], [22], [23], [24]. In addition, Qi et al. reported smoother and more precise curve of evolution of functional groups obtained by in-situ FTIR than that obtained by ex-situ FTIR during coal oxidation [25].
In coal structure, aliphatic groups (CH3, CH2, CH), aromatic groups (aromatic CC and CH), and oxygen-containing groups (hydroxyl, carbonyl, carboxyl and ether) are the most abundant functional groups that appear in the infrared spectrum and are strongly correlated with CO2, CO and tar [26]. Understanding of the evolution of these functional groups can help optimize thermal treatment of coal processes such as gasification and production of coke and tar.
For kinetic characterization of coal pyrolysis, several methods derived from TGA have been used for isothermal and non-isothermal conditions. These include the Ozawa [27] method and the integral method [28], [29]. However, with the exception of the work by Li et al., reports on the kinetic properties based on quantitative assessment of the functional groups are rare [30]. Li et al. investigated the decomposition kinetics of hydrogen bonds by the in-situ diffuse reflectance FT-IR (DRIFT) based on the loss of absorption of different types of hydrogen bonds.
In our previous works, the structural and thermal characterization of perhydrous coal was investigated by TGA-MS [16], [31], while in the present study in-situ FTIR was used to investigate the pyrolysis process of a perhydrous bituminous coal under non-isothermal heating condition. The spectra obtained at certain temperatures were deconvolved into peaks assigned to the corresponding functional groups. The main objectives of this study are (a) to investigate the pyrolysis mechanism of perhydrous bituminous coal based on the direct loss of functional groups in solid coal; (b) to establish a kinetic method for evolution of functional groups; (c) to determine kinetic characterization of evolution of functional groups during pyrolysis. The result of this study is expected to provide a useful basis for the optimization of coal treatment.
Section snippets
Coal sample
The coal sample (DJ coal) was collected from No. 13 coal seam at Dingji mine, Huainan coalfield, China, which is one of the main mined seams in the Huainan coalfield. The ultimate and proximate analysis results are shown in Table 1. The coal from this seam is classified as high volatile perhydrous bituminous coal and contributes 8% and 9% for the coking and power generation in China, respectively [16]. The sample was ground to <0.096 mm (−160 mesh) before used.
In-situ transmission FTIR
The in-situ transmission FTIR device
Result and discussion
The FTIR spectra of coal at different temperatures, shown in Fig. A.2, can only reflect obscure information about the changes of functional groups during pyrolysis. Hence, the difference spectrum was used to describe the process more clearly. 24 FTIR difference spectra were obtained for the coal by subtracting the spectrum at the neighboring temperature points (high temperature subtracting low temperature) with the subtracting factor of 1.0, as shown in Fig. 2(a)–(c). These difference spectra
Conclusions
To gain a better understanding of the mechanism and kinetic characterization of pyrolysis of perhydrous bituminous coal, in-situ transmission FTIR was used to investigate the evolution of the main functional groups in coal structure during pyrolysis at a heating rate of 10 °C/min below 500 °C under N2 flow. Two main conclusions were obtained.
Acknowledgement
This work was supported by National Basic Research Program of China (973 Program, 2014CB238903), National Natural Science Foundation of China (No. 41173032 and 41373110). The authors also thank the technical support from Instruments Center for Physical Science, USTC, China, for assistance with FTIR spectroscopy measurement.
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