International audienceSoil hydraulic characterization is crucial to describe the retention and transport of water in soil, but current methodologies limit its spatial applicability. This paper presents a cost-effective general Beerkan Estimation of Soil Transfer parameters (BEST) methodology using single ring infiltration experiments to derive soil hydraulic parameters for any unimodal water retention and hydraulic conductivity functions. The proposed method relies on the BEST approach. The novelty lies in the use of Kosugi hydraulic parameters without need for textural in- formation. In addition, the method uses a quasi-exact formulation that is valid for all times, which avoids the use of approximate expansions and related inaccuracy. The...
Testing infiltrometer techniques to determine soil hydraulic properties is necessary for specific so...
[Departement_IRSTEA]Eaux [TR1_IRSTEA]ARCEAUInternational audienceModelling and understanding water f...
The macroscopic capillary length, λc, is a fundamental soil parameter expressing the relative import...
International audiencetudying soil hydrological processes requires the determination of soil hydraul...
Theories and models used in soil hydrological sciences rely on the knowledge of the spatially and te...
The Beerkan Estimation of Soil Transfer parameters (BEST) procedure is attractive for a simple soil ...
Establishing the ability of the Beerkan Estimation of Soil Transfer parameters (BEST) procedure to r...
[Departement_IRSTEA]RE [TR1_IRSTEA]RIE / TRANSFEAU [TR2_IRSTEA]RIE / PHYLEAUInternational audienceSt...
International audienceAbstract The determination of soil hydraulic properties is important in severa...
International audienceWater movement in soil can be described accurately at the local scale, provide...
Single-ring infiltration experiments carried out in the field, such as the Beerkan runs, allow easy ...
The Beerkan Estimation of Soil Transfer parameters (BEST) procedure is an attractive, easy, robust, ...
Interpreting and simulating hydrological processes need a large number of field saturated soil hydra...
Testing infiltrometer techniques to determine soil hydraulic properties is necessary for specific so...
[Departement_IRSTEA]Eaux [TR1_IRSTEA]ARCEAUInternational audienceModelling and understanding water f...
The macroscopic capillary length, λc, is a fundamental soil parameter expressing the relative import...
International audiencetudying soil hydrological processes requires the determination of soil hydraul...
Theories and models used in soil hydrological sciences rely on the knowledge of the spatially and te...
The Beerkan Estimation of Soil Transfer parameters (BEST) procedure is attractive for a simple soil ...
Establishing the ability of the Beerkan Estimation of Soil Transfer parameters (BEST) procedure to r...
[Departement_IRSTEA]RE [TR1_IRSTEA]RIE / TRANSFEAU [TR2_IRSTEA]RIE / PHYLEAUInternational audienceSt...
International audienceAbstract The determination of soil hydraulic properties is important in severa...
International audienceWater movement in soil can be described accurately at the local scale, provide...
Single-ring infiltration experiments carried out in the field, such as the Beerkan runs, allow easy ...
The Beerkan Estimation of Soil Transfer parameters (BEST) procedure is an attractive, easy, robust, ...
Interpreting and simulating hydrological processes need a large number of field saturated soil hydra...
Testing infiltrometer techniques to determine soil hydraulic properties is necessary for specific so...
[Departement_IRSTEA]Eaux [TR1_IRSTEA]ARCEAUInternational audienceModelling and understanding water f...
The macroscopic capillary length, λc, is a fundamental soil parameter expressing the relative import...