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Hydrology and Earth System Sciences An interactive open-access journal of the European Geosciences Union
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Volume 18, issue 3
Hydrol. Earth Syst. Sci., 18, 1105-1118, 2014
https://doi.org/10.5194/hess-18-1105-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
Hydrol. Earth Syst. Sci., 18, 1105-1118, 2014
https://doi.org/10.5194/hess-18-1105-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 21 Mar 2014

Research article | 21 Mar 2014

Measuring and modeling water-related soil–vegetation feedbacks in a fallow plot

N. Ursino1, G. Cassiani2, R. Deiana3, G. Vignoli4, and J. Boaga2 N. Ursino et al.
  • 1Department ICEA, University of Padova, Padova, Italy
  • 2Department of Geosciences, University of Padova, Padova, Italy
  • 3Department dBC, University of Padova, Padova, Italy
  • 4Geological Survey of Denmark and Greenland, Groundwater and Quaternary Geology Mapping Department, Lyseng Alle 1, 8270 Hojbjerg, Denmark

Abstract. Land fallowing is one possible response to shortage of water for irrigation. Leaving the soil unseeded implies a change of the soil functioning that has an impact on the water cycle. The development of a soil crust in the open spaces between the patterns of grass weed affects the soil properties and the field-scale water balance. The objectives of this study are to test the potential of integrated non-invasive geophysical methods and ground-image analysis and to quantify the effect of the soil–vegetation interaction on the water balance of fallow land at the local- and plot scale.

We measured repeatedly in space and time local soil saturation and vegetation cover over two small plots located in southern Sardinia, Italy, during a controlled irrigation experiment. One plot was left unseeded and the other was cultivated. The comparative analysis of ERT maps of soil moisture evidenced a considerably different hydrologic response to irrigation of the two plots. Local measurements of soil saturation and vegetation cover were repeated in space to evidence a positive feedback between weed growth and infiltration at the fallow plot. A simple bucket model captured the different soil moisture dynamics at the two plots during the infiltration experiment and was used to estimate the impact of the soil vegetation feedback on the yearly water balance at the fallow site.

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