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Richards equation

The Richards equation represents the movement of water in unsaturated soils, and is attributed to Lorenzo A. Richards who published the equation in 1931. It is a quasilinear partial differential equation; its analytical solution is often limited to specific initial and boundary conditions. Proof of the existence and uniqueness of solution was given only…

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Formulations

Parametrization

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Richards equation

Nodes34
Edges33
Triples15
Avg. degree1.94
Density0.058824
Components1

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Richards equation

Top relations

related to Formulations · 6
Richards equation → Applying, It, Richards, The, The Richards, This
related to Parametrization · 5
Richards equation → Further, Genuchten, Identification, The, The Richards
related to Limitations · 4
Richards equation → Advanced, In, Richards, The

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equation richards displaystyle theta water solution soil flow also retention frac numerical saturated stated infiltration attributed conditions known curve applying

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SubjectPredicateObjectConfidenceSrc
Richards equationrelated to FormulationsThe Richards0.60section
Richards equationrelated to FormulationsIt0.60section
Richards equationrelated to FormulationsThe0.60section
Richards equationrelated to FormulationsThis0.60section
Richards equationrelated to FormulationsApplying0.60section
Richards equationrelated to FormulationsRichards0.60section
Richards equationrelated to LimitationsThe0.60section
Richards equationrelated to LimitationsRichards0.60section
Richards equationrelated to LimitationsAdvanced0.60section
Richards equationrelated to LimitationsIn0.60section
Richards equationrelated to ParametrizationThe Richards0.60section
Richards equationrelated to ParametrizationThe0.60section

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