Role of chemical structures in coalbed methane adsorption for anthracites and bituminous coals

被引:61
作者
Fu, Yongshuai [1 ,3 ]
Liu, Xianfeng [2 ]
Ge, Boqing [2 ]
Liu, Zhenghong [1 ]
机构
[1] Jilin Univ, Coll Earth Sci, Changchun 130061, Peoples R China
[2] China Univ Min & Technol Beijing, Sch Resources & Safety Engn, Beijing 10083, Peoples R China
[3] China Coal Res Inst, Shenyang Branch, Shenyang 110016, Peoples R China
来源
ADSORPTION-JOURNAL OF THE INTERNATIONAL ADSORPTION SOCIETY | 2017年 / 23卷 / 05期
关键词
Chemical structure; Coal; Coalbed methane; Adsorption capacity; STATE C-13 NMR; FRACTAL CHARACTERISTICS; RAMAN-SPECTROSCOPY; BAND ASSIGNMENTS; PORE STRUCTURE; CHAR FORMATION; FT-IR; SURFACE; TEMPERATURE; PYROLYSIS;
D O I
10.1007/s10450-017-9888-z
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
An in-depth investigation was conducted on four bituminous coals and three anthracites regarding the chemical structural characteristics using Fourier transform infrared spectroscopy (FTIR). The FTIR spectra of coals can be well approximated by the combination of Gaussian/Lorentzian peaks. FTIR parameters, including aromatic structures, aliphatic structures and oxygen-containing groups (C=O), were determined from curve-fitting analysis. Methane adsorption measurements were carried out through an equilibrium volumetric method, and the Langmuir equation was applied to fit the experimental data. Correlations were established for these FTIR structural parameters and methane adsorption parameters (V (L) and P (L)). From the results obtained, it can be seen that rapid changes occur for bituminous coals with the vitrinite reflectance, R (o) = 1.1-2.1%. The sharp variations of the apparent aromaticity, f (a), and A(CH2)/A(CH3) indicate the significant intensive aromatization and the decrease of aliphatic methylene groups, respectively. As a consequence, the size of aromatic clusters is greatly enhanced with increasing coalification. However, the oxygen-containing functional groups, A ' CA ', varying from 0.43 for sample WJD to 0.10 for sample ZZ, presents a negative linear relationship with R (o). Once R (o) > 2.1% (anthracite), both f (a) and A(CH2)/A(CH3) tend to be steady. The defects and degree of disorder in coal structure have been reduced to a large extent, and the graphite microcrystalline structure in coal is gradually perfected for anthracites. Coals with higher f (a) provide more adsorption sites for methane occupation on coal surface, thus demonstrating stronger adsorption capacities. However, the aliphatic methylene groups and oxygen-containing functional groups can decrease the CH4 adsorption amount at low pressure stage (< 5 MPa), further reducing the adsorption properties. These findings may have great significance for accurate estimation reserves of coalbed methane and the prevention of gas disasters underground coal mine.
引用
收藏
页码:711 / 721
页数:11
相关论文
共 64 条
[1]   Novel Simplification Approach for Large-Scale Structural Models of Coal: Three-Dimensional Molecules to Two-Dimensional Lattices. Part 1: Lattice Creation [J].
Alvarez, Yesica E. ;
Watson, Justin K. ;
Mathews, Jonathan P. .
ENERGY & FUELS, 2012, 26 (08) :4938-4945
[2]   The effect of small micropores on methane adsorption of coals from Northern China [J].
An, Feng-Hua ;
Cheng, Yuan-Ping ;
Wu, Dong-Mei ;
Wang, Liang .
ADSORPTION-JOURNAL OF THE INTERNATIONAL ADSORPTION SOCIETY, 2013, 19 (01) :83-90
[3]  
[Anonymous], 2016, GREENHOUSE GAS SCI T, DOI DOI 10.1186/s40164-016-005055
[4]   Structure of some western Anatolia coals investigated by FTIR, Raman, 13C solid state NMR spectroscopy and X-ray diffraction [J].
Baysal, Mustafa ;
Yurum, Alp ;
Yildiz, Burcin ;
Yurum, Yuda .
INTERNATIONAL JOURNAL OF COAL GEOLOGY, 2016, 163 :166-176
[5]   Instantaneous outbursts in underground coal mines: An overview and association with coal type [J].
Beamish, BB ;
Crosdale, PJ .
INTERNATIONAL JOURNAL OF COAL GEOLOGY, 1998, 35 (1-4) :27-55
[6]   Adsorption of carbon dioxide-methane mixtures in porous carbons: effect of surface chemistry [J].
Billemont, Pierre ;
Coasne, Benoit ;
De Weireld, Guy .
ADSORPTION-JOURNAL OF THE INTERNATIONAL ADSORPTION SOCIETY, 2014, 20 (2-3) :453-463
[7]   Characterization of chemical functional groups in macerals across different coal ranks via micro-FTIR spectroscopy [J].
Chen, Yanyan ;
Mastalerz, Maria ;
Schimmelmann, Arndt .
INTERNATIONAL JOURNAL OF COAL GEOLOGY, 2012, 104 :22-33
[8]   The effect of pore structure and gas pressure upon the transport properties of coal: a laboratory and modeling study. 1. Isotherms and pore volume distributions [J].
Clarkson, CR ;
Bustin, RM .
FUEL, 1999, 78 (11) :1333-1344
[9]   Variation of the coal chemical structure and determination of the char molecular size at the early stage of rapid pyrolysis [J].
Cui, Tongmin ;
Fan, Wenke ;
Dai, Zhenghua ;
Guo, Qinghua ;
Yu, Guangsuo ;
Wang, Fuchen .
APPLIED ENERGY, 2016, 179 :650-659
[10]   Agglomeration of low rank Indian coal fines with an organic binder and the thermal behavior of the agglomerate produced: Part I [J].
Das, Tonkeswar ;
Saikia, Binoy K. ;
Dutta, Dileep K. ;
Bordoloi, Dipok ;
Baruah, Bimala P. .
FUEL, 2015, 147 :269-278