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Hydrology and Earth System Sciences An interactive open-access journal of the European Geosciences Union
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Volume 10, issue 4 | Copyright
Hydrol. Earth Syst. Sci., 10, 495-506, 2006
https://doi.org/10.5194/hess-10-495-2006
© Author(s) 2006. This work is licensed under
the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 License.

  07 Jul 2006

07 Jul 2006

The dominant role of structure for solute transport in soil: experimental evidence and modelling of structure and transport in a field experiment

H.-J. Vogel1,4, I. Cousin2, O. Ippisch3, and P. Bastian3 H.-J. Vogel et al.
  • 1Institute of Environmental Physics, University of Heidelberg, Germany
  • 2INRA, Unité de Science du Sol, Orléans, France
  • 3Interdisciplinary Center of Scientific Computing, University of Heidelberg, Germany
  • 4UFZ – Center for Environmental Research, Leipzig-Halle, Germany

Abstract. A classical transport experiment was performed in a field plot of 2.5 m2 using the dye tracer brilliant blue. The measured tracer distribution demonstrates the dominant role of the heterogeneous soil structure for solute transport. As with many other published experiments, this evidences the need of considering the macroscopic structure of soil to predict flow and transport. We combine three different approaches to represent the relevant structure of the specific situation of our experiment: i) direct measurement, ii) statistical description of heterogeneities and iii) a conceptual model of structure formation. The structure of soil layers was directly obtained from serial sections in the field. The sub-scale heterogeneity within the soil horizons was modelled through correlated random fields with estimated correlation lengths and anisotropy. Earthworm burrows played a dominant role at the transition between the upper soil horizon and the subsoil. A model based on percolation theory is introduced that mimics the geometry of earthworm burrow systems. The hydraulic material properties of the different structural units were obtained by direct measurements where available and by a best estimate otherwise. From the hydraulic structure, the 3-dimensional velocity field of water was calculated by solving Richards' Equation and solute transport was simulated. The simulated tracer distribution compares reasonably well with the experimental data. We conclude that a rough representation of the structure and a rough representation of the hydraulic properties might be sufficient to predict flow and transport, but both elements are definitely required.

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