The Similarity Hypothesis and New Analytical Support on the Estimation of Horizontal Infiltration into Sand

A method based on a specific power-law relationship between the hydraulic head and the Boltzmann variable, presented using a similarity hypothesis, was recently generalized to a range of powers to satisfy the Bruce and Klute equation exactly. Here, considerations are presented on the proposed simila...

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Main Authors: Celso L. Prevedello, Jocely M. T. Loyola
Format: Article
Language:English
Published: Hindawi Limited 2010-01-01
Series:Applied and Environmental Soil Science
Online Access:http://dx.doi.org/10.1155/2010/657402
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spelling doaj-b0762499f23b4c5bba2a8b7f3b773e4e2020-11-24T23:04:21ZengHindawi LimitedApplied and Environmental Soil Science1687-76671687-76752010-01-01201010.1155/2010/657402657402The Similarity Hypothesis and New Analytical Support on the Estimation of Horizontal Infiltration into SandCelso L. Prevedello0Jocely M. T. Loyola1Soils and Agricultural Engineering Department, Federal University of Paraná Rua dos Funcionários 1540, 80030-035 Curitiba, PR, BrazilCivil Construction Department, Federal University of Paraná, 81531-990 Curitiba, PR, BrazilA method based on a specific power-law relationship between the hydraulic head and the Boltzmann variable, presented using a similarity hypothesis, was recently generalized to a range of powers to satisfy the Bruce and Klute equation exactly. Here, considerations are presented on the proposed similarity assumption, and new analytical support is given to estimate the water density flux into and inside the soil, based on the concept of sorptivity and on Buckingham-Darcy's law. Results show that the new analytical solution satisfies both theories in the calculation of water density fluxes and is in agreement with experimental results of water infiltrating horizontally into sand. However, the utility of this analysis still needs to be verified for a variety of different textured soils having a diverse range of initial soil water contents.http://dx.doi.org/10.1155/2010/657402
collection DOAJ
language English
format Article
sources DOAJ
author Celso L. Prevedello
Jocely M. T. Loyola
spellingShingle Celso L. Prevedello
Jocely M. T. Loyola
The Similarity Hypothesis and New Analytical Support on the Estimation of Horizontal Infiltration into Sand
Applied and Environmental Soil Science
author_facet Celso L. Prevedello
Jocely M. T. Loyola
author_sort Celso L. Prevedello
title The Similarity Hypothesis and New Analytical Support on the Estimation of Horizontal Infiltration into Sand
title_short The Similarity Hypothesis and New Analytical Support on the Estimation of Horizontal Infiltration into Sand
title_full The Similarity Hypothesis and New Analytical Support on the Estimation of Horizontal Infiltration into Sand
title_fullStr The Similarity Hypothesis and New Analytical Support on the Estimation of Horizontal Infiltration into Sand
title_full_unstemmed The Similarity Hypothesis and New Analytical Support on the Estimation of Horizontal Infiltration into Sand
title_sort similarity hypothesis and new analytical support on the estimation of horizontal infiltration into sand
publisher Hindawi Limited
series Applied and Environmental Soil Science
issn 1687-7667
1687-7675
publishDate 2010-01-01
description A method based on a specific power-law relationship between the hydraulic head and the Boltzmann variable, presented using a similarity hypothesis, was recently generalized to a range of powers to satisfy the Bruce and Klute equation exactly. Here, considerations are presented on the proposed similarity assumption, and new analytical support is given to estimate the water density flux into and inside the soil, based on the concept of sorptivity and on Buckingham-Darcy's law. Results show that the new analytical solution satisfies both theories in the calculation of water density fluxes and is in agreement with experimental results of water infiltrating horizontally into sand. However, the utility of this analysis still needs to be verified for a variety of different textured soils having a diverse range of initial soil water contents.
url http://dx.doi.org/10.1155/2010/657402
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