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Dispersion variance for transport in heterogeneous porous media
Author(s) -
Dentz Marco,
Barros Felipe P. J.
Publication year - 2013
Publication title -
water resources research
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.863
H-Index - 217
eISSN - 1944-7973
pISSN - 0043-1397
DOI - 10.1002/wrcr.20288
Subject(s) - dispersion (optics) , statistical physics , porous medium , perturbation (astronomy) , random field , stochastic process , mathematics , physics , statistics , materials science , optics , porosity , quantum mechanics , composite material
We study dispersion in heterogeneous porous media for solutes evolving from point‐like and extended source distributions in d = 2 and d = 3 spatial dimensions. The impact of heterogeneity on the dispersion behavior is captured by a stochastic modeling approach that represents the spatially fluctuating flow velocity as a spatial random field. We focus here on the sample‐to‐sample fluctuations of the dispersion coefficients about their ensemble mean. For finite source sizes, the definition of dispersion coefficients in single realizations is not unique. We consider dispersion measures that describe the extension of the solute distribution, as well as dispersion coefficients that quantify the solute spreading relative to injection points of the partial plumes that constitute the solute distribution. While the ensemble averages of these dispersion quantities may be identical, their fluctuation behavior is found to be different. Using a perturbation approach in the fluctuations of the random flow field, we derive explicit expressions for the temporal evolution of the variances of the dispersion coefficients between realizations. Their evolution is governed by the typical dispersion time over the characteristic heterogeneity scale and the dimensions of the source distribution. We find that the dispersion variance decreases toward zero with time in d = 3 spatial dimensions, while in d = 2 it converges toward a finite long time value that is independent of the source dimensions.