In this study, different methods were compared in order to determine the soil hydraulic conductivity at the saturation (Ks) of two heavily anthropized soils in northern Italy: an irrigated field and a landfill cover. In situ, laboratory measurements (falling head and evaporation method) and pedotransfer functions (ROSETTA and HYPRES) were used for the Ks estimation. In accordance with scientific literature, the results have shown that Ks is largely dependent on the type of technique used in taking the measurements. The ROSETTA and HYPRES pedotransfer functions show quite similar performances, while their easiness and convenient use make them potential alternative techniques for the Ks estimation in comparison with the in situ and laboratory measurements. The Ks estimate is sensitive to the selected method and this sensitivity affects the hydrological model simulations. Therefore, none of the tested methods can be considered as a benchmark, but the results found in this study confirm that the applied method for the determination of Ks, may provide a first estimate of Ks to be subsequently optimised after the simulations.

A comparative assessment of the estimates of the saturated hydraulic conductivity of two anthropogenic soils and their impact on hydrological model simulations

Feki M.;Ravazzani G.;Ceppi A.;Mancini M.
2020

Abstract

In this study, different methods were compared in order to determine the soil hydraulic conductivity at the saturation (Ks) of two heavily anthropized soils in northern Italy: an irrigated field and a landfill cover. In situ, laboratory measurements (falling head and evaporation method) and pedotransfer functions (ROSETTA and HYPRES) were used for the Ks estimation. In accordance with scientific literature, the results have shown that Ks is largely dependent on the type of technique used in taking the measurements. The ROSETTA and HYPRES pedotransfer functions show quite similar performances, while their easiness and convenient use make them potential alternative techniques for the Ks estimation in comparison with the in situ and laboratory measurements. The Ks estimate is sensitive to the selected method and this sensitivity affects the hydrological model simulations. Therefore, none of the tested methods can be considered as a benchmark, but the results found in this study confirm that the applied method for the determination of Ks, may provide a first estimate of Ks to be subsequently optimised after the simulations.
Double ring infiltrometer
Evaporation method
Guelph permeameter
Hydraulic conductivity at soil saturation
Laboratory experiments
Pedotransfer functions
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Utilizza questo identificativo per citare o creare un link a questo documento: http://hdl.handle.net/11311/1158695
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