4.7 Article

Discrete Dilatant Pathway Modeling of Gas Migration Through Compacted Bentonite Clay

出版社

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.ijrmms.2020.104569

关键词

Gas; Flow; Bentonite; Modeling; Dilatant; Stress; Pressure

资金

  1. Andra
  2. BGR/UFZ
  3. CNSC
  4. US DOE
  5. ENSI
  6. JAEA
  7. IRSN
  8. KAERI
  9. NWMO
  10. RWM
  11. SURAO
  12. SSM
  13. Taipower
  14. Spent Fuel and Waste Science and Technology Campaign, Office of Nuclear Energy, of the U.S. Department of Energy [DE-AC02-05CH11231]
  15. Lawrence Berkeley National Laboratory
  16. NERC [bgs06001] Funding Source: UKRI

向作者/读者索取更多资源

By applying a coupled multiphase fluid flow and discrete fracturing model, this study simulated gas migration experiments on compacted bentonite. Calibration of model parameters and the establishment of a best-fit conceptual model were necessary to achieve a good match with the experimental results.
A coupled multiphase fluid flow and discrete fracturing model is applied to simulate bench-scale gas migration experiments on compacted bentonite. The numerical modeling is based on the linking of the multiphase fluid flow simulator TOUGH2 with a Rigid-Body-Spring Network model, which enables a discrete (lattice) representation of elasticity and individual fractures. The evolution of a complex network of dilatant flow paths is modeled through opening and breakage of lattice interface bonds between porous-elastic matrix elements. To achieve a good match with the experimental results, including an abrupt gas breakthrough along with pressure and stress responses, it was necessary to calibrate model parameters for (1) air-entry pressure, (2) shear and tensile failure of lattice interface bonds, (3) moisture swelling/shrinkage effects on stress, and (4) aperture-dependent permeability of dilatant flow paths. Our best-fit conceptual model considers a pervasive network of discrete flow paths propagating from the gas injection point, whereas some of the experimental data indicate the potential for heterogeneous and unstable flow paths.

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