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,b
Models
Comments
Continuum flow
Darcy’s equation for laminar flow and Forchheimer’s equation for turbulent flow
Assumes immobile fluid at the pore wall, and no permeability correction is generally required.
Slip flow
Darcy’s equation with Klinkenberg’s correction or Knudsen’s correction
Klinkenberg’s correction is generally implemented due to its easiness, and Knudsen’s correction is more accurate.
Transition flow
Darcy’s law with Knudsen’s correction can be applied. Alternative method is Burnett’s equation with slip boundary conditionc
Knudsen’s diffusion equation is a more reliable approach, especially when is closer to 10.
Free molecular flow
Knudsen’s diffusion equationd, alternative methods are DSMC and lattice Boltzmannc
Usually 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.