解吸
扩散
甲烷
煤
体积热力学
煤层气
化学
气体扩散
热力学
矿物学
煤矿开采
吸附
物理化学
物理
有机化学
电极
作者
Douglas M. Smith,Frank Williams
出处
期刊:Fuel
[Elsevier]
日期:1984-02-01
卷期号:63 (2): 251-255
被引量:104
标识
DOI:10.1016/0016-2361(84)90046-2
摘要
Experimental studies of methane diffusion from coal cuttings have been analysed with both a unipore diffusion model and a bi-disperse pore structure diffusion model to determine the time range of each model's validity. Initial desorption, during the first 50% of volume desorbed, can be adequately described by the unipore model. For Fruitland coals of the San Juan Basin, the unipore diffusion coefficient varied by less than a factor of 2 from a value of 1 × 10−5s−1 despite large variations in sample depth and location. The unipore diffusion model has been successfully incorporated into a lost-gas-correction-factor determination as part of a new technique to delineate coal-bed methane. To describe methane diffusion over the full timescale of desorption, a more complex model which more accurately represents the observed bi-disperse pore structure of coal is required. Using that model the observed desorption rate is described over all the desorption. This model is especially applicable as a source term in describing overall well production.
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