Abstract

This paper reports the modelling of two-dimensional infiltration experiments, with diesel or water as the permeate liquids in an unsaturated dune sand. Also reports the measurements of soil hydraulic properties (retention curve and saturated hydraulic conductivity) in laboratory, and infiltration experiments using a 2D channel. The time ratio (T diesel/T water) for the wetting fronts to reach the tensiometers was consistent with the ratio of mobilities water/diesel, The SEEP/W, a numerical 2D code, modelled well the successive wetting front vertical positions for the liquids. However, the simulations for the lateral spreading were better for diesel, as this experiment was a complete wetting phenomenon, differently for water, that developed unsaturated conditions inside the column. The Philip 1D equation modelled the successive vertical positions for the liquids, using two different sets of parameters. The first set (ϕ, Kñsat , hp = 0): porosity, unsaturated hydraulic conductivity and incipient hydraulic head; and the second set, (ϕ c, Ksat , hp = 0): corrected porosity value to include the plume lateral spreading, saturated hydraulic conductivity and incipient hydraulic head. Although both sets of parameters are adequate to model the vertical component of the infiltration experiments, the first set is more efficient as it is independent of the corrected porosity, a value known afterwards.

Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.