Comparison of pedotransfer functions for the determination of saturated hydraulic conductivity coefficient

On one hand, direct methods of measurement of saturated hydraulic conductivity coefficient are time consuming, and on the other hand, laboratory methods are cost consuming. That is why the popularity of empirical methods has increased. Their main advantages are speed of calculations and low costs. C...

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Main Authors: Ryczek Marek, Kruk Edyta, Malec Magdalena, Klatka Sławomir
Format: Article
Language:English
Published: Sciendo 2017-03-01
Series:Environmental Protection and Natural Resources
Subjects:
Online Access:https://doi.org/10.1515/oszn-2017-0005
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author Ryczek Marek
Kruk Edyta
Malec Magdalena
Klatka Sławomir
author_facet Ryczek Marek
Kruk Edyta
Malec Magdalena
Klatka Sławomir
author_sort Ryczek Marek
collection DOAJ
description On one hand, direct methods of measurement of saturated hydraulic conductivity coefficient are time consuming, and on the other hand, laboratory methods are cost consuming. That is why the popularity of empirical methods has increased. Their main advantages are speed of calculations and low costs. Comparison of various empirical methods (pedotransfer functions) for the determination of saturated hydraulic conductivity coefficient was the purpose of this work. The methods used were Shepard’s, Hazen’s, USBR (United States Bureau of Reclamation), Saxton et al.’s, Kozeny–Carman’s, Krüger’s, Terzaghi’s, Chapuis’s, Sheelheim’s, Chapuis’, and NAVFAC (Naval Facilities Engineering Command) methods. Calculations were carried out for the soil samples of differential texture. The obtained results shows the methods used for the determination of permeability coefficient differ considerably. Mean values obtained by analysed methods fluctuated between 0.0006 and 12.0 m·day−1. The results of calculations by the chosen methods were compared with the results of the laboratory method. The best compatibility with laboratory method was obtained by using the Terzaghi method.
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spelling doaj.art-2af564ba42b043e2afea4c0ebd422a2f2022-12-21T23:30:21ZengSciendoEnvironmental Protection and Natural Resources2353-85892017-03-01281253010.1515/oszn-2017-0005oszn-2017-0005Comparison of pedotransfer functions for the determination of saturated hydraulic conductivity coefficientRyczek Marek0Kruk Edyta1Malec Magdalena2Klatka Sławomir3Department of Land Reclamation and Environmental Development, Agriculture University of Krakow, Mickiewicza 24/28 St, 30-059 Krakow, PolandDepartment of Land Reclamation and Environmental Development, Agriculture University of Krakow, Mickiewicza 24/28 St, 30-059 Krakow, PolandDepartment of Land Reclamation and Environmental Development, Agriculture University of Krakow, Mickiewicza 24/28 St, 30-059 Krakow, PolandDepartment of Land Reclamation and Environmental Development, Agriculture University of Krakow, Mickiewicza 24/28 St, 30-059 Krakow, PolandOn one hand, direct methods of measurement of saturated hydraulic conductivity coefficient are time consuming, and on the other hand, laboratory methods are cost consuming. That is why the popularity of empirical methods has increased. Their main advantages are speed of calculations and low costs. Comparison of various empirical methods (pedotransfer functions) for the determination of saturated hydraulic conductivity coefficient was the purpose of this work. The methods used were Shepard’s, Hazen’s, USBR (United States Bureau of Reclamation), Saxton et al.’s, Kozeny–Carman’s, Krüger’s, Terzaghi’s, Chapuis’s, Sheelheim’s, Chapuis’, and NAVFAC (Naval Facilities Engineering Command) methods. Calculations were carried out for the soil samples of differential texture. The obtained results shows the methods used for the determination of permeability coefficient differ considerably. Mean values obtained by analysed methods fluctuated between 0.0006 and 12.0 m·day−1. The results of calculations by the chosen methods were compared with the results of the laboratory method. The best compatibility with laboratory method was obtained by using the Terzaghi method.https://doi.org/10.1515/oszn-2017-0005saturated hydraulic conductivitypedotransfer functions
spellingShingle Ryczek Marek
Kruk Edyta
Malec Magdalena
Klatka Sławomir
Comparison of pedotransfer functions for the determination of saturated hydraulic conductivity coefficient
Environmental Protection and Natural Resources
saturated hydraulic conductivity
pedotransfer functions
title Comparison of pedotransfer functions for the determination of saturated hydraulic conductivity coefficient
title_full Comparison of pedotransfer functions for the determination of saturated hydraulic conductivity coefficient
title_fullStr Comparison of pedotransfer functions for the determination of saturated hydraulic conductivity coefficient
title_full_unstemmed Comparison of pedotransfer functions for the determination of saturated hydraulic conductivity coefficient
title_short Comparison of pedotransfer functions for the determination of saturated hydraulic conductivity coefficient
title_sort comparison of pedotransfer functions for the determination of saturated hydraulic conductivity coefficient
topic saturated hydraulic conductivity
pedotransfer functions
url https://doi.org/10.1515/oszn-2017-0005
work_keys_str_mv AT ryczekmarek comparisonofpedotransferfunctionsforthedeterminationofsaturatedhydraulicconductivitycoefficient
AT krukedyta comparisonofpedotransferfunctionsforthedeterminationofsaturatedhydraulicconductivitycoefficient
AT malecmagdalena comparisonofpedotransferfunctionsforthedeterminationofsaturatedhydraulicconductivitycoefficient
AT klatkasławomir comparisonofpedotransferfunctionsforthedeterminationofsaturatedhydraulicconductivitycoefficient