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The associated factors exerted influence on the soil hydraulic properties at their own dominant scale(s).
Four PTFs (referred to as Model V, Model S, Model W, and Model L) were then used to predict the hydraulic properties at the sampled locations.
The objective of this study is to apply this framework to characterizing the impacts of soil hydraulic properties at multiple scales on moisture storage and distributed runoff generation in a forested catchment.
These numerical tests were conducted using models of the soil hydraulic properties like the van Genuchten Mualem model, which account only for water retention and conductivity in completely filled capillaries and thus give biased descriptions of the hydraulic properties at low moisture contents.
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As for the exponent, besides the role of field scale soil hydraulic properties as suggested by hydraulic theory, it is found to be more strongly affected by climate (aridity) at the catchment scale.
The stemflow and throughfall regions exhibited contrasting hydraulic properties as indicated by the estimated hydraulic parameters.
Realistic models of contaminant transport in groundwater demand detailed characterization of the spatial distribution of subsurface hydraulic properties, while at the same time programmatic constraints may limit collection of pertinent hydraulic data.
The hydraulic properties of the soils at the site were determined using in situ experiments and laboratory measurements.
This case study illustrates the complexity of finding validated scaling relationships for the hydraulic properties of heterogeneous soils at scales larger than the usual small column scale.
To determine the most important constraints imposed by termite mounds on plant establishment, we investigated chemical, physical, and hydraulic properties of termite mounds at an 8-year-old secondary forest site, and their effects on the development of native plant species.
Considering that one important application of the LB model in porous materials is to calculate their hydraulic properties when flow is at steady state, we develop a simple LB model to simulate steady water flow at pore scale in unsaturated soils.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com