2003
DOI: 10.1016/s0016-2361(03)00010-3
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A bidisperse pore diffusion model for methane displacement desorption in coal by CO2 injection☆

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Cited by 244 publications
(139 citation statements)
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“…To interpret and quantify the observed gas uptake rates in coal two models have been used: unipore model, based on the solution to Fick's second law for spherical symmetric flow [18][19][20][21][22] and bidisperse sorption/diffusion gas transport model for coals characterized by two distinct pore systems [18,20,[23][24][25][26][27][28]. It is generally confirmed that the amount micropores increase and mesopores decrease with coal rank.…”
Section: Introductionmentioning
confidence: 99%
“…To interpret and quantify the observed gas uptake rates in coal two models have been used: unipore model, based on the solution to Fick's second law for spherical symmetric flow [18][19][20][21][22] and bidisperse sorption/diffusion gas transport model for coals characterized by two distinct pore systems [18,20,[23][24][25][26][27][28]. It is generally confirmed that the amount micropores increase and mesopores decrease with coal rank.…”
Section: Introductionmentioning
confidence: 99%
“…Gas in coal cleat system is stored in free and absorbed states and gas circulation is accomplished through the laminar process. In the last one, and taking into account the gas concentration and the location, gas circulates into a specific direction depending on the pressure gradient and on the fluid properties (Kolesar and Ertekin, 1986;Shi and Durucan, 2003). In contrast, the gas stored in coal pores is in the adsorbed state and diffusion is the dominant gas circulation process.…”
Section: Introductionmentioning
confidence: 99%
“…In the diffusion process, the gas flow depends on three main related parameters: (1) the pressure variation effect, which induces distinct behaviours in the different components present on the gas mixture; (2) the interactions that these gas components establish with the coal porous structure, and, consequently; (3) the coal porous structure shrinking and swelling effects. Several models have been and are being used to describe gas circulation in coal seams, such as those presented by Brouers et al (2005), Cui et al (2004 b), Mavor et al (1990), Mehrer (2007), Pruess (2006), Ruckenstein et al (1971), Saghafi et al (2007), and Shi and Durucan (2003). In fact, two different models are being adopted to study the gas circulation in coal seams: one is the unipore diffusion model (Crank, 1975), which is mainly concerned in studying the gas circulation in coal porous structure, i.e.…”
Section: Introductionmentioning
confidence: 99%
“…A variety of models have been developed to describe gas diffusion between matrix and cleats, which include the equilibrium model with instantaneous diffusion, non-equilibrium model with pseudo-steady-state or unsteady-state diffusion governed by Fick's Law [11], and the bidisperse diffusion model [12]. Flow through the natural fractures can typically be represented by dual-porosity single-permeability model (without the presence of large-scale fractures) or triple-porosity dual-permeability model.…”
Section: Introductionmentioning
confidence: 99%