Extension of the Gardner exponential equation to represent the hydraulic conductivity curve
The relative hydraulic conductivity curve Kr(h) = K/Ks is a key variable in soil modeling. This study proposes a model to represent Kr(h), the so-called Gardner dual (GD) model, which extends the classical Gardner exponential model to h values greater than ho, the suction value at the inflection poi...
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doaj-1dadde6e80fa44f0a41f8677577c9b742021-09-06T19:41:40ZengSciendoJournal of Hydrology and Hydromechanics0042-790X2019-12-0167435937110.2478/johh-2019-0015Extension of the Gardner exponential equation to represent the hydraulic conductivity curveOttoni Filho Theophilo B.0Lopes Alvarez Marlon G.1Ottoni Marta V.2Amorim Arthur Bernardo Barbosa Dib3Department of Water Resources and Environment, Politechnical School, Federal Univ. of Rio de Janeiro (CT/UFRJ), Ilha do Fundão, Rio de Janeiro, RJ, Brazil. CEP: 21941-909State Environmental Institute (INEA), Av. Venezuela 110, Saúde, Rio de Janeiro, RJ, Brazil. CEP: 20081-312.Department of Hydrology, Geological Survey of Brazil (CPRM), Av. Pasteur, 404, Urca, Rio de Janeiro, RJ, Brazil. CEP: 22290-240Department of Water Resources and Environment, Politechnical School, Federal Univ. of Rio de Janeiro (CT/UFRJ), Ilha do Fundão, Rio de Janeiro, RJ, Brazil. CEP: 21941-909The relative hydraulic conductivity curve Kr(h) = K/Ks is a key variable in soil modeling. This study proposes a model to represent Kr(h), the so-called Gardner dual (GD) model, which extends the classical Gardner exponential model to h values greater than ho, the suction value at the inflection point of the Kr(h) curve in the log-log scale. The goodness of fit of GD using experimental data from UNSODA was compared to that of the MVG [two-parameter (Kro, L) Mualem-van Genuchten] model and a corresponding modified MVG model (MVGm). In 77 soils without evidence of macropore flow, GD reduced the RMSE errors by 64% (0.525 to 0.191) and 29% (0.269 to 0.193) in relation to MVG and MVGm, respectively. In the remaining 76 soils, GD generally was less accurate than MVG and MVGm, since most of these soils presented evidence of macropore flow (dual permeability). GD has three parameters and two degrees of freedom, like MVG. Two of them allow the calculation of the macroscopic capillary length, a parameter from the infiltration literature. The three parameters are highly dependent on the Kr(h) data measurement in a short wet suction range around ho, which is an experimental advantage.https://doi.org/10.2478/johh-2019-0015hydraulic conductivity curvegardner exponential modelmualem-van genuchten model |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Ottoni Filho Theophilo B. Lopes Alvarez Marlon G. Ottoni Marta V. Amorim Arthur Bernardo Barbosa Dib |
spellingShingle |
Ottoni Filho Theophilo B. Lopes Alvarez Marlon G. Ottoni Marta V. Amorim Arthur Bernardo Barbosa Dib Extension of the Gardner exponential equation to represent the hydraulic conductivity curve Journal of Hydrology and Hydromechanics hydraulic conductivity curve gardner exponential model mualem-van genuchten model |
author_facet |
Ottoni Filho Theophilo B. Lopes Alvarez Marlon G. Ottoni Marta V. Amorim Arthur Bernardo Barbosa Dib |
author_sort |
Ottoni Filho Theophilo B. |
title |
Extension of the Gardner exponential equation to represent the hydraulic conductivity curve |
title_short |
Extension of the Gardner exponential equation to represent the hydraulic conductivity curve |
title_full |
Extension of the Gardner exponential equation to represent the hydraulic conductivity curve |
title_fullStr |
Extension of the Gardner exponential equation to represent the hydraulic conductivity curve |
title_full_unstemmed |
Extension of the Gardner exponential equation to represent the hydraulic conductivity curve |
title_sort |
extension of the gardner exponential equation to represent the hydraulic conductivity curve |
publisher |
Sciendo |
series |
Journal of Hydrology and Hydromechanics |
issn |
0042-790X |
publishDate |
2019-12-01 |
description |
The relative hydraulic conductivity curve Kr(h) = K/Ks is a key variable in soil modeling. This study proposes a model to represent Kr(h), the so-called Gardner dual (GD) model, which extends the classical Gardner exponential model to h values greater than ho, the suction value at the inflection point of the Kr(h) curve in the log-log scale. The goodness of fit of GD using experimental data from UNSODA was compared to that of the MVG [two-parameter (Kro, L) Mualem-van Genuchten] model and a corresponding modified MVG model (MVGm). In 77 soils without evidence of macropore flow, GD reduced the RMSE errors by 64% (0.525 to 0.191) and 29% (0.269 to 0.193) in relation to MVG and MVGm, respectively. In the remaining 76 soils, GD generally was less accurate than MVG and MVGm, since most of these soils presented evidence of macropore flow (dual permeability). GD has three parameters and two degrees of freedom, like MVG. Two of them allow the calculation of the macroscopic capillary length, a parameter from the infiltration literature. The three parameters are highly dependent on the Kr(h) data measurement in a short wet suction range around ho, which is an experimental advantage. |
topic |
hydraulic conductivity curve gardner exponential model mualem-van genuchten model |
url |
https://doi.org/10.2478/johh-2019-0015 |
work_keys_str_mv |
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