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Title: EVALUATING THE FRACTIONAL CONVECTIVE-DISPERSIVE EQUATION AS A SOLUTE TRANSPORT MODEL WITH DATA FROM MISCIBLE DISPLACEMENT EXPERIMENTS

Author
item SAN JOSE MARTINEZ, FERNANDO - U. OF MADRID, SPAIN
item Pachepsky, Yakov
item Rawls, Walter

Submitted to: ASA-CSSA-SSSA Annual Meeting Abstracts
Publication Type: Abstract Only
Publication Acceptance Date: 5/8/2006
Publication Date: 11/12/2006
Citation: San Jose Martinez, F., Pachepsky, Y.A., Rawls, W.J. 2006. Evaluating the fractional convective-dispersive equation as a solute transport model with data from miscible displacement experiments [abstract]. ASA-CSSA-SSSA International Meeting. 2006 CDROM.

Interpretive Summary:

Technical Abstract: Solute transport in soils and sediments is commonly simulated with the parabolic advective-dispersive equation, or ADE, that can be derived assuming solute particles undergo Brownian motion. Recently, a new model was proposed that assumes that the movement of solute particles belongs to the family of Lévy motions. A one-dimensional solute transport equation was derived for Lévy motions using fractional derivatives to describe the dispersion. Our objective was to test applicability of this fractional ADE, or FADE, to soils. We evaluated the FADE as the transport model in comparison with ADE with data from published miscible displacement experiments. The FADE, as a general model that included ADE, accurately simulated experimental breakthrough curves. Of the 53 experiments considered, 28 were fitted better with Levy parameter smaller than two, i.e. with the fractional model, and 25 have been best fitted with the Levy parameter equal to two, i.e. the classical ADE model. This suggested that FADE rather than ADE could be used as a general framework to study solute transport in soil. The Levy parameter varied with solute transport experimental conditions, i.e. type of soil, type of tracer, flow velocity and saturation degree. These differences presumably reflected different degrees of complexity in the movement of solute particles in soil that might be caused by the differences in the hierarchical structure of soil pore space for each particular case. Trends of the increase in the Levy parameter values with the increase in saturation and in flow velocity were been observed. The fractional advective-dispersive equation as a generalization of classical advective-dispersive equation is a promising enhancement in the soil hydrologist toolbox.