2015
DOI: 10.1016/j.coal.2015.05.010
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An analytical model for shale gas permeability

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Cited by 97 publications
(40 citation statements)
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“…When the pore pressure increases from 10 to 50 MPa, rv shows a minor increase from 0.832 to 0.967, and rk decreases smoothly from 0.168 to 0.033. This is because that, according to (11), with increasing pore pressure rv gradually converges to 1. Thus, at high pore pressure (>30 MPa), rv is not sensitive to pore pressure.…”
Section: Gas Transport Dynamics In Shalementioning
confidence: 96%
See 1 more Smart Citation
“…When the pore pressure increases from 10 to 50 MPa, rv shows a minor increase from 0.832 to 0.967, and rk decreases smoothly from 0.168 to 0.033. This is because that, according to (11), with increasing pore pressure rv gradually converges to 1. Thus, at high pore pressure (>30 MPa), rv is not sensitive to pore pressure.…”
Section: Gas Transport Dynamics In Shalementioning
confidence: 96%
“…Gas transport in shale involves different transport mechanisms, including viscous flow, slip flow, Knudsen diffusion, and surface diffusion [7][8][9]. A variety of studies have been done on studying these different mechanisms [10][11][12][13][14]. However, most of studies consider shale media as a bundle of uniform capillaries with an effective pore radius e .…”
Section: Introductionmentioning
confidence: 99%
“…Therefore, the Darcy law reflecting continuum flow is no longer applicable for shale gas due to the significant influence of molecular diffusion and gas slippage. To date, it has been generally accepted that gas flow regimes can be subdivided into continuum flow (K n < 0.001), slip flow (0.001 < K n < 0.1), transition flow (0.1 < K n < 10) and free molecular flow (K n > 10) based on the Knudsen number (K n , i.e., the ratio of the mean free path of molecule to pore diameter) Kim et al, 2015;Kazemi and Takbiri-Borujeni, 2015), as shown in Fig. 1.…”
Section: Introductionmentioning
confidence: 99%
“…Sigal (2013) thought the adsorbed layer diffusional transport may be the second mechanism for methane transport, but it requires large values of the diffusion coefficient. However, some literature treats the adsorbed phase as immobile, such as Cui et al (2009), Sakhaee-Pour andBryant (2012), and Kazemi and Ali (2015). Based on these arguments, one of the objectives of this work is to focus on evaluating the contribution of surface diffusion to the apparent permeability.…”
Section: Accepted Manuscriptmentioning
confidence: 98%