Search results for "Richards equation"

showing 3 items of 3 documents

Analytical Solution of the Richards Equation under Gravity-Driven Infiltration and Constant Rainfall Intensity

2020

In the field of soil hydrology, the Richards equation is commonly used to model water flow in unsaturated soils. The high nonlinearity of the Richards equation makes it very challenging to solve analytically for situations that are meaningful in practical applications. In this paper, an exact and simple analytical solution of the Richards equation under gravity-driven infiltration and constant rainfall intensity is derived. First, the solution is presented under Torricelli's law, which mimics the soil hydraulic conductivity function and describes the emptying or filling process of a nonlinear water reservoir. Then, following a similar approach, the solution is extended to the Brooks and Cor…

Water flowSoil scienceSoil hydrologyNonlinear systemInfiltration (hydrology)Soil waterRichards equation analytical solution soil water infiltrationSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliEnvironmental ChemistryRichards equationGeologyGeneral Environmental ScienceWater Science and TechnologyCivil and Structural EngineeringJournal of Hydrologic Engineering
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Saturation excess runoff numerical simulation

2005

Saturation excess runoff is a relevant process which needs additional experimental and modeling efforts. This work is focused on its numerical modeling. The final objective is the successive interpretation of ongoing experimental monitoring results in two watersheds in different areas of Italy where the saturation excess runoff formation mechanism seems to be important. The numerical solution of the two-dimensional Richards’ equation allows the evaluation of the sensitivity to the various influent parameters : rainfall intensity, soil properties, depth and initial water content, slope and hillslope length. Also the subsurface flow is simulated at the same time, allowing the evaluation of th…

Soil Saturation excess Numerical solution Richards equationSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestali
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Modelling infiltration by means of a nonlinear fractional diffusion model

2006

The classical Richards equation describes infiltration into porous soil as a nonlinear diffusion process. Recent experiments have suggested that this process exhibits anomalous scaling behaviour. These observations suggest generalizing the classical Richards equation by introducing fractional time derivatives. The resulting fractional Richards equation with appropriate initial and boundary values is solved numerically in this paper. The numerical code is tested against analytical solutions in the linear case. Saturation profiles are calculated for the fully nonlinear fractional Richards equation. Isochrones and isosaturation curves are given. The cumulative moisture intake is found as a fun…

Acoustics and UltrasonicsMathematical analysisCondensed Matter PhysicsSurfaces Coatings and FilmsElectronic Optical and Magnetic MaterialsFractional calculusInfiltration (hydrology)Nonlinear systemFractional diffusionRichards equationPorositySaturation (chemistry)ScalingMathematicsJournal of Physics D: Applied Physics
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