Relationship between hydrochemical patterns and depths of water bearing frac-tures in acid volcanic rocks from serra geral formation
This study aimed to evaluate the existence of different hydrochemical patterns of fractured aquifers of the Serra Geral Aquifer System (SGAS), relating these patterns with the depths of the fractures bearing water in the city of Carlos Barbosa-RS. Hydrochemical information from samples collected in...
| Autores: | , , , |
|---|---|
| Formato: | artículo |
| Estado: | Versión publicada |
| Fecha de publicación: | 2016 |
| País: | Brasil |
| Recursos: | Associação Brasileira de Águas Subterrâneas |
| Repositorio: | Águas Subterrâneas (São Paulo. Online) |
| Idioma: | portugués |
| OAI Identifier: | oai:ojs.aguassubterraneas.abas.org:article/28585 |
| Acesso em linha: | https://aguassubterraneas.abas.org/asubterraneas/article/view/28585 |
| Access Level: | acceso abierto |
| Palavra-chave: | Hydrochemical. Fractured aquifers. Serra Geral Aquifer System Hidroquímica. Aquíferos fraturados. Sistema Aquífero Serra Geral. |
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Relationship between hydrochemical patterns and depths of water bearing frac-tures in acid volcanic rocks from serra geral formationRelação entre padrões hidroquímicos e as profundidades de fraturas com entra-das de água em rochas vulcânicas ácidas da formação serra geralHydrochemical. Fractured aquifers. Serra Geral Aquifer SystemHidroquímica. Aquíferos fraturados. Sistema Aquífero Serra Geral.This study aimed to evaluate the existence of different hydrochemical patterns of fractured aquifers of the Serra Geral Aquifer System (SGAS), relating these patterns with the depths of the fractures bearing water in the city of Carlos Barbosa-RS. Hydrochemical information from samples collected in 12 wells and 3 springs along two sampling campaigns were used for this work. Schoeller and Stiff diagrams were employed for data analysis, beyond the statistical cluster analysis in order to verify similar patterns between the sampled points. Good correlation between hydrochemical patterns and the depth of the fractures bearing water were observed, allowing the identification of two groundwater groups. One group of wells aggregates samples presenting low concentration of ions associated to fractures depths located less than 30 meters, the second group is constituted by wells presenting high concentration of ions such as calcium, sodium, bicarbonates, and fractures depths located between 50 and 112 meters. The explanation of these differences can be related to the movement of water and water-rock interaction occurs differently depending on the depth of water inflow.Este trabalho buscou avaliar a existência de diferentes padrões hidroquímicos dos aquíferos fraturados do Sistema Aquífero Serra Geral (SASG), relacionando esses padrões com as profundidades das entradas de água, no município de Carlos Barbosa-RS. Para este trabalho foram utilizadas informações hidroquímicas da água referentes a duas amostragens realizadas em 12 poços tubulares e 3 fontes. Para análise dos dados empregou-se os diagramas de Schoeller e Stiff, além da análise estatística de agrupamento, a fim de verificar padrões semelhantes entre os pontos amostrados. Observou-se uma boa correlação entre os padrões hidroquímicos e a profundidade das entradas de água, o que permitiu a elaboração de um modelo conceitual hidroquímico, onde foram identificadas águas com baixa concentração de íons em grupo de poços que possuem entradas de água localizadas em profundidades inferiores a 30 metros. Também foi identificado um grupo de poços cujas entradas de água estão localizadas entre 50 e 112 metros e apresentam águas com maior concentração de íons como cálcio, sódio, bicarbonatos. A explicação dessas diferenças pode estar relacionada com a circulação de água e com tempo de interação água-rocha que ocorre de forma diferente dependendo da profundidade das entradas de água. ABAS - Associação Brasileira de Águas Subterrâneas2016-04-27info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://aguassubterraneas.abas.org/asubterraneas/article/view/2858510.14295/ras.v30i1.28585Águas Subterrâneas; v. 30 n. 1 (2016): REVISTA ÁGUAS SUBTERRÂNEAS; 99-1182179-97840101-7004reponame:Águas Subterrâneas (São Paulo. Online)instname:Associação Brasileira de Águas Subterrâneasinstacron:ABASporhttps://aguassubterraneas.abas.org/asubterraneas/article/view/28585/18558Copyright (c) 2016 Águas Subterrâneasinfo:eu-repo/semantics/openAccessBortolin, Taison AndersonReginato, Pedro Antonio RoeheLeão, Marcos ImérioSchneider, Vania Elisabete2019-02-16T21:43:51Zoai:ojs.aguassubterraneas.abas.org:article/28585Revistahttps://aguassubterraneas.abas.org/asubterraneas/ONGhttps://aguassubterraneas.abas.org/asubterraneas/oaihidropaulo@gmail.com2179-97840101-7004opendoar:2019-02-16T21:43:51Águas Subterrâneas (São Paulo. Online) - Associação Brasileira de Águas Subterrâneasfalse |
| dc.title.none.fl_str_mv |
Relationship between hydrochemical patterns and depths of water bearing frac-tures in acid volcanic rocks from serra geral formation Relação entre padrões hidroquímicos e as profundidades de fraturas com entra-das de água em rochas vulcânicas ácidas da formação serra geral |
| title |
Relationship between hydrochemical patterns and depths of water bearing frac-tures in acid volcanic rocks from serra geral formation |
| spellingShingle |
Relationship between hydrochemical patterns and depths of water bearing frac-tures in acid volcanic rocks from serra geral formation Bortolin, Taison Anderson Hydrochemical. Fractured aquifers. Serra Geral Aquifer System Hidroquímica. Aquíferos fraturados. Sistema Aquífero Serra Geral. |
| title_short |
Relationship between hydrochemical patterns and depths of water bearing frac-tures in acid volcanic rocks from serra geral formation |
| title_full |
Relationship between hydrochemical patterns and depths of water bearing frac-tures in acid volcanic rocks from serra geral formation |
| title_fullStr |
Relationship between hydrochemical patterns and depths of water bearing frac-tures in acid volcanic rocks from serra geral formation |
| title_full_unstemmed |
Relationship between hydrochemical patterns and depths of water bearing frac-tures in acid volcanic rocks from serra geral formation |
| title_sort |
Relationship between hydrochemical patterns and depths of water bearing frac-tures in acid volcanic rocks from serra geral formation |
| dc.creator.none.fl_str_mv |
Bortolin, Taison Anderson Reginato, Pedro Antonio Roehe Leão, Marcos Imério Schneider, Vania Elisabete |
| author |
Bortolin, Taison Anderson |
| author_facet |
Bortolin, Taison Anderson Reginato, Pedro Antonio Roehe Leão, Marcos Imério Schneider, Vania Elisabete |
| author_role |
author |
| author2 |
Reginato, Pedro Antonio Roehe Leão, Marcos Imério Schneider, Vania Elisabete |
| author2_role |
author author author |
| dc.subject.por.fl_str_mv |
Hydrochemical. Fractured aquifers. Serra Geral Aquifer System Hidroquímica. Aquíferos fraturados. Sistema Aquífero Serra Geral. |
| topic |
Hydrochemical. Fractured aquifers. Serra Geral Aquifer System Hidroquímica. Aquíferos fraturados. Sistema Aquífero Serra Geral. |
| description |
This study aimed to evaluate the existence of different hydrochemical patterns of fractured aquifers of the Serra Geral Aquifer System (SGAS), relating these patterns with the depths of the fractures bearing water in the city of Carlos Barbosa-RS. Hydrochemical information from samples collected in 12 wells and 3 springs along two sampling campaigns were used for this work. Schoeller and Stiff diagrams were employed for data analysis, beyond the statistical cluster analysis in order to verify similar patterns between the sampled points. Good correlation between hydrochemical patterns and the depth of the fractures bearing water were observed, allowing the identification of two groundwater groups. One group of wells aggregates samples presenting low concentration of ions associated to fractures depths located less than 30 meters, the second group is constituted by wells presenting high concentration of ions such as calcium, sodium, bicarbonates, and fractures depths located between 50 and 112 meters. The explanation of these differences can be related to the movement of water and water-rock interaction occurs differently depending on the depth of water inflow. |
| publishDate |
2016 |
| dc.date.none.fl_str_mv |
2016-04-27 |
| dc.type.driver.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion |
| format |
article |
| status_str |
publishedVersion |
| dc.identifier.uri.fl_str_mv |
https://aguassubterraneas.abas.org/asubterraneas/article/view/28585 10.14295/ras.v30i1.28585 |
| url |
https://aguassubterraneas.abas.org/asubterraneas/article/view/28585 |
| identifier_str_mv |
10.14295/ras.v30i1.28585 |
| dc.language.iso.fl_str_mv |
por |
| language |
por |
| dc.relation.none.fl_str_mv |
https://aguassubterraneas.abas.org/asubterraneas/article/view/28585/18558 |
| dc.rights.driver.fl_str_mv |
Copyright (c) 2016 Águas Subterrâneas info:eu-repo/semantics/openAccess |
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Copyright (c) 2016 Águas Subterrâneas |
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openAccess |
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application/pdf |
| dc.publisher.none.fl_str_mv |
ABAS - Associação Brasileira de Águas Subterrâneas |
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ABAS - Associação Brasileira de Águas Subterrâneas |
| dc.source.none.fl_str_mv |
Águas Subterrâneas; v. 30 n. 1 (2016): REVISTA ÁGUAS SUBTERRÂNEAS; 99-118 2179-9784 0101-7004 reponame:Águas Subterrâneas (São Paulo. Online) instname:Associação Brasileira de Águas Subterrâneas instacron:ABAS |
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Associação Brasileira de Águas Subterrâneas |
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ABAS |
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ABAS |
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Águas Subterrâneas (São Paulo. Online) |
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Águas Subterrâneas (São Paulo. Online) |
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Águas Subterrâneas (São Paulo. Online) - Associação Brasileira de Águas Subterrâneas |
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hidropaulo@gmail.com |
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15,301629 |