Open AccessComposition, Origin, and Accumulation Model of Coalbed Methane in the Panxie Coal Mining Area, Anhui Province, China
Author(s) -
Qiang Wei,
Baolin Hu,
Huihuang Fang,
Song Chen,
Shouhua Feng,
Cancan Wu,
Chunshan Zheng
Publication year - 2022
Publication title -
acs omega
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.779
H-Index - 40
ISSN - 2470-1343
DOI - 10.1021/acsomega.2c01227
Subject(s) - coalbed methane , methane , fractionation , coal , coal mining , environmental science , propane , geology , environmental chemistry , mineralogy , dissolution , chemistry , chromatography , organic chemistry
To investigate the geochemical characteristic, genetic types, and accumulation model of coalbed methane (CBM), 16 samples from a burial depth of 621-1494 m were collected in the Panxie Coal Mining Area of Huainan Coalfield. The results indicate that the samples are dominated by methane, and the concentrations are distributed in the range of 73.11-95.42%. The dryness coefficient is 0.77-1.00 (average, 0.93), and the ratio of methane to the sum of ethane and propane (C 1 /(C 2 + C 3 )) is 3.18-242.64 (average, 36.15). The δ 13 C CH 4 values are distributed in the range of -65.44 to -32.38‰ (average, -45.22‰), the δD CH 4 values are in the range of -226.84 to -156.82‰ (average, -182.93‰), and the δ 13 C CO 2 values are in the range of -19.7 to -10.1‰ (average, -15.51‰). CBM samples in the study area are dominated by thermogenic gases, followed by secondary biogenic gases with CO 2 reduction. For the percentages of different genetic gases, the distribution range of thermogenic gas is 70.11-97.86%, whereas that of biogenic gas is 58.65-77.86% for five samples from Zhangji, Panyi, Pansan, and Panbei Coalmines. Moreover, desorption-diffusion fractionation and the effect of groundwater dissolution occurred in the Panxie Coal Mining Area, and higher δ 13 C CH 4 values mostly existed in the deeper coal seams. Furthermore, the biogenic gases are more likely to be secondary biogenic gases generated by CO 2 reduction on the basis of data comparison, which is related to the flowing water underground. Accumulation models of different genetic types of CBM are correlated with the burial depth of coal seams, location, and type of faults and aquifers.