• DOI:10.1007/s11004-020-09889-8
• Corpus ID: 221376836

Uncoupling Electrokinetic Flow Solutions

@article{Kuhlman2020UncouplingEF,
  title={Uncoupling Electrokinetic Flow Solutions},
  author={Kristopher L. Kuhlman and Bwalya Malama},
  journal={Mathematical Geosciences},
  year={2020},
  volume={53},
  pages={1293 - 1318}
}

• Kristopher L. Kuhlman, B. Malama
• Published 28 August 2020
• Physics
• Mathematical Geosciences

The continuum-scale electrokinetic porous-media flow and excess charge redistribution equations are uncoupled using eigenvalue decomposition. The uncoupling results in a pair of independent diffusion equations for “intermediate” potentials subject to modified material properties and boundary conditions. The fluid pressure and electrostatic potential are then found by recombining the solutions to the two intermediate uncoupled problems in a matrix-vector multiplication. Expressions for the material properties or source terms in the intermediate uncoupled problem may require extended precision or careful rewriting to avoid numerical cancellation, but the solutions themselves can typically be computed in double precision. The approach works with analytical or gridded numerical solutions and is illustrated through two examples. The solution for flow to a pumping well is manipulated to predict streaming potential and electroosmosis, and a periodic one-dimensional analytical solution is derived and used to predict electroosmosis and streaming potential in a laboratory flow cell subjected to low frequency alternating current and pressure excitation. The examples illustrate the utility of the eigenvalue decoupling approach, repurposing existing analytical solutions or numerical models and leveraging solutions that are simpler to derive for coupled physics.