Hydrogeochemistry as a tool for the assessment of aquifers in gaps of lithological well profiles
The study area is located 30 km north of Belo Horizonte, and includes the entire Lagoa Santa Karst Environmental Protection Area and its surroundings. It represents an area of 505 km². The karst-fissure aquifer, developed in carbonated rocks of inferior (impure) and superior (pure) members of Sete L...
| Authors: | , , |
|---|---|
| Format: | article |
| Status: | Published version |
| Publication Date: | 2020 |
| Country: | Brasil |
| Institution: | Associação Brasileira de Águas Subterrâneas |
| Repository: | Águas Subterrâneas (São Paulo. Online) |
| Language: | Portuguese |
| OAI Identifier: | oai:ojs.aguassubterraneas.abas.org:article/29764 |
| Online Access: | https://aguassubterraneas.abas.org/asubterraneas/article/view/29764 |
| Access Level: | Open access |
| Keyword: | EPA Lagoa Santa Karst. Hydrogeochemistry. Karst Aquifers. Statistic. APA Carste de Lagoa Santa. Hidrogeoquímica. Aquíferos cárstico-fissurais. Estatística. |
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Hydrogeochemistry as a tool for the assessment of aquifers in gaps of lithological well profilesHidrogeoquímica como ferramenta para o reconhecimento de aquíferos em lacunas de perfis litológicos de poços tubularesEPA Lagoa Santa Karst. Hydrogeochemistry. Karst Aquifers. Statistic.APA Carste de Lagoa Santa. Hidrogeoquímica. Aquíferos cárstico-fissurais. Estatística.The study area is located 30 km north of Belo Horizonte, and includes the entire Lagoa Santa Karst Environmental Protection Area and its surroundings. It represents an area of 505 km². The karst-fissure aquifer, developed in carbonated rocks of inferior (impure) and superior (pure) members of Sete Lagoas Formation – Pedro Leopoldo and Lagoa Santa respectively, is the most exploited. The other aquifers, which are comparably less explored, are the ones in metapelites of Serra de Santa Helena Formation, granites of Belo Horizonte Complex and granular overburden. Despite the large number of operating tube wells in this area, lithological description from rock loggings is precarious, which compromises their use in hydrogeological studies. In order to overcome this problem, hydrochemical results obtained and available lithological data were used. These are sourced from 21 sub-superficial and 85 deep circulation water samples. Piper and Stiff diagrams and statistical treatment of data, including Boxplots and Cluster analysis, were used in the study to classify groundwater according to its source. The classification proved to be effective, especially in the separation of silica and carbonate units. Further analysis can emphasize difference between both carbonated units.A área estudada, situada 30 km a norte de Belo Horizonte, engloba toda Área de Proteção Ambiental Carste de Lagoa Santa e arredores, perfazendo 505 km². Os aquíferos cárstico-fissurais, desenvolvidos nas rochas carbonáticas dos membros inferior (impuro) e superior (puro) da Formação Sete Lagoas - Pedro Leopoldo e Lagoa Santa, respectivamente, são mais explorados, seguidos dos fissurais em metapelitos da Formação Serra de Santa Helena, granitos do embasamento do Complexo Belo Horizonte, e granulares de cobertura. Apesar do grande número de poços tubulares operantes, ocorre grande precariedade de descrição litológica nos perfis desses poços, comprometendo sua utilização. Visando ladear esse problema, segundo resultados hidroquímicos obtidos e dados litológicos disponíveis, classificou-se, por unidades aquíferas, 21 amostras de água sub-superficial, e 85 de circulação profunda. A divisão foi avaliada por diagramas de Piper e Stiff e tratamento estatístico dos dados, incluindo Boxplots e análise de Cluster. A classificação mostrou-se eficaz, especialmente na separação das unidades silicáticas e carbonáticas. A distinção entre as duas unidades carbonáticas pode ser ampliada com análises complementares.ABAS - Associação Brasileira de Águas Subterrâneas2020-07-09info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://aguassubterraneas.abas.org/asubterraneas/article/view/2976410.14295/ras.v34i2.29764Águas Subterrâneas; v. 34 n. 2 (2020): REVISTA ÁGUAS SUBTERRÂNEAS; 204-2202179-97840101-7004reponame:Águas Subterrâneas (São Paulo. Online)instname:Associação Brasileira de Águas Subterrâneasinstacron:ABASporhttps://aguassubterraneas.abas.org/asubterraneas/article/view/29764/19316Copyright (c) 2020 Águas Subterrâneasinfo:eu-repo/semantics/openAccessVieira, Luisa Costa MartinsVelasquez, Leila Nunes MenegasseBorba, Ricardo Perobelli2020-07-25T01:43:13Zoai:ojs.aguassubterraneas.abas.org:article/29764Revistahttps://aguassubterraneas.abas.org/asubterraneas/ONGhttps://aguassubterraneas.abas.org/asubterraneas/oaihidropaulo@gmail.com2179-97840101-7004opendoar:2020-07-25T01:43:13Águas Subterrâneas (São Paulo. Online) - Associação Brasileira de Águas Subterrâneasfalse |
| dc.title.none.fl_str_mv |
Hydrogeochemistry as a tool for the assessment of aquifers in gaps of lithological well profiles Hidrogeoquímica como ferramenta para o reconhecimento de aquíferos em lacunas de perfis litológicos de poços tubulares |
| title |
Hydrogeochemistry as a tool for the assessment of aquifers in gaps of lithological well profiles |
| spellingShingle |
Hydrogeochemistry as a tool for the assessment of aquifers in gaps of lithological well profiles Vieira, Luisa Costa Martins EPA Lagoa Santa Karst. Hydrogeochemistry. Karst Aquifers. Statistic. APA Carste de Lagoa Santa. Hidrogeoquímica. Aquíferos cárstico-fissurais. Estatística. |
| title_short |
Hydrogeochemistry as a tool for the assessment of aquifers in gaps of lithological well profiles |
| title_full |
Hydrogeochemistry as a tool for the assessment of aquifers in gaps of lithological well profiles |
| title_fullStr |
Hydrogeochemistry as a tool for the assessment of aquifers in gaps of lithological well profiles |
| title_full_unstemmed |
Hydrogeochemistry as a tool for the assessment of aquifers in gaps of lithological well profiles |
| title_sort |
Hydrogeochemistry as a tool for the assessment of aquifers in gaps of lithological well profiles |
| dc.creator.none.fl_str_mv |
Vieira, Luisa Costa Martins Velasquez, Leila Nunes Menegasse Borba, Ricardo Perobelli |
| author |
Vieira, Luisa Costa Martins |
| author_facet |
Vieira, Luisa Costa Martins Velasquez, Leila Nunes Menegasse Borba, Ricardo Perobelli |
| author_role |
author |
| author2 |
Velasquez, Leila Nunes Menegasse Borba, Ricardo Perobelli |
| author2_role |
author author |
| dc.subject.por.fl_str_mv |
EPA Lagoa Santa Karst. Hydrogeochemistry. Karst Aquifers. Statistic. APA Carste de Lagoa Santa. Hidrogeoquímica. Aquíferos cárstico-fissurais. Estatística. |
| topic |
EPA Lagoa Santa Karst. Hydrogeochemistry. Karst Aquifers. Statistic. APA Carste de Lagoa Santa. Hidrogeoquímica. Aquíferos cárstico-fissurais. Estatística. |
| description |
The study area is located 30 km north of Belo Horizonte, and includes the entire Lagoa Santa Karst Environmental Protection Area and its surroundings. It represents an area of 505 km². The karst-fissure aquifer, developed in carbonated rocks of inferior (impure) and superior (pure) members of Sete Lagoas Formation – Pedro Leopoldo and Lagoa Santa respectively, is the most exploited. The other aquifers, which are comparably less explored, are the ones in metapelites of Serra de Santa Helena Formation, granites of Belo Horizonte Complex and granular overburden. Despite the large number of operating tube wells in this area, lithological description from rock loggings is precarious, which compromises their use in hydrogeological studies. In order to overcome this problem, hydrochemical results obtained and available lithological data were used. These are sourced from 21 sub-superficial and 85 deep circulation water samples. Piper and Stiff diagrams and statistical treatment of data, including Boxplots and Cluster analysis, were used in the study to classify groundwater according to its source. The classification proved to be effective, especially in the separation of silica and carbonate units. Further analysis can emphasize difference between both carbonated units. |
| publishDate |
2020 |
| dc.date.none.fl_str_mv |
2020-07-09 |
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info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion |
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article |
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publishedVersion |
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https://aguassubterraneas.abas.org/asubterraneas/article/view/29764 10.14295/ras.v34i2.29764 |
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https://aguassubterraneas.abas.org/asubterraneas/article/view/29764 |
| identifier_str_mv |
10.14295/ras.v34i2.29764 |
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por |
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por |
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https://aguassubterraneas.abas.org/asubterraneas/article/view/29764/19316 |
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Copyright (c) 2020 Águas Subterrâneas info:eu-repo/semantics/openAccess |
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Copyright (c) 2020 Águas Subterrâneas |
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openAccess |
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application/pdf |
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ABAS - Associação Brasileira de Águas Subterrâneas |
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ABAS - Associação Brasileira de Águas Subterrâneas |
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Águas Subterrâneas; v. 34 n. 2 (2020): REVISTA ÁGUAS SUBTERRÂNEAS; 204-220 2179-9784 0101-7004 reponame:Águas Subterrâneas (São Paulo. Online) instname:Associação Brasileira de Águas Subterrâneas instacron:ABAS |
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Águas Subterrâneas (São Paulo. Online) - Associação Brasileira de Águas Subterrâneas |
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