The Richards equation represents the movement of water in unsaturated soils, and is attributed to Lorenzo A. Richards who published the equation in 1931. |
| Уравнение Ричардса |  |
Уравнение Ричардса, описывающее влагоперенос в зоне аэрации, было сформулировано Лоренцо А. Ричардсом в 1931 году. Оно представляет собой нелинейное дифференциальное уравнение в частных производных, основная трудность решения которого заключается... Википедия
The Richards equation (Richards, 1931), a physical–mathematical model developed in the context of a volume averaged and porous-continuum approach, ... |
The Richardson–Richards Equation is the most widely-used equation governing the movement of water in unsaturated soils. |
The corresponding mathematical model is a generalized Richards' equation in which the derivative of water content on time is a fractional one with the order. |
19 окт. 2017 г. · Richards' equation can be seen as a simplification of the standard two-phase flow formulation for a gas and water phase in a porous medium where ... |
5 сент. 2016 г. · GREEN AMPT METHOD: When the rainfall occurs on the plain surface, the soils in the top surface may be saturated or unsaturated before rainfall. |
22 окт. 2024 г. · The Richards equation [22] is a mechanistic model that accounts for various hydrological processes, including irrigation, rain, ... |
27 янв. 2023 г. · Richards' equation (RE) describes the movement of water in variably saturated porous media. Almost any practical application of RE requires a ... |
1 нояб. 2017 г. · The Richards equation, commonly used to model water flow in unsaturated soils, is highly nonlinear, thus making it very challenging to solve ... |
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