ANALYTICAL SOLUTION OF UNSATURATED SOIL WATER FLOW FROM A POINT SOURCE

نویسندگان

چکیده

Water flow into unsaturated porous media is governed by the Richards’ partial differential equation expressing mass conservation and Darcy’s laws. The may be written in three forms,where dependent variable pressure head or moisture content, constitutive relationships between water content allow for conversion of one form other. In present paper, “moisture-based" linearized applying Kirchhoff’s transformation, whichcombines soil diffusivity content. Then similarity method used to obtain analytical solution wetting front position. This exact obtained means Lie’s infinitesimal transformation groups. predicted results agreed well with available experiments numerical solutions.

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ژورنال

عنوان ژورنال: Ma?allat? al-handasat?

سال: 2023

ISSN: ['1726-4073', '2520-3339']

DOI: https://doi.org/10.31026/j.eng.2012.01.07