Diffusive mixing and Tsallis entropy.

Daniel O'Malley1, Velimir V Vesselinov1, John H Cushman2

  • 1Computational Earth Science, Los Alamos National Laboratory, Los Alamos, New Mexico 87545, USA.

Summary

This study introduces a generalized Brownian motion that maximizes Tsallis q entropy, offering a new model for nonergodic systems. This approach accounts for random diffusion coefficients, with applications in porous media transport.

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