Evaluation of infiltration models for mineral soils with different land uses in the tropics

The aims of this study were to evaluate five infiltration models for mineral soils in the tropics with different land use types, such as settlements, plantations, rice fields, and forests. The infiltration models evaluated were Green–Ampt, Kostiakov, Kostiakov–Lewis, Philip, and Horton. The research...

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Main Authors: Suryoputro Nugroho, Suhardjono, Soetopo Widandi, Suhartanto Ery S., Limantara Lily M.
Format: Article
Language:English
Published: Polish Academy of Sciences 2018-06-01
Series:Journal of Water and Land Development
Subjects:
Online Access:http://www.degruyter.com/view/j/jwld.2018.37.issue-1/jwld-2018-0034/jwld-2018-0034.xml?format=INT
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author Suryoputro Nugroho
Suhardjono
Soetopo Widandi
Suhartanto Ery S.
Limantara Lily M.
author_facet Suryoputro Nugroho
Suhardjono
Soetopo Widandi
Suhartanto Ery S.
Limantara Lily M.
author_sort Suryoputro Nugroho
collection DOAJ
description The aims of this study were to evaluate five infiltration models for mineral soils in the tropics with different land use types, such as settlements, plantations, rice fields, and forests. The infiltration models evaluated were Green–Ampt, Kostiakov, Kostiakov–Lewis, Philip, and Horton. The research was conducted at the Amprong watershed, Malang, Indonesia. The infiltration rate of the thirteen soil samples was analysed. The infiltration was tested using Turf-Tech infiltrometer. Moreover, each soil sample was tested in terms of the bulk density, specific gravity, porosity, soil moisture, and soil texture. The results of the study indicate that there is no significant difference (α = 5%) in the infiltration rate among the five models of infiltration. The infiltration rate in the study site was considered fast. Three models exhibiting the best performance are Kostiakov, Kostiakov–Lewis, and Horton model, respectively. The highest infiltration rate occurred in the forest land use while the lowest occurred in the rice field land use. The results of this study suggest that the infiltration model parameters correlate closely with the initial infiltration rate (fo) and the final infiltration rate (fc). In other words there is a correlation between the soil's ability to absorb water (representing the capillary force or horizontal flow) at the beginning of the infiltration (fo) and the gravity or the vertical flow upon reaching the final infiltration rate (fc).
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spelling doaj.art-f9847b02bf0c4b12a38e8b58124df9772023-08-02T07:40:33ZengPolish Academy of SciencesJournal of Water and Land Development2083-45352018-06-0137115316010.2478/jwld-2018-0034jwld-2018-0034Evaluation of infiltration models for mineral soils with different land uses in the tropicsSuryoputro Nugroho0Suhardjono1Soetopo Widandi2Suhartanto Ery S.3Limantara Lily M.4State University of Malang, Faculty of Engineering, Department of Civil Engineering, Malang, East Java Province, IndonesiaUniversity of Brawijaya, Faculty of Engineering, Department of Water Resources, Jl. Mt Haryono No 167, 65141Malang, East Java Province, IndonesiaUniversity of Brawijaya, Faculty of Engineering, Department of Water Resources, Jl. Mt Haryono No 167, 65141Malang, East Java Province, IndonesiaUniversity of Brawijaya, Faculty of Engineering, Department of Water Resources, Jl. Mt Haryono No 167, 65141Malang, East Java Province, IndonesiaUniversity of Brawijaya, Faculty of Engineering, Department of Water Resources, Jl. Mt Haryono No 167, 65141Malang, East Java Province, IndonesiaThe aims of this study were to evaluate five infiltration models for mineral soils in the tropics with different land use types, such as settlements, plantations, rice fields, and forests. The infiltration models evaluated were Green–Ampt, Kostiakov, Kostiakov–Lewis, Philip, and Horton. The research was conducted at the Amprong watershed, Malang, Indonesia. The infiltration rate of the thirteen soil samples was analysed. The infiltration was tested using Turf-Tech infiltrometer. Moreover, each soil sample was tested in terms of the bulk density, specific gravity, porosity, soil moisture, and soil texture. The results of the study indicate that there is no significant difference (α = 5%) in the infiltration rate among the five models of infiltration. The infiltration rate in the study site was considered fast. Three models exhibiting the best performance are Kostiakov, Kostiakov–Lewis, and Horton model, respectively. The highest infiltration rate occurred in the forest land use while the lowest occurred in the rice field land use. The results of this study suggest that the infiltration model parameters correlate closely with the initial infiltration rate (fo) and the final infiltration rate (fc). In other words there is a correlation between the soil's ability to absorb water (representing the capillary force or horizontal flow) at the beginning of the infiltration (fo) and the gravity or the vertical flow upon reaching the final infiltration rate (fc).http://www.degruyter.com/view/j/jwld.2018.37.issue-1/jwld-2018-0034/jwld-2018-0034.xml?format=INTinfiltration modelsland usemineral soiltropical climate
spellingShingle Suryoputro Nugroho
Suhardjono
Soetopo Widandi
Suhartanto Ery S.
Limantara Lily M.
Evaluation of infiltration models for mineral soils with different land uses in the tropics
Journal of Water and Land Development
infiltration models
land use
mineral soil
tropical climate
title Evaluation of infiltration models for mineral soils with different land uses in the tropics
title_full Evaluation of infiltration models for mineral soils with different land uses in the tropics
title_fullStr Evaluation of infiltration models for mineral soils with different land uses in the tropics
title_full_unstemmed Evaluation of infiltration models for mineral soils with different land uses in the tropics
title_short Evaluation of infiltration models for mineral soils with different land uses in the tropics
title_sort evaluation of infiltration models for mineral soils with different land uses in the tropics
topic infiltration models
land use
mineral soil
tropical climate
url http://www.degruyter.com/view/j/jwld.2018.37.issue-1/jwld-2018-0034/jwld-2018-0034.xml?format=INT
work_keys_str_mv AT suryoputronugroho evaluationofinfiltrationmodelsformineralsoilswithdifferentlandusesinthetropics
AT suhardjono evaluationofinfiltrationmodelsformineralsoilswithdifferentlandusesinthetropics
AT soetopowidandi evaluationofinfiltrationmodelsformineralsoilswithdifferentlandusesinthetropics
AT suhartantoerys evaluationofinfiltrationmodelsformineralsoilswithdifferentlandusesinthetropics
AT limantaralilym evaluationofinfiltrationmodelsformineralsoilswithdifferentlandusesinthetropics