Geometry and water quality of the unconfined aquifer near the Piracicaba river, Ipatinga/MG, Brazil

Groundwater is the main source of drinking water for the city of Ipatinga/MG, Brazil. However, there is a lack of study about hydrogeology in the region, as well as indications of quality alterations of water resources. The goal is to understand the hydrogeology surrounding the COPASA's Water T...

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Main Authors: Débora Almeida de Oliveira, Paulo Galvão
Format: Article
Language:English
Published: KeAi Communications Co., Ltd. 2019-12-01
Series:HydroResearch
Online Access:http://www.sciencedirect.com/science/article/pii/S2589757819300174
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spelling doaj-bf373359940844c4b53d7bd3e6b561a02021-04-02T11:31:53ZengKeAi Communications Co., Ltd.HydroResearch2589-75782019-12-0123139Geometry and water quality of the unconfined aquifer near the Piracicaba river, Ipatinga/MG, BrazilDébora Almeida de Oliveira0Paulo Galvão1Federal University of Ouro Preto, Department of Geology, Morro do Cruzeiro Campus, Ouro Preto, MG 35400-000, BrazilCorresponding author.; Federal University of Ouro Preto, Department of Geology, Morro do Cruzeiro Campus, Ouro Preto, MG 35400-000, BrazilGroundwater is the main source of drinking water for the city of Ipatinga/MG, Brazil. However, there is a lack of study about hydrogeology in the region, as well as indications of quality alterations of water resources. The goal is to understand the hydrogeology surrounding the COPASA's Water Treatment Plant and the Piracicaba river areas, where the main water supply wells are located. Maps of potentiometric surface, isobaths and isopachs, hydrogeological cross-section, aquifer pumping tests, and physicochemical analysis interpretations were performed. Results indicate the aquifer is unconfined, with high transmissivity and hydraulic conductivity values, which explain the high values of discharge in the wells. The Piracicaba river can be considered as influent, with its water flow converging to the aquifer. Groundwater shows chemical parameters at low levels, according to Brazilian drinking-water quality guidelines, with local presence of aluminum, iron, and manganese, requiring only conventional treatment processes before distribution. Keywords: Hydrogeology, Geometry, Pumping tests, Physicochemical analysishttp://www.sciencedirect.com/science/article/pii/S2589757819300174
collection DOAJ
language English
format Article
sources DOAJ
author Débora Almeida de Oliveira
Paulo Galvão
spellingShingle Débora Almeida de Oliveira
Paulo Galvão
Geometry and water quality of the unconfined aquifer near the Piracicaba river, Ipatinga/MG, Brazil
HydroResearch
author_facet Débora Almeida de Oliveira
Paulo Galvão
author_sort Débora Almeida de Oliveira
title Geometry and water quality of the unconfined aquifer near the Piracicaba river, Ipatinga/MG, Brazil
title_short Geometry and water quality of the unconfined aquifer near the Piracicaba river, Ipatinga/MG, Brazil
title_full Geometry and water quality of the unconfined aquifer near the Piracicaba river, Ipatinga/MG, Brazil
title_fullStr Geometry and water quality of the unconfined aquifer near the Piracicaba river, Ipatinga/MG, Brazil
title_full_unstemmed Geometry and water quality of the unconfined aquifer near the Piracicaba river, Ipatinga/MG, Brazil
title_sort geometry and water quality of the unconfined aquifer near the piracicaba river, ipatinga/mg, brazil
publisher KeAi Communications Co., Ltd.
series HydroResearch
issn 2589-7578
publishDate 2019-12-01
description Groundwater is the main source of drinking water for the city of Ipatinga/MG, Brazil. However, there is a lack of study about hydrogeology in the region, as well as indications of quality alterations of water resources. The goal is to understand the hydrogeology surrounding the COPASA's Water Treatment Plant and the Piracicaba river areas, where the main water supply wells are located. Maps of potentiometric surface, isobaths and isopachs, hydrogeological cross-section, aquifer pumping tests, and physicochemical analysis interpretations were performed. Results indicate the aquifer is unconfined, with high transmissivity and hydraulic conductivity values, which explain the high values of discharge in the wells. The Piracicaba river can be considered as influent, with its water flow converging to the aquifer. Groundwater shows chemical parameters at low levels, according to Brazilian drinking-water quality guidelines, with local presence of aluminum, iron, and manganese, requiring only conventional treatment processes before distribution. Keywords: Hydrogeology, Geometry, Pumping tests, Physicochemical analysis
url http://www.sciencedirect.com/science/article/pii/S2589757819300174
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