The recent similarity hypotheses to describe water infiltration into homogeneous soils

ABSTRACT A similarity hypothesis recently presented to describe horizontal infiltration into homogeneous soils, developed for coarse-textured soils like sieved marine sand, implies that the soil water retention function θ(h) is the mirror image of an extended Boltzmann transform function θ(λ2). A se...

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Main Authors: Klaus Reichardt, Luís Carlos Timm, Durval Dourado-Neto
Format: Article
Language:English
Published: Universidade de São Paulo 2016-08-01
Series:Scientia Agricola
Subjects:
Online Access:http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0103-90162016000400379&lng=en&tlng=en
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spelling doaj-3664655d7c924cada347e7d6dae0fa952020-11-24T21:14:49ZengUniversidade de São PauloScientia Agricola1678-992X2016-08-0173437938310.1590/0103-9016-2015-0364S0103-90162016000400379The recent similarity hypotheses to describe water infiltration into homogeneous soilsKlaus ReichardtLuís Carlos TimmDurval Dourado-NetoABSTRACT A similarity hypothesis recently presented to describe horizontal infiltration into homogeneous soils, developed for coarse-textured soils like sieved marine sand, implies that the soil water retention function θ(h) is the mirror image of an extended Boltzmann transform function θ(λ2). A second hypothesis applicable to vertical infiltration suggests that the soil water retention function θ(h) is also the mirror image of the soil water profile θ(z). Using previously published infiltration data, we investigated whether these two similarity solutions successfully describe infiltration into two “normal” soils. Although the theory using the first similarity assumption adequately describes horizontal cumulative infiltration and infiltration rate into both soils, it fails to estimate soil water distributions measured between soil profiles. The second similarity solution for vertical infiltration into either soil completely fails to coincide with measured soil water distributions, cumulative infiltration and infiltration rate.http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0103-90162016000400379&lng=en&tlng=enBoltzmann functionmirror imagewetting front
collection DOAJ
language English
format Article
sources DOAJ
author Klaus Reichardt
Luís Carlos Timm
Durval Dourado-Neto
spellingShingle Klaus Reichardt
Luís Carlos Timm
Durval Dourado-Neto
The recent similarity hypotheses to describe water infiltration into homogeneous soils
Scientia Agricola
Boltzmann function
mirror image
wetting front
author_facet Klaus Reichardt
Luís Carlos Timm
Durval Dourado-Neto
author_sort Klaus Reichardt
title The recent similarity hypotheses to describe water infiltration into homogeneous soils
title_short The recent similarity hypotheses to describe water infiltration into homogeneous soils
title_full The recent similarity hypotheses to describe water infiltration into homogeneous soils
title_fullStr The recent similarity hypotheses to describe water infiltration into homogeneous soils
title_full_unstemmed The recent similarity hypotheses to describe water infiltration into homogeneous soils
title_sort recent similarity hypotheses to describe water infiltration into homogeneous soils
publisher Universidade de São Paulo
series Scientia Agricola
issn 1678-992X
publishDate 2016-08-01
description ABSTRACT A similarity hypothesis recently presented to describe horizontal infiltration into homogeneous soils, developed for coarse-textured soils like sieved marine sand, implies that the soil water retention function θ(h) is the mirror image of an extended Boltzmann transform function θ(λ2). A second hypothesis applicable to vertical infiltration suggests that the soil water retention function θ(h) is also the mirror image of the soil water profile θ(z). Using previously published infiltration data, we investigated whether these two similarity solutions successfully describe infiltration into two “normal” soils. Although the theory using the first similarity assumption adequately describes horizontal cumulative infiltration and infiltration rate into both soils, it fails to estimate soil water distributions measured between soil profiles. The second similarity solution for vertical infiltration into either soil completely fails to coincide with measured soil water distributions, cumulative infiltration and infiltration rate.
topic Boltzmann function
mirror image
wetting front
url http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0103-90162016000400379&lng=en&tlng=en
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