期刊
ENERGY & FUELS
卷 28, 期 6, 页码 3673-3678出版社
AMER CHEMICAL SOC
DOI: 10.1021/ef5004123
关键词
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资金
- National Major Research Program for Science and Technology of China [2011ZX05034-001]
- National Natural Science Foundation of China [U1262104]
- Foundation for the Author of National Excellent Doctoral Dissertation of People's Republic of China [201253]
- Program for New Century Excellent Talents in University [NCET-11-0721]
- Beijing Higher Education Young Elite Teacher Project [YETP0660]
Coal matrix compressibility caused by a pressure change is an important parameter in evaluating the permeability change during coalbed methane production. In this study, the pressure-driven coal matrix compressibility for 21 coals in the rank range from high-volatile A bituminous (0.65% R-o,R-m) to low-volatile bituminous (1.77% R-o,R-m) was evaluated by combining the results from mercury intrusion porosimetry (MIP) with N-2 adsorption analysis. The pressure interval was chosen to be from 7.35 MPa to ensure that the compression is totally from the coal matrix. The calculated coal matrix compressibility shows a U-shaped relationship with increasing coal rank, and it obtains relatively low values at the medium-volatile bituminous coals. The coal matrix compressibility of high-volatile A bituminous coals is of 1.6398-2.9060 x 10(-4) MPa-1 and medium- and low-volatile bituminous coals have coal matrix compressibility of 0.3451-1.5519 x 10(-4) and 0.7625-2.5554 X 10(-4) MPa-1 respectively. Moreover, with the data of petrographic and proximate analyses, the porosity, moisture content, and macerals have influence on coal matrix compressibility.
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