28 Pags.- 5 Figs.- 3 Tabls. The definitive version is available at: https://www.sciencedirect.com/science/journal/00221694Soil water infiltration can be described with the quasi-analytical Haverkamp et al. (1994) equation, defined by the hydraulic conductivity (Ks), sorptivity (S) and the β parameter. Ks and S are commonly estimated from the transient cumulative infiltration curve, using a constant β value. The objective of this work was to study the influence of β on the estimation of Ks and S. The study was first performed on synthetic 1-D infiltration curves generated at different infiltration times for loam sandy, loamy and silty soils, and next extrapolated to a 3-D loam synthetic soil and on 10 infiltrations curves measured on the fi...
[Departement_IRSTEA]RE [TR1_IRSTEA]RIE / TRANSFEAU [TR2_IRSTEA]RIE / PHYLEAUInternational audienceSt...
11 pags.- 5 Figs.- 5 Tabls. © 2022 The Authors. Published by Elsevier B.V. This is an open access...
Abstract Many different equations ranging from simple empirical to semi‐analytical solutions of the ...
34 Pags.- 2 Tabls.- 6 Figs. The definitive version is available at: https://www.sciencedirect.com/s...
AbstractThis paper describes a new method (NSQE) to estimate soil hydraulic properties (sorptivity, ...
In the present study, the determination of soil saturated hydraulic conductivity (Ks) and soil sorpt...
38 Pags.- 3 Tabls.- 10 Figs. The definitive version is available at: https://www.sciencedirect.com/...
Hydraulic parameters of the soil play a considerable role in the hydrological cycle, irrigation plan...
Modeling infiltration in water-repellent soils is difficult, as the underlying processes remain poor...
International audiencetudying soil hydrological processes requires the determination of soil hydraul...
The topic of infiltration of water into variably saturated soils has received muchattention in the s...
Simple and reasonably rapid experiments are desirable to conduct a spatially distributed determinati...
36 pags.- 8 Figs.- 2 Tabls. The definitive version is available at: https://www.sciencedirect.com/s...
International audienceThe soil sorptivity, S, and saturated hydraulic conductivity, Ks, can be estim...
38 pags.- 3 Tabls.- 11 Figs. The definitive version is available at: http://onlinelibrary.wiley.com...
[Departement_IRSTEA]RE [TR1_IRSTEA]RIE / TRANSFEAU [TR2_IRSTEA]RIE / PHYLEAUInternational audienceSt...
11 pags.- 5 Figs.- 5 Tabls. © 2022 The Authors. Published by Elsevier B.V. This is an open access...
Abstract Many different equations ranging from simple empirical to semi‐analytical solutions of the ...
34 Pags.- 2 Tabls.- 6 Figs. The definitive version is available at: https://www.sciencedirect.com/s...
AbstractThis paper describes a new method (NSQE) to estimate soil hydraulic properties (sorptivity, ...
In the present study, the determination of soil saturated hydraulic conductivity (Ks) and soil sorpt...
38 Pags.- 3 Tabls.- 10 Figs. The definitive version is available at: https://www.sciencedirect.com/...
Hydraulic parameters of the soil play a considerable role in the hydrological cycle, irrigation plan...
Modeling infiltration in water-repellent soils is difficult, as the underlying processes remain poor...
International audiencetudying soil hydrological processes requires the determination of soil hydraul...
The topic of infiltration of water into variably saturated soils has received muchattention in the s...
Simple and reasonably rapid experiments are desirable to conduct a spatially distributed determinati...
36 pags.- 8 Figs.- 2 Tabls. The definitive version is available at: https://www.sciencedirect.com/s...
International audienceThe soil sorptivity, S, and saturated hydraulic conductivity, Ks, can be estim...
38 pags.- 3 Tabls.- 11 Figs. The definitive version is available at: http://onlinelibrary.wiley.com...
[Departement_IRSTEA]RE [TR1_IRSTEA]RIE / TRANSFEAU [TR2_IRSTEA]RIE / PHYLEAUInternational audienceSt...
11 pags.- 5 Figs.- 5 Tabls. © 2022 The Authors. Published by Elsevier B.V. This is an open access...
Abstract Many different equations ranging from simple empirical to semi‐analytical solutions of the ...