Published online 13 May 2005
Published in Vadose Zone J 4:310-316 (2005)
DOI: 10.2136/vzj2004.0090
© 2005 Soil Science Society of America
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Simulation of Tracer Dispersion in Porous Media Using Lattice Boltzmann and Random Walk Models
Francisco J. Jiménez-Horneroa,*,
Juan V. Giráldezb and
Ana Lagunac
a Dep. of Agronomy, University of Córdoba, P.O. Box 3048, 14080 Córdoba, Spain
b Dep. of Agronomy, University of Córdoba and Institute of Sustainable Agriculture, CSIC, P.O. Box 3048, 14080 Córdoba, Spain
c Dep. of Applied Physics, University of Córdoba, P.O. Box 3048, 14080 Córdoba, Spain

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Fig. 1. Neighborhood relationships used in the BGK model for the description of advection (d2q9), and diffusion (d2q4), where d is the dimension number and q the number of adopted neighbors.
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Fig. 2. Dispersion of a passive tracer in a medium with porosity = 0.76, simulated with the BGK model. The flow was forced from left to right with the parameters Re = 39.7 and Pe = 110.2. The dark and white hues correspond to regions with higher and lower tracer concentration, respectively. The concentration values are normalized with respect to their initial value. The numbers in the figure corresponds to the computed time steps.
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Fig. 3. Dispersion of a passive tracer in a medium with porosity = 0.76, simulated with the BGK/RW model. The flow was forced from left to right with the parameters Re = 39.7 and Pe = 110.2. The dark and white hues correspond to regions with higher and lower tracer concentration, respectively. The concentration values are normalized with respect to their initial value. The numbers in the figure corresponds to the computed time steps.
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Fig. 4. Breakthrough curves computed with BGK (full line) and the BGK/RW models (dashed line) for simulating the dispersion of a passive tracer in a medium with porosity = 0.76 using the parameters Re = 39.7 and Pe = 110.2.
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Fig. 6. Breakthrough curve computed with the BGK model (solid line), for TaylorAris dispersion of a passive tracer during flow with the Re = Pe = 4.8, and comparison with the theoretical solution (dashed line).
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Fig. 7. Breakthrough curve computed with the BGK/RW model (solid line), for TaylorAris dispersion of a passive tracer during flow with the Re = Pe = 4.8, and comparison with the theoretical solution (dashed line).
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Copyright © 2005 by the Soil Science Society of America.