Derivation of the SCS-CN parameter S from linearized Fokker-Planck equation

• Autorzy: Mishra S. , Singh V.
• Języki publikacji: EN

Abstrakty

EN

The potential maximum retention, S, of the Soil Conservation Service Curve Number (SCS-CN) method (SCS, 1956) was derived for a large set of published infiltration data ranging from Plainfield sand to Yololight clay using the relations between psi (negative pressure) and theta (moisture content) and between K (hydraulic conductivity) and theta. The physical significance of S is explained using the diffusion term of the linearized, Fokker-Planck equation for infiltration, which relates S to the storage and transmission properties of the soil. The s-values exhibit a strong looped relationship with the initial moisture content, analogous to that for curve numbers for three antecedent moisture conditions. The variations of S in vertical infiltration is also explained and discussed.

Słowa kluczowe

EN

curve number; infiltration; Fokker-Planck equation; SCS-CN method

• Wydawca: Instytut Geofizyki PAN
• Czasopismo: Acta Geophysica Polonica
• Rocznik: 2003
• Tom: Vol. 51, nr 2
• Strony: 179--202
• Opis fizyczny: Bibliogr. 56 poz.

Twórcy

autor

Mishra S.

• National Institute of Hydrology, Roorkee-247 667, India

autor

Singh V.

• Department of Civil and Environmental Engineering Louisiana, State of University, Baton Rouge, Louisiana 70803-6405, USA

Bibliografia

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