Spatial and Temporal Potential Groundwater Recharge: the Case of the Doce River Basin, Brazil

Detalhes bibliográficos
Autor(a) principal: Souza,Eliana de
Data de Publicação: 2019
Outros Autores: Pontes,Lucas Machado, Fernandes Filho,Elpídio Inácio, Schaefer,Carlos Ernesto Goncalves Reynaud, Santos,Eliana Elizabet dos
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Revista Brasileira de Ciência do Solo (Online)
Texto Completo: http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0100-06832019000100501
Resumo: ABSTRACT: Little is known about the groundwater recharge potential of weathered tropical catchments, where increasing water uptake is widespread to meet various water demands. This study aimed to estimate the volume of groundwater recharge of the Doce River Basin, Minas Gerais, Brazil. The BALSEQ model was applied to calculate the water balance over a period of two years (2007-2009). Evapotranspiration, runoff, and potential groundwater recharge (PGR) were calculated, using daily data on rainfall, potential evapotranspiration, and plant-available water. A soil survey was undertaken for all major soils occurring in the basin. Soils samples were used to determine hydraulic conductivity, bulk density, and water content at field capacity and at the permanent wilting point. Vegetation data were obtained from the literature and used to determine the following parameters: canopy interception, crop coefficient, and root depth. The estimated groundwater was spatially predicted using the Random Forests model with digital elevation, vegetation index, pedological, lithological, and climate maps. During the two years, an average of 32 % of rainfall was converted to groundwater. Annually, the percent of rainwater converted to groundwater varied between 27 and 48 % for all soil classes, highlighting the great temporal variability. The spatial prediction showed a volume of approximately 17,484 and 35,410 m3 of rainfall being converted to groundwater for the first and second year, respectively. The BALSEQ model showed a feasibility for the water balance calculation and can be reapplied for updating the groundwater maps of the Doce River Basin. These maps could then be used to guide land use planning programs, with the aim to protect water resources.
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spelling Spatial and Temporal Potential Groundwater Recharge: the Case of the Doce River Basin, Brazilaquiferinfiltrationpotential rechargeRandom Forests Modelwater balanceABSTRACT: Little is known about the groundwater recharge potential of weathered tropical catchments, where increasing water uptake is widespread to meet various water demands. This study aimed to estimate the volume of groundwater recharge of the Doce River Basin, Minas Gerais, Brazil. The BALSEQ model was applied to calculate the water balance over a period of two years (2007-2009). Evapotranspiration, runoff, and potential groundwater recharge (PGR) were calculated, using daily data on rainfall, potential evapotranspiration, and plant-available water. A soil survey was undertaken for all major soils occurring in the basin. Soils samples were used to determine hydraulic conductivity, bulk density, and water content at field capacity and at the permanent wilting point. Vegetation data were obtained from the literature and used to determine the following parameters: canopy interception, crop coefficient, and root depth. The estimated groundwater was spatially predicted using the Random Forests model with digital elevation, vegetation index, pedological, lithological, and climate maps. During the two years, an average of 32 % of rainfall was converted to groundwater. Annually, the percent of rainwater converted to groundwater varied between 27 and 48 % for all soil classes, highlighting the great temporal variability. The spatial prediction showed a volume of approximately 17,484 and 35,410 m3 of rainfall being converted to groundwater for the first and second year, respectively. The BALSEQ model showed a feasibility for the water balance calculation and can be reapplied for updating the groundwater maps of the Doce River Basin. These maps could then be used to guide land use planning programs, with the aim to protect water resources.Sociedade Brasileira de Ciência do Solo2019-01-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersiontext/htmlhttp://old.scielo.br/scielo.php?script=sci_arttext&pid=S0100-06832019000100501Revista Brasileira de Ciência do Solo v.43 2019reponame:Revista Brasileira de Ciência do Solo (Online)instname:Sociedade Brasileira de Ciência do Solo (SBCS)instacron:SBCS10.1590/18069657rbcs20180010info:eu-repo/semantics/openAccessSouza,Eliana dePontes,Lucas MachadoFernandes Filho,Elpídio InácioSchaefer,Carlos Ernesto Goncalves ReynaudSantos,Eliana Elizabet doseng2019-08-13T00:00:00Zoai:scielo:S0100-06832019000100501Revistahttp://www.scielo.br/scielo.php?script=sci_serial&pid=0100-0683&lng=es&nrm=isohttps://old.scielo.br/oai/scielo-oai.php||sbcs@ufv.br1806-96570100-0683opendoar:2019-08-13T00:00Revista Brasileira de Ciência do Solo (Online) - Sociedade Brasileira de Ciência do Solo (SBCS)false
dc.title.none.fl_str_mv Spatial and Temporal Potential Groundwater Recharge: the Case of the Doce River Basin, Brazil
title Spatial and Temporal Potential Groundwater Recharge: the Case of the Doce River Basin, Brazil
spellingShingle Spatial and Temporal Potential Groundwater Recharge: the Case of the Doce River Basin, Brazil
Souza,Eliana de
aquifer
infiltration
potential recharge
Random Forests Model
water balance
title_short Spatial and Temporal Potential Groundwater Recharge: the Case of the Doce River Basin, Brazil
title_full Spatial and Temporal Potential Groundwater Recharge: the Case of the Doce River Basin, Brazil
title_fullStr Spatial and Temporal Potential Groundwater Recharge: the Case of the Doce River Basin, Brazil
title_full_unstemmed Spatial and Temporal Potential Groundwater Recharge: the Case of the Doce River Basin, Brazil
title_sort Spatial and Temporal Potential Groundwater Recharge: the Case of the Doce River Basin, Brazil
author Souza,Eliana de
author_facet Souza,Eliana de
Pontes,Lucas Machado
Fernandes Filho,Elpídio Inácio
Schaefer,Carlos Ernesto Goncalves Reynaud
Santos,Eliana Elizabet dos
author_role author
author2 Pontes,Lucas Machado
Fernandes Filho,Elpídio Inácio
Schaefer,Carlos Ernesto Goncalves Reynaud
Santos,Eliana Elizabet dos
author2_role author
author
author
author
dc.contributor.author.fl_str_mv Souza,Eliana de
Pontes,Lucas Machado
Fernandes Filho,Elpídio Inácio
Schaefer,Carlos Ernesto Goncalves Reynaud
Santos,Eliana Elizabet dos
dc.subject.por.fl_str_mv aquifer
infiltration
potential recharge
Random Forests Model
water balance
topic aquifer
infiltration
potential recharge
Random Forests Model
water balance
description ABSTRACT: Little is known about the groundwater recharge potential of weathered tropical catchments, where increasing water uptake is widespread to meet various water demands. This study aimed to estimate the volume of groundwater recharge of the Doce River Basin, Minas Gerais, Brazil. The BALSEQ model was applied to calculate the water balance over a period of two years (2007-2009). Evapotranspiration, runoff, and potential groundwater recharge (PGR) were calculated, using daily data on rainfall, potential evapotranspiration, and plant-available water. A soil survey was undertaken for all major soils occurring in the basin. Soils samples were used to determine hydraulic conductivity, bulk density, and water content at field capacity and at the permanent wilting point. Vegetation data were obtained from the literature and used to determine the following parameters: canopy interception, crop coefficient, and root depth. The estimated groundwater was spatially predicted using the Random Forests model with digital elevation, vegetation index, pedological, lithological, and climate maps. During the two years, an average of 32 % of rainfall was converted to groundwater. Annually, the percent of rainwater converted to groundwater varied between 27 and 48 % for all soil classes, highlighting the great temporal variability. The spatial prediction showed a volume of approximately 17,484 and 35,410 m3 of rainfall being converted to groundwater for the first and second year, respectively. The BALSEQ model showed a feasibility for the water balance calculation and can be reapplied for updating the groundwater maps of the Doce River Basin. These maps could then be used to guide land use planning programs, with the aim to protect water resources.
publishDate 2019
dc.date.none.fl_str_mv 2019-01-01
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
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dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv 10.1590/18069657rbcs20180010
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dc.publisher.none.fl_str_mv Sociedade Brasileira de Ciência do Solo
publisher.none.fl_str_mv Sociedade Brasileira de Ciência do Solo
dc.source.none.fl_str_mv Revista Brasileira de Ciência do Solo v.43 2019
reponame:Revista Brasileira de Ciência do Solo (Online)
instname:Sociedade Brasileira de Ciência do Solo (SBCS)
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instname_str Sociedade Brasileira de Ciência do Solo (SBCS)
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institution SBCS
reponame_str Revista Brasileira de Ciência do Solo (Online)
collection Revista Brasileira de Ciência do Solo (Online)
repository.name.fl_str_mv Revista Brasileira de Ciência do Solo (Online) - Sociedade Brasileira de Ciência do Solo (SBCS)
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