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Soil micromorphology use for modeling of a non-equilibrium water and solute movement

Author

Listed:
  • R. Kodešová

    (Department of Soil Science and Soil Protection, Czech University of Life Sciences Prague, Prague, Czech Republic)

Abstract

Soil micromorphology was applied to specify flow domains in different soils and to select a suitable numerical model for simulation of water flow and herbicide transport. Pore structure detected on soil micromorphological images represented in all cases domains of prevailing water flow and solute transport. Depending on pore configuration and boundary conditions either water immobilization or preferential flow was observed and simulated. The benefits and limitations of the soil micromorphology imaging are discussed and compared with the more often used X-ray computer tomography, magnetic resonance imaging and dye tracer imaging.

Suggested Citation

  • R. Kodešová, 2009. "Soil micromorphology use for modeling of a non-equilibrium water and solute movement," Plant, Soil and Environment, Czech Academy of Agricultural Sciences, vol. 55(10), pages 424-428.
    • Handle: RePEc:caa:jnlpse:v:55:y:2009:i:10:id:137-2009-pse
    DOI: 10.17221/137/2009-PSE
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    References listed on IDEAS

    as
    1. Jiří Šimůnek & J. Maximilian Köhne & Radka Kodešová & Miroslav Šejna, 2008. "Simulating nonequilibrium movement of water, solutes and particles using hydrus - a review of recent applications," Soil and Water Research, Czech Academy of Agricultural Sciences, vol. 3(SpecialIs), pages 42-51.
    2. R. Kodešová & J. Kozák & O. Vacek, 2004. "Field and numerical study of chlorotoluron transport in the soil profile," Plant, Soil and Environment, Czech Academy of Agricultural Sciences, vol. 50(8), pages 333-338.
    3. M. Kočárek & R. Kodešová & J. Kozák & O. Drábek & O. Vacek, 2005. "Chlortoluron behavior in five different soil types," Plant, Soil and Environment, Czech Academy of Agricultural Sciences, vol. 51(7), pages 304-309.
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