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Relationship between van Genuchten's parameters of the retention curve equation and physical properties of soil solid phase

D. Porebska, +3 more
- 01 Jan 2006 - 
- Vol. 20, Iss: 2, pp 153-159
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TLDR
Van Genuchten parameters α, n, θ s, θ r were determined for 24 Phaeozems and 54 Gleysols samples taken from surface, subsurface and subsoil horizons as discussed by the authors.
Abstract
Van Genuchten parameters α, n, θ s , θ r were determined for 24 Phaeozems and 54 Gleysols samples taken from surface, subsurface and subsoil horizons. No evident dependences between van Genuchten's a, n,θ s ,θ r parameters and the physical properties of Phaeozems soil samples were observed, which was due to a similar genesis and similar properties of soil solid phase. Analysis of Gleysols, on the other hand, revealed dependences between the physical soil properties and van Genuchten's parameters resulting from different geneses of these soils and, hence, different physical properties of soil solid phase. The obtained results should be considered as preliminary and further studies on a larger number ofsoil samples are planned.

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Citations
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References
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Journal ArticleDOI

A closed-form equation for predicting the hydraulic conductivity of unsaturated soils

TL;DR: Van Genuchten et al. as mentioned in this paper proposed a closed-form analytical expression for predicting the hydraulic conductivity of unsaturated soils based on the Mualem theory, which can be used to predict the unsaturated hydraulic flow and mass transport in unsaturated zone.
Journal ArticleDOI

Estimation of Soil Water Properties

TL;DR: In this article, a comprehensive search of the literature and data sources for hydraulic conductivity and related soil-water data was made in 1978 and data for 1,323 soils with about 5,350 horizons from 32 states were assembled.
Journal ArticleDOI

Estimating soil water retention characteristics from particle size distribution, organic matter percent, and bulk density

TL;DR: In this article, regression models for estimating soil-water-retention curves from particle-size distribution, percentage of organic matter, and bulk density were presented for estimating water retention curves.
Book ChapterDOI

Estimation of Soil Water Retention and Hydraulic Properties

TL;DR: Water flow in soils can be characterized, in principle, for many boundary and initial conditions by solving the proper governing differential equations as discussed by the authors, but this state-of-the-art technology is not yet fully utilized.
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