Hydrological simulation in a basin of typical tropical climate and soil using the SWAT Model Part II: Simulation of hydrological variables and soil use scenarios

Study region: The study was developed for the Pomba river basin, which is located in southeast region of Brazil in the continent of South America. Study focus: Hydrological simulation may be used to estimate the water availability, flood streamflows and the basin's hydrological response due to...

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Main Authors: Donizete dos R. Pereira, Mauro A. Martinez, Demetrius D. da Silva, Fernando F. Pruski
Format: Article
Language:English
Published: Elsevier 2016-03-01
Series:Journal of Hydrology: Regional Studies
Online Access:http://www.sciencedirect.com/science/article/pii/S2214581815001238
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spelling doaj-c2721db14cf8403ab2d758d675d2731c2020-11-25T00:14:37ZengElsevierJournal of Hydrology: Regional Studies2214-58182016-03-015149163Hydrological simulation in a basin of typical tropical climate and soil using the SWAT Model Part II: Simulation of hydrological variables and soil use scenariosDonizete dos R. Pereira0Mauro A. Martinez1Demetrius D. da Silva2Fernando F. Pruski3Institute of Agrarian Sciences—UFV/Campus Florestal, Rodovia LMG 818, km 6, CEP 35, Florestal, MG, Brazil; Corresponding author.Department of Agricultural Engineering—DEA/UFV, Avenida PH Rolfs, Campus Universitário, CEP 36, Viçosa, MG, BrazilDepartment of Agricultural Engineering—DEA/UFV, Avenida PH Rolfs, Campus Universitário, CEP 36, Viçosa, MG, BrazilDepartment of Agricultural Engineering—DEA/UFV, Avenida PH Rolfs, Campus Universitário, CEP 36, Viçosa, MG, BrazilStudy region: The study was developed for the Pomba river basin, which is located in southeast region of Brazil in the continent of South America. Study focus: Hydrological simulation may be used to estimate the water availability, flood streamflows and the basin's hydrological response due to changes in soil use. Thus, aimed to apply the SWAT model, version 2005, to simulate (i) the minimum and maximum annual daily streamflows associated to different return times, (ii) minimum reference streamflows for water rights, and (iii) scenarios of changes in soil use. Were simulated the following scenarios of soil use: S1—preservation, considering the permanent preservation areas (PPAs); S2—reforestation expansion and S3—agricultural expansion, considering the replacement of 10% of the basin's total area covered with pastures for eucalyptus and crops, respectively. The current use (S0) being employed as the baseline. New hydrological insights for the region: It was observed that the values of maximum and minimum annual daily streamflows with different return times, and of minimum reference streamflows for water rights simulated by the SWAT did not statistically differ from the values observed according to T-test at 5% probability level. When assessing the effects of changes in soil use, a mean annual reduction in runoff from 13.6, 4.0, and 6.5 mm was observed for scenarios S1, S2, and S3, respectively. Keywords: Maximum streamflows, Minimum streamflows, Reference streamflows, Soil use and cover, Annual runoff, Basinhttp://www.sciencedirect.com/science/article/pii/S2214581815001238
collection DOAJ
language English
format Article
sources DOAJ
author Donizete dos R. Pereira
Mauro A. Martinez
Demetrius D. da Silva
Fernando F. Pruski
spellingShingle Donizete dos R. Pereira
Mauro A. Martinez
Demetrius D. da Silva
Fernando F. Pruski
Hydrological simulation in a basin of typical tropical climate and soil using the SWAT Model Part II: Simulation of hydrological variables and soil use scenarios
Journal of Hydrology: Regional Studies
author_facet Donizete dos R. Pereira
Mauro A. Martinez
Demetrius D. da Silva
Fernando F. Pruski
author_sort Donizete dos R. Pereira
title Hydrological simulation in a basin of typical tropical climate and soil using the SWAT Model Part II: Simulation of hydrological variables and soil use scenarios
title_short Hydrological simulation in a basin of typical tropical climate and soil using the SWAT Model Part II: Simulation of hydrological variables and soil use scenarios
title_full Hydrological simulation in a basin of typical tropical climate and soil using the SWAT Model Part II: Simulation of hydrological variables and soil use scenarios
title_fullStr Hydrological simulation in a basin of typical tropical climate and soil using the SWAT Model Part II: Simulation of hydrological variables and soil use scenarios
title_full_unstemmed Hydrological simulation in a basin of typical tropical climate and soil using the SWAT Model Part II: Simulation of hydrological variables and soil use scenarios
title_sort hydrological simulation in a basin of typical tropical climate and soil using the swat model part ii: simulation of hydrological variables and soil use scenarios
publisher Elsevier
series Journal of Hydrology: Regional Studies
issn 2214-5818
publishDate 2016-03-01
description Study region: The study was developed for the Pomba river basin, which is located in southeast region of Brazil in the continent of South America. Study focus: Hydrological simulation may be used to estimate the water availability, flood streamflows and the basin's hydrological response due to changes in soil use. Thus, aimed to apply the SWAT model, version 2005, to simulate (i) the minimum and maximum annual daily streamflows associated to different return times, (ii) minimum reference streamflows for water rights, and (iii) scenarios of changes in soil use. Were simulated the following scenarios of soil use: S1—preservation, considering the permanent preservation areas (PPAs); S2—reforestation expansion and S3—agricultural expansion, considering the replacement of 10% of the basin's total area covered with pastures for eucalyptus and crops, respectively. The current use (S0) being employed as the baseline. New hydrological insights for the region: It was observed that the values of maximum and minimum annual daily streamflows with different return times, and of minimum reference streamflows for water rights simulated by the SWAT did not statistically differ from the values observed according to T-test at 5% probability level. When assessing the effects of changes in soil use, a mean annual reduction in runoff from 13.6, 4.0, and 6.5 mm was observed for scenarios S1, S2, and S3, respectively. Keywords: Maximum streamflows, Minimum streamflows, Reference streamflows, Soil use and cover, Annual runoff, Basin
url http://www.sciencedirect.com/science/article/pii/S2214581815001238
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