Review Article

Study on Competitive Adsorption and Displacing Properties of CO2 Enhanced Shale Gas Recovery: Advances and Challenges

Table 3

Characteristics of various flow regime under different Knudsen number [111].

Flow regime rangea,bModelsComments

Continuum flowDarcy’s equation for laminar flow and Forchheimer’s equation for turbulent flowAssumes immobile fluid at the pore wall, and no permeability correction is generally required.
Slip flowDarcy’s equation with Klinkenberg’s correction or Knudsen’s correctionKlinkenberg’s correction is generally implemented due to its easiness, and Knudsen’s correction is more accurate.
Transition flowDarcy’s law with Knudsen’s correction can be applied. Alternative method is Burnett’s equation with slip boundary conditioncKnudsen’s diffusion equation is a more reliable approach, especially when is closer to 10.
Free molecular flowKnudsen’s diffusion equationd, alternative methods are DSMC and lattice BoltzmanncUsually occurs in shale formations where the pore throat radius is very small.

aThis Knudsen number classification is taken from Karniadakis et al. [112]. bSome reference suggests () as a cut off for continuum flow [109]. cFor more details, see Agarwal et al. [113]. dKnudsen’s diffusion can coexist with bulk and surface diffusion.