The use of Ground Penetrating Radar (GPR) in the definition of salt wedge penetration and groundwater monitoring in the estuarine Amazonian beach

Bibliographic Details
Main Author: Correia, Karolina Almeida
Publication Date: 2019
Other Authors: da Silva, Marcos Welby Correa, Mendes, Amilcar Carvalho, de Miranda, Artur Gustavo Oliveira, Luczynsky, Estanislau, da Cunha, Ivson Roberto Viana
Format: Article
Language: por
Source: Águas Subterrâneas (São Paulo. Online)
Download full: https://aguassubterraneas.abas.org/asubterraneas/article/view/29095
Summary: The association of survey data with records obtained through the use of the Ground Penetrating Radar (GPR), taking into account the climatic seasonality, in Praia do Farol (Mosqueiro Island / Belém-PA), revealed the behavior of the water table and the record of the penetration of the salt wedge into subsurface in this estuarine environment. The identification of the water table was very clear, revealing a transition between unsaturated zone and well-defined saturated zone. The GPR profiles show that the level of the top of the water table is registered as a strong horizontal reflector, diving towards the sea. The top of the water table in the post-beach zone is located approximately 1 meter deep in the rainy season (March), becoming deeper in the intertidal zone. During the dry season (November), the top of the surface of the sheet undergoes deepening, ranging from 1.9 meters in the supramarine zone to 2 meters in the intertidal zone. The soil moisture and, above all, the presence of salt in the beach sediments had a strong influence on the reflection signals, changing the dielectric constant of the sediments and, consequently, creating zones of signal attenuation, thus allowing mapping of the salt wedge in subsurface during the dry season. However, a geophysical study is recommended using other methods, seeking better results from a hydrogeological point of view.
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spelling The use of Ground Penetrating Radar (GPR) in the definition of salt wedge penetration and groundwater monitoring in the estuarine Amazonian beachA utilização do Ground Penetrating Radar (GPR) na definição de penetração de cunha salina e no monitoramento do nível freático em praia estuarina amazônicaGPR. Salt wedge estuarine beach. Groundwater. Amazon.GPR. Cunha salina. Praia estuarina. Nível freático. Amazônia.The association of survey data with records obtained through the use of the Ground Penetrating Radar (GPR), taking into account the climatic seasonality, in Praia do Farol (Mosqueiro Island / Belém-PA), revealed the behavior of the water table and the record of the penetration of the salt wedge into subsurface in this estuarine environment. The identification of the water table was very clear, revealing a transition between unsaturated zone and well-defined saturated zone. The GPR profiles show that the level of the top of the water table is registered as a strong horizontal reflector, diving towards the sea. The top of the water table in the post-beach zone is located approximately 1 meter deep in the rainy season (March), becoming deeper in the intertidal zone. During the dry season (November), the top of the surface of the sheet undergoes deepening, ranging from 1.9 meters in the supramarine zone to 2 meters in the intertidal zone. The soil moisture and, above all, the presence of salt in the beach sediments had a strong influence on the reflection signals, changing the dielectric constant of the sediments and, consequently, creating zones of signal attenuation, thus allowing mapping of the salt wedge in subsurface during the dry season. However, a geophysical study is recommended using other methods, seeking better results from a hydrogeological point of view.A identificação do nível freático foi bastante clara, revelando uma transição entre zona não saturada e zona saturada bem definida. Os perfis de GPR mostraram que o topo do nível freático é registrado como um refletor horizontal forte, mergulhando em direção ao mar. O topo do nível freático na zona de pós-praia está localizado em aproximadamente 1 metro de profundidade, no período chuvoso (março), tornando-se mais profundo na zona intermarés. No período de estiagem (novembro), o topo da superfície do nível sofre rebaixamento, variando de 1,9 metros na zona supramarés, a e 2 metros na zona intermarés. A umidade do solo e, sobretudo, a presença de sal nos sedimentos praiais tiveram forte influência nos sinais da reflexão, mudando a constante dielétrica dos sedimentos e, consequentemente, criando zonas de atenuação de sinais, permitindo, dessa forma, mapear a cunha salina em subsuperfície durante o período de estiagem. Contudo, é recomendado um estudo geofísico utilizando outros métodos, buscando melhores resultados do ponto de vista hidrogeológico.ABAS - Associação Brasileira de Águas Subterrâneas2019-03-06info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://aguassubterraneas.abas.org/asubterraneas/article/view/2909510.14295/ras.v33i1.29095Águas Subterrâneas; v. 33 n. 1 (2019): REVISTA ÁGUAS SUBTERRÂNEAS; 87-1012179-97840101-7004reponame:Águas Subterrâneas (São Paulo. Online)instname:Associação Brasileira de Águas Subterrâneasinstacron:ABASporhttps://aguassubterraneas.abas.org/asubterraneas/article/view/29095/19078Copyright (c) 2019 Águas Subterrâneasinfo:eu-repo/semantics/openAccessCorreia, Karolina Almeidada Silva, Marcos Welby CorreaMendes, Amilcar Carvalhode Miranda, Artur Gustavo OliveiraLuczynsky, Estanislauda Cunha, Ivson Roberto Viana2019-12-11T21:58:03Zoai:ojs.aguassubterraneas.abas.org:article/29095Revistahttps://aguassubterraneas.abas.org/asubterraneas/ONGhttps://aguassubterraneas.abas.org/asubterraneas/oaihidropaulo@gmail.com2179-97840101-7004opendoar:2019-12-11T21:58:03Águas Subterrâneas (São Paulo. Online) - Associação Brasileira de Águas Subterrâneasfalse
dc.title.none.fl_str_mv The use of Ground Penetrating Radar (GPR) in the definition of salt wedge penetration and groundwater monitoring in the estuarine Amazonian beach
A utilização do Ground Penetrating Radar (GPR) na definição de penetração de cunha salina e no monitoramento do nível freático em praia estuarina amazônica
title The use of Ground Penetrating Radar (GPR) in the definition of salt wedge penetration and groundwater monitoring in the estuarine Amazonian beach
spellingShingle The use of Ground Penetrating Radar (GPR) in the definition of salt wedge penetration and groundwater monitoring in the estuarine Amazonian beach
Correia, Karolina Almeida
GPR. Salt wedge estuarine beach. Groundwater. Amazon.
GPR. Cunha salina. Praia estuarina. Nível freático. Amazônia.
title_short The use of Ground Penetrating Radar (GPR) in the definition of salt wedge penetration and groundwater monitoring in the estuarine Amazonian beach
title_full The use of Ground Penetrating Radar (GPR) in the definition of salt wedge penetration and groundwater monitoring in the estuarine Amazonian beach
title_fullStr The use of Ground Penetrating Radar (GPR) in the definition of salt wedge penetration and groundwater monitoring in the estuarine Amazonian beach
title_full_unstemmed The use of Ground Penetrating Radar (GPR) in the definition of salt wedge penetration and groundwater monitoring in the estuarine Amazonian beach
title_sort The use of Ground Penetrating Radar (GPR) in the definition of salt wedge penetration and groundwater monitoring in the estuarine Amazonian beach
author Correia, Karolina Almeida
author_facet Correia, Karolina Almeida
da Silva, Marcos Welby Correa
Mendes, Amilcar Carvalho
de Miranda, Artur Gustavo Oliveira
Luczynsky, Estanislau
da Cunha, Ivson Roberto Viana
author_role author
author2 da Silva, Marcos Welby Correa
Mendes, Amilcar Carvalho
de Miranda, Artur Gustavo Oliveira
Luczynsky, Estanislau
da Cunha, Ivson Roberto Viana
author2_role author
author
author
author
author
dc.contributor.author.fl_str_mv Correia, Karolina Almeida
da Silva, Marcos Welby Correa
Mendes, Amilcar Carvalho
de Miranda, Artur Gustavo Oliveira
Luczynsky, Estanislau
da Cunha, Ivson Roberto Viana
dc.subject.por.fl_str_mv GPR. Salt wedge estuarine beach. Groundwater. Amazon.
GPR. Cunha salina. Praia estuarina. Nível freático. Amazônia.
topic GPR. Salt wedge estuarine beach. Groundwater. Amazon.
GPR. Cunha salina. Praia estuarina. Nível freático. Amazônia.
description The association of survey data with records obtained through the use of the Ground Penetrating Radar (GPR), taking into account the climatic seasonality, in Praia do Farol (Mosqueiro Island / Belém-PA), revealed the behavior of the water table and the record of the penetration of the salt wedge into subsurface in this estuarine environment. The identification of the water table was very clear, revealing a transition between unsaturated zone and well-defined saturated zone. The GPR profiles show that the level of the top of the water table is registered as a strong horizontal reflector, diving towards the sea. The top of the water table in the post-beach zone is located approximately 1 meter deep in the rainy season (March), becoming deeper in the intertidal zone. During the dry season (November), the top of the surface of the sheet undergoes deepening, ranging from 1.9 meters in the supramarine zone to 2 meters in the intertidal zone. The soil moisture and, above all, the presence of salt in the beach sediments had a strong influence on the reflection signals, changing the dielectric constant of the sediments and, consequently, creating zones of signal attenuation, thus allowing mapping of the salt wedge in subsurface during the dry season. However, a geophysical study is recommended using other methods, seeking better results from a hydrogeological point of view.
publishDate 2019
dc.date.none.fl_str_mv 2019-03-06
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/29095
10.14295/ras.v33i1.29095
url https://aguassubterraneas.abas.org/asubterraneas/article/view/29095
identifier_str_mv 10.14295/ras.v33i1.29095
dc.language.iso.fl_str_mv por
language por
dc.relation.none.fl_str_mv https://aguassubterraneas.abas.org/asubterraneas/article/view/29095/19078
dc.rights.driver.fl_str_mv Copyright (c) 2019 Águas Subterrâneas
info:eu-repo/semantics/openAccess
rights_invalid_str_mv Copyright (c) 2019 Águas Subterrâneas
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
dc.publisher.none.fl_str_mv ABAS - Associação Brasileira de Águas Subterrâneas
publisher.none.fl_str_mv ABAS - Associação Brasileira de Águas Subterrâneas
dc.source.none.fl_str_mv Águas Subterrâneas; v. 33 n. 1 (2019): REVISTA ÁGUAS SUBTERRÂNEAS; 87-101
2179-9784
0101-7004
reponame:Águas Subterrâneas (São Paulo. Online)
instname:Associação Brasileira de Águas Subterrâneas
instacron:ABAS
instname_str Associação Brasileira de Águas Subterrâneas
instacron_str ABAS
institution ABAS
reponame_str Águas Subterrâneas (São Paulo. Online)
collection Águas Subterrâneas (São Paulo. Online)
repository.name.fl_str_mv Águas Subterrâneas (São Paulo. Online) - Associação Brasileira de Águas Subterrâneas
repository.mail.fl_str_mv hidropaulo@gmail.com
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