| HOME | HELP | FEEDBACK | SUBSCRIPTIONS | ARCHIVE | SEARCH | TABLE OF CONTENTS |
|
|
|
|||||||
|
|||||||||
a USDA-ARS Hydrology Lab., Bldg. 007, Rm.104 BARC-WEST, Beltsville, MD 20705 USA
b Desert Research Institute, 2215 Raggio Parkway, Reno, NV 89512-1095 USA
ypachepsky{at}hydrolab.arsusda.gov
Solute dispersivity defined from the classical advective–dispersive equation (ADE) was found to increase as the length of a soil column or the soil depth increased. The heterogeneity of soil is a physical reason for this scale dependence. Such transport can be described assuming that the random movement of solute particles belongs to the family of so-called Lévy motions. Recently a differential solute transport equation was derived for Lévy motions using fractional derivatives to describe advective dispersion. Our objective was to test applicability of the fractional ADE, or FADE, to solute transport in soils and to compare results of FADE and ADE applications. The one-dimensional FADE with symmetrical dispersion included two parameters: the fractional dispersion coefficient and the order of fractional differentiation 
, 0 < 
2. The FADE reduces to the ADE when the parameter
. Analytical solutions of the FADE and the ADE were fitted to the data from experiments on Cl- transport in sand, in structured clay soil, and in columns made of soil aggregates. The FADE simulated scale effects and tails on the breakthrough curves (BTCs) better than, or as well as, the ADE. The fractional dispersion coefficient did not depend on the distance. In the clay soil column, the parameter did not change significantly when the flow rate changed provided the degree of saturation changed only slightly. With the FADE, the scale effects are reflected by the order of the fractional derivative, and the fractional dispersion coefficient needs to be found at only one scale.
Abbreviations: ADE, advective–dispersive equation • BTC, breakthrough curve • CTRW, continuous time random walks • FADE, fractional advective–dispersive equation • FPE, Fokker-Planck equation • MIM, mobile–immobile model
This article has been cited by other articles:
|
|
 |
|
  F. S. J. Martinez, Y. A. Pachepsky, and W. J. Rawls Advective-Dispersive Equation with Spatial Fractional Derivatives Evaluated with Tracer Transport Data Vadose Zone J., March 5, 2009; 8(1): 242 - 249. [Abstract] [Full Text] [PDF]
|
|
|
|
|
|
L. Bolshov, P. Kondratenko, K. Pruess, and V. Semenov Nonclassical Transport Processes in Geologic Media: Review of Field and Laboratory Observations and Basic Physical Concepts Vadose Zone J., November 1, 2008; 7(4): 1181 - 1190. [Abstract] [Full Text] [PDF]
|
|
|
|
|
|
J. Vanderborght and H. Vereecken One-Dimensional Modeling of Transport in Soils with Depth-Dependent Dispersion, Sorption and Decay Vadose Zone J., January 24, 2007; 6(1): 140 - 148. [Abstract] [Full Text] [PDF]
|
|
|
|
 |
|
 A. Cortis and B. Berkowitz Anomalous Transport in "Classical" Soil and Sand Columns Soil Sci. Soc. Am. J., September 1, 2004; 68(5): 1539 - 1548. [Abstract] [Full Text] [PDF]
|
|
|
|
|
|
L. Zhou and H. M. Selim Application of the Fractional Advection-Dispersion Equation in Porous Media Soil Sci. Soc. Am. J., July 1, 2003; 67(4): 1079 - 1084. [Abstract] [Full Text] [PDF]
|
|
| HOME | HELP | FEEDBACK | SUBSCRIPTIONS | ARCHIVE | SEARCH | TABLE OF CONTENTS |
| The SCI Journals | Agronomy Journal | Crop Science | |||
| Journal of Natural Resources and Life Sciences Education |
Vadose Zone Journal | ||||
| Journal of Plant Registrations | Journal of Environmental Quality |
The Plant Genome | |||
