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• W2070507184 abstract "Systematic experimental deviations from theoretical predictions for water retention characteristics of fractal porous media develop at a moisture content, θd. Below θd larger suction pressures are required than would otherwise be predicted from the implied fractal pore-size distribution. Inferred values of θd were shown to be compatible with observed values of the volumetric moisture content, θt, at which solute diffusion vanishes. The comparison was based on an accurate phenomenological result for θt. The approximate equivalence of the two moisture contents was interpreted in the context of continuum percolation theory (at low moisture contents, below a critical volume fraction of water, αc, connections for capillary flow are interrupted, leading to a near vanishing of solute diffusion and increasing enormously the time required for equilibration to new pressures). The experimental results for θd are now investigated to determine whether their values are generally compatible with theoretically based estimates for αc." @default.
• W2070507184 created "2016-06-24" @default.
• W2070507184 creator A5074221720 @default.
• W2070507184 date "2004-02-01" @default.
• W2070507184 modified "2023-09-23" @default.
• W2070507184 title "Continuum percolation theory for water retention and hydraulic conductivity of fractal soils: estimation of the critical volume fraction for percolation" @default.
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• W2070507184 doi "https://doi.org/10.1016/j.advwatres.2003.10.004" @default.
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