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BY-NC-ND 3.0 license Open Access Published by De Gruyter November 1, 2006

Impact of plant roots and soil organisms on soil micromorphology and hydraulic properties

  • Radka Kodešová EMAIL logo , Vít Kodeš , Anna Žigová and Jiří Šimůnek
From the journal Biologia

Abstract

A soil micromorphological study was performed to demonstrate the impact of soil organisms on soil pore structure. Two examples are shown here. First, the influence of earthworms, enchytraeids and moles on the pore structure of a Greyic Phaeozem is demonstrated by comparing two soil samples taken from the same depth of the soil profile that either were affected or not affected by these organisms. The detected image porosity of the organism-affected soil sample was 5 times larger then the porosity of the not-affected sample. The second example shows macropores created by roots and soil microorganisms in a Haplic Luvisol and subsequently affected by clay coatings. Their presence was reflected in the soil water retention curve, which displayed multiple S-shaped features as obtained from the water balance carried out for the multi-step outflow experiment. The dual permeability models implemented in HYDRUS-1D was applied to obtain parameters characterizing multimodal soil hydraulic properties using the numerical inversion of the multi-step outflow experiment.

[1] Bouma, J., Jongerius, A., Boersma, O., Jager, A. & Schoonderbeek, D. 1977. The function of different types of macropores during saturated flow through four swelling soil horizons. Soil Sci. Soc. Am. J. 41: 945–950. http://dx.doi.org/10.2136/sssaj1977.03615995004100050028x10.2136/sssaj1977.03615995004100050028xSearch in Google Scholar

[2] Bruand, A., Cousin, I., Nicoullaud, B., Duval, O. & Bégon, J.C. 1996. Backscatter electron scanning images of soil porosity for analyzing soil compaction around roots. Soil Sci. Soc. Am. J. 60: 1718–1724. http://dx.doi.org/10.2136/sssaj1996.03615995006000030031x10.2136/sssaj1996.03615995006000030031xSearch in Google Scholar

[3] Catt, J. A. 1990. Paleopedology manual. Quaternary International 6: 1–95. http://dx.doi.org/10.1016/1040-6182(90)90002-L10.1016/1040-6182(90)90002-LSearch in Google Scholar

[4] Durner, W. 1994. Hydraulic conductivity estimation for soils with heterogeneous pore structure. Water Resour. Res. 30: 211–233. http://dx.doi.org/10.1029/93WR0267610.1029/93WR02676Search in Google Scholar

[5] Dušek, J., Vogel, T., Lichner, L’., Čipáková, A. & Dohnal, M. 2006. Simulated cadmium transport in macroporous soil during heavy rainstorm using dual-permeability approach. Biologia, Bratislava 61(Supl. 19): S251–S254. Search in Google Scholar

[6] Kočárek, M., Kodešová, R., Kozák, J., Drábek, O. & Vacek, O. 2005. Chlorotoluron behaviour in five different soil types. Plant, Soil Environ. 51: 304–309. Search in Google Scholar

[7] Kodešová, R., Kozák, J., Šimůnek, J. & Vacek, O. 2005. Single and dual-permeability model of chlorotoluron transport in the soil profile. Plant, Soil Environ. 51: 310–315. Search in Google Scholar

[8] Pagliai, M., La Mace, M. & Lucamante, G. 1983. Micromorphometric and micromorphological investigations of a clay loam soil in viticulture under zero and conventional tillage. J. Soil Sci. 34: 391–403. http://dx.doi.org/10.1111/j.1365-2389.1983.tb01044.x10.1111/j.1365-2389.1983.tb01044.xSearch in Google Scholar

[9] Pagliai, M., Vignozzi, N. & Pellegrini, S. 2004. Soil structure and the effect of management practices. Soil Till. Res. 79: 131–143. http://dx.doi.org/10.1016/j.still.2004.07.00210.1016/j.still.2004.07.002Search in Google Scholar

[10] Rösslerová-Kodešová, R. & Kodeš, V. 1999. Percolation model for interpretation of moisture retention curves for mono-modal and bi-modal soil porous systems, pp. 81–91. In: van Genuchten, M. Th., Leij, F.J. & Wu, L. (eds), Characterization and measurement of the hydraulic properties of unsaturated porous media. University of California, Riverside. Search in Google Scholar

[11] Šimůnek, J., Jarvis, N.J., van Genuchten, M.Th. & Gärdenäs A. 2003. Review and comparison of models for describing non-equilibrium and preferential flow and transport in the vadose zone. J. Hydrol. 272: 14–35. http://dx.doi.org/10.1016/S0022-1694(02)00252-410.1016/S0022-1694(02)00252-4Search in Google Scholar

[12] Šimůnek, J., van Genuchten, M.Th. & Šejna M. 2005. The HYDRUS-1D software package for simulating the one-dimensional movement of water, heat and multiple solutes in variably-saturated media. Version 3.0. Dept. of Environmental Sciences, University of California Riverside, Riverside, California, 240 pp. Search in Google Scholar

[13] van Genuchten, M.Th. 1980. A closed-form equation for predicting the hydraulic conductivity of unsaturated soils. Soil Sci. Soc. Am. J. 44: 892–898. http://dx.doi.org/10.2136/sssaj1980.03615995004400050002x10.2136/sssaj1980.03615995004400050002xSearch in Google Scholar

Published Online: 2006-11-1
Published in Print: 2006-11-1

© 2006 Institute of Botany, Slovak Academy of Sciences

This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 3.0 License.

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