4.7 Article

Shale Gas Transport in Nanopores: Contribution of Different Transport Mechanisms and Influencing Factors

Journal

ENERGY & FUELS
Volume 35, Issue 3, Pages 2033-2047

Publisher

AMER CHEMICAL SOC
DOI: 10.1021/acs.energyfuels.0c03463

Keywords

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Funding

  1. National Natural Science Foundation of China (Key Program) [51534006]
  2. National Natural Science Foundation of China [51874251, 52074235]
  3. Science and Technology Cooperation Project of the CNPC-SWPU Innovation Alliance [2020CX020202, 2020CX030202, 2020CX010403]
  4. China Postdoctoral Science Foundation [2020M673287]
  5. 111 Project [D18016]

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In this study, the dimensionless relaxation time expression was modified and the Peng-Robinson equation of state (P-R EOS) was introduced to the microscale gas flow lattice Boltzmann model. Various transport mechanisms for shale gas flow in nanopores were considered, and the contributions of different factors to the total gas flow rate were studied. The results indicated that different transport mechanisms have varying influences on shale gas flow in nanopores under different conditions.
The classical Darcy's law cannot effectively describe the microscopic flow rules of shale gas. In addition, conducting gas transport experiments in nanopores is difficult, and the correctness of the simulation results is not guaranteed. Studies on the flow and transmission of shale gas in microscopic nanopores can effectively guide the macroscopic numerical simulation of shale gas reservoirs, which is of great significance to the economical and efficient development of such reservoirs. In this work, the dimensionless relaxation time expression is modified, and the Peng-Robinson equation of state (P-R EOS) is introduced to the microscale gas flow lattice Boltzmann model. The influences of viscous flow, slippage effect, boundary Knudsen layer, adsorbed gas layer, and surface diffusion are considered, and the results are combined with the real isothermal adsorption experimental data of shale samples collected from the Longmaxi formation in Sichuan Basin. Finally, the contributions of various transport mechanisms to shale gas flow in nanopores and their influencing factors are studied. Results show that the gas velocity and mass flux (Q) obtained using the ideal gas EOS are higher than those obtained using P-R EOS under high pressure. When the effective pore diameter (H-e) is less than 5 nm, surface diffusion and its induced free flow are the main transport mechanisms of shale gas flow in nanopores. Viscous flow becomes the main transport mechanism when H-e exceeds 20 nm. H-e, pressure, and shale adsorption capacity significantly affect the contribution rate of each transport mechanism to the total Q of shale gas. By comparison, the influence of temperature on the Q of shale gas is relatively small and can be neglected under high pressure.

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