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...
Main Authors: | , , , |
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Format: | Article |
Language: | English |
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Sciendo
2017-03-01
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Series: | Environmental Protection and Natural Resources |
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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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institution | Directory Open Access Journal |
issn | 2353-8589 |
language | English |
last_indexed | 2024-12-13T21:48:16Z |
publishDate | 2017-03-01 |
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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 |