Fuzzy Analytical Solution of Horizontal Diffusion Equation into the Vadose Zone
نویسندگان
چکیده
The process of how soil moisture profiles evolve into the and reach root zone could be estimated by solving appropriate strong nonlinear Richards’ equation. nonlinearity equation occurs because diffusivity D is generally an exponential function water content. In this work, boundary conditions physical problem are considered fuzzy for various reasons (e.g., machine impression, human errors, etc.), overall encountered with a new approximate analytical solution, leading to system crisp value problems. According results, proposed solution in close agreement Philip’s semi-analytical method, which used as reference after testing 12 different types soils. Additionally, possibility theory applied, enabling decision-makers take meaningful actions gain knowledge hydraulic properties sorptivity, infiltration, etc.) rational productive engineering studies irrigation systems).
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ژورنال
عنوان ژورنال: Hydrology
سال: 2023
ISSN: ['2330-7609', '2330-7617']
DOI: https://doi.org/10.3390/hydrology10050107