2007
DOI: 10.1016/j.coal.2006.04.006
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A theoretical model for gas adsorption-induced coal swelling

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Cited by 496 publications
(259 citation statements)
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“…Above 1.1 mmol·g coal -1 , the slope gradually decreases until flattening at ~1.7 mmol·g coal -1 . This effect is recognized by other authors, and is attributed to superposition of adsorption-induced and poroelastic strains (Hol and Spiers, 2012;Pan and Connell, 2007;Vandamme et al, 2010), where at higher CO 2 pressure (here: above ~4 MPa) poroelastic compression of the matrix significantly affects the measured swelling strains. Correcting the data of Day et al (2008) for poroelastic effects (following Hol and Spiers, 2012), yields a roughly linear trend that extends down to ~0.2 mmol·g coal -1 (Fig.…”
mentioning
confidence: 77%
“…Above 1.1 mmol·g coal -1 , the slope gradually decreases until flattening at ~1.7 mmol·g coal -1 . This effect is recognized by other authors, and is attributed to superposition of adsorption-induced and poroelastic strains (Hol and Spiers, 2012;Pan and Connell, 2007;Vandamme et al, 2010), where at higher CO 2 pressure (here: above ~4 MPa) poroelastic compression of the matrix significantly affects the measured swelling strains. Correcting the data of Day et al (2008) for poroelastic effects (following Hol and Spiers, 2012), yields a roughly linear trend that extends down to ~0.2 mmol·g coal -1 (Fig.…”
mentioning
confidence: 77%
“…The geometry of pores and porosity value are directly related to coal permeability (Reiss 1980;McKee et al 1987;Seidle and Huitt 1995). Gas adsorption/desorption is a well-known phenomenon that results in coal swelling/shrinkage and is regarded as a key factor for permeability behavior in coalbed methane recovery (Pan and Connell 2007;Pan et al 2010). Besides, coal permeability is also affected by other factors, such as different gases (Chen et al 2011;Siriwardane et al 2009), temperature (Hu et al 2010), and wettability (Han et al 2010).…”
mentioning
confidence: 99%
“…After a small drawdown, the mechanically induced stress change dominates since the gas desorption-induced strain is small at high pressure [Levine, 1996; (Figures 7b-7e) show the state of stress after the same pressure drawdown with different reservoir formation properties; the dashed semicircles illustrate the initial state of stress for reference. Pan and Connell, 2007;Harpalani, 2013a, 2013b]. Therefore, Mohr's circle moves to the right, as illustrated by the thin solid line in Figure 8.…”
Section: Coal Formation Stability Analysismentioning
confidence: 89%