Technological Characterization and Radon Exhalation Rate of an Olivine Diabase Porphyritic of the Apuiarés Region – CE
Autor(a) principal: | |
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Data de Publicação: | 2022 |
Outros Autores: | , , , , , |
Tipo de documento: | Artigo |
Idioma: | por |
Título da fonte: | Repositório Institucional da UNESP |
Texto Completo: | http://dx.doi.org/10.11137/1982-3908_2022_45_39354 http://hdl.handle.net/11449/230467 |
Resumo: | Radon gas (²²²Rn) after cigarette smoking, has been considered the leading cause of lung cancer in the United States, according to studies, 21,000 people die each year from gas inhalation. Thus, it is very important that radon concentrations be known indoors: residences, mines, galleries, among others. The objective of this paper is to present the results of studies on the mineralogical and technological characteristics of a diabase dyke, with the purpose of obtaining characteristics oriented to the application as ornamental rock and for coatings, following the norms of the ABNT and to evaluate the exhalation rate of radon, through the application of methods active detection of radon gas. The dike is located in the municipality of Apuiarés-CE, geologically located in the Borborema Province, NE of Brazil, NE of the Central Ceará Domain, related to meso-cenozoic intrusive and effusive magmatic phenomena. Two blocks of diabase with dimensions of 30x40x30 cm were collected and sent to the laboratory, where the specimens were made for the technological and radiometric tests. The dike is petrographically characterized with Porphyritic Olivine Diabase it corresponds to a rock of dark gray color with variations for black, isotropic structure and porphyritic texture, showing no stains or irregularities in the texture that would compromise the aesthetic standard for use as ornamental rock. The radon exhalation test resulted in 1 ± 3 Bq m-3 and at exhalation rate of radon per unit area (E), 0.001 Bq m-2.h-1. Therefore, in terms of technology characterization and radon exhalation rate ²²²Rn, the Porphyritic Olivine Diabase presents the requirements of use as dimension stones. |
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Technological Characterization and Radon Exhalation Rate of an Olivine Diabase Porphyritic of the Apuiarés Region – CECaracterização Tecnológica e Taxa de Exalação de Radônio de um Olivina Diabásio Porfirítico da Região de Apuiarés – CEDimension stonesPorphyritic olivine diabaseRadonRadon gas (²²²Rn) after cigarette smoking, has been considered the leading cause of lung cancer in the United States, according to studies, 21,000 people die each year from gas inhalation. Thus, it is very important that radon concentrations be known indoors: residences, mines, galleries, among others. The objective of this paper is to present the results of studies on the mineralogical and technological characteristics of a diabase dyke, with the purpose of obtaining characteristics oriented to the application as ornamental rock and for coatings, following the norms of the ABNT and to evaluate the exhalation rate of radon, through the application of methods active detection of radon gas. The dike is located in the municipality of Apuiarés-CE, geologically located in the Borborema Province, NE of Brazil, NE of the Central Ceará Domain, related to meso-cenozoic intrusive and effusive magmatic phenomena. Two blocks of diabase with dimensions of 30x40x30 cm were collected and sent to the laboratory, where the specimens were made for the technological and radiometric tests. The dike is petrographically characterized with Porphyritic Olivine Diabase it corresponds to a rock of dark gray color with variations for black, isotropic structure and porphyritic texture, showing no stains or irregularities in the texture that would compromise the aesthetic standard for use as ornamental rock. The radon exhalation test resulted in 1 ± 3 Bq m-3 and at exhalation rate of radon per unit area (E), 0.001 Bq m-2.h-1. Therefore, in terms of technology characterization and radon exhalation rate ²²²Rn, the Porphyritic Olivine Diabase presents the requirements of use as dimension stones.Curso de Engenharia de Minas Universidade Federal do Ceará/UFC Campus de Crateús, CELaboratório de Microscopia Eletrônica Departamento de Geologia Universidade Federal do Ceará/UFC, Campus do Pici, CEFundação Núcleo de Tecnologia Industrial do Ceará/NUTEC, Campus do Pici, CEFaculdade de Ciências e Tecnologia Universidade Federal de Goiás/UFG, GODepartamento de Petrologia e Metalogênia Instituto de Geociências e Ciências Exatas Universidade Estadual Paulista/UNESP, SPUniversidade Federal do Pampa/UNIPAMPA Campus Caçapava do Sul, RSDepartamento de Petrologia e Metalogênia Instituto de Geociências e Ciências Exatas Universidade Estadual Paulista/UNESP, SPUniversidade Federal do Ceará/UFCFundação Núcleo de Tecnologia Industrial do Ceará/NUTECUniversidade Federal de Goiás (UFG)Universidade Estadual Paulista (UNESP)Universidade Federal do Pampa/UNIPAMPASilva, Francisco Diones OliveiraNeto, Antônio LealSoares, Wollker CunhaNeto, José de Araújo NogueiraArtur, Antônio Carlos [UNESP]Mattos, Irani ClezarClemente, Igor Magalhães2022-04-29T08:40:06Z2022-04-29T08:40:06Z2022-01-01info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articlehttp://dx.doi.org/10.11137/1982-3908_2022_45_39354Anuario do Instituto de Geociencias, v. 45.1982-39080101-9759http://hdl.handle.net/11449/23046710.11137/1982-3908_2022_45_393542-s2.0-85125385147Scopusreponame:Repositório Institucional da UNESPinstname:Universidade Estadual Paulista (UNESP)instacron:UNESPporAnuario do Instituto de Geocienciasinfo:eu-repo/semantics/openAccess2022-04-29T08:40:06Zoai:repositorio.unesp.br:11449/230467Repositório InstitucionalPUBhttp://repositorio.unesp.br/oai/requestopendoar:29462024-08-05T17:04:20.609622Repositório Institucional da UNESP - Universidade Estadual Paulista (UNESP)false |
dc.title.none.fl_str_mv |
Technological Characterization and Radon Exhalation Rate of an Olivine Diabase Porphyritic of the Apuiarés Region – CE Caracterização Tecnológica e Taxa de Exalação de Radônio de um Olivina Diabásio Porfirítico da Região de Apuiarés – CE |
title |
Technological Characterization and Radon Exhalation Rate of an Olivine Diabase Porphyritic of the Apuiarés Region – CE |
spellingShingle |
Technological Characterization and Radon Exhalation Rate of an Olivine Diabase Porphyritic of the Apuiarés Region – CE Silva, Francisco Diones Oliveira Dimension stones Porphyritic olivine diabase Radon |
title_short |
Technological Characterization and Radon Exhalation Rate of an Olivine Diabase Porphyritic of the Apuiarés Region – CE |
title_full |
Technological Characterization and Radon Exhalation Rate of an Olivine Diabase Porphyritic of the Apuiarés Region – CE |
title_fullStr |
Technological Characterization and Radon Exhalation Rate of an Olivine Diabase Porphyritic of the Apuiarés Region – CE |
title_full_unstemmed |
Technological Characterization and Radon Exhalation Rate of an Olivine Diabase Porphyritic of the Apuiarés Region – CE |
title_sort |
Technological Characterization and Radon Exhalation Rate of an Olivine Diabase Porphyritic of the Apuiarés Region – CE |
author |
Silva, Francisco Diones Oliveira |
author_facet |
Silva, Francisco Diones Oliveira Neto, Antônio Leal Soares, Wollker Cunha Neto, José de Araújo Nogueira Artur, Antônio Carlos [UNESP] Mattos, Irani Clezar Clemente, Igor Magalhães |
author_role |
author |
author2 |
Neto, Antônio Leal Soares, Wollker Cunha Neto, José de Araújo Nogueira Artur, Antônio Carlos [UNESP] Mattos, Irani Clezar Clemente, Igor Magalhães |
author2_role |
author author author author author author |
dc.contributor.none.fl_str_mv |
Universidade Federal do Ceará/UFC Fundação Núcleo de Tecnologia Industrial do Ceará/NUTEC Universidade Federal de Goiás (UFG) Universidade Estadual Paulista (UNESP) Universidade Federal do Pampa/UNIPAMPA |
dc.contributor.author.fl_str_mv |
Silva, Francisco Diones Oliveira Neto, Antônio Leal Soares, Wollker Cunha Neto, José de Araújo Nogueira Artur, Antônio Carlos [UNESP] Mattos, Irani Clezar Clemente, Igor Magalhães |
dc.subject.por.fl_str_mv |
Dimension stones Porphyritic olivine diabase Radon |
topic |
Dimension stones Porphyritic olivine diabase Radon |
description |
Radon gas (²²²Rn) after cigarette smoking, has been considered the leading cause of lung cancer in the United States, according to studies, 21,000 people die each year from gas inhalation. Thus, it is very important that radon concentrations be known indoors: residences, mines, galleries, among others. The objective of this paper is to present the results of studies on the mineralogical and technological characteristics of a diabase dyke, with the purpose of obtaining characteristics oriented to the application as ornamental rock and for coatings, following the norms of the ABNT and to evaluate the exhalation rate of radon, through the application of methods active detection of radon gas. The dike is located in the municipality of Apuiarés-CE, geologically located in the Borborema Province, NE of Brazil, NE of the Central Ceará Domain, related to meso-cenozoic intrusive and effusive magmatic phenomena. Two blocks of diabase with dimensions of 30x40x30 cm were collected and sent to the laboratory, where the specimens were made for the technological and radiometric tests. The dike is petrographically characterized with Porphyritic Olivine Diabase it corresponds to a rock of dark gray color with variations for black, isotropic structure and porphyritic texture, showing no stains or irregularities in the texture that would compromise the aesthetic standard for use as ornamental rock. The radon exhalation test resulted in 1 ± 3 Bq m-3 and at exhalation rate of radon per unit area (E), 0.001 Bq m-2.h-1. Therefore, in terms of technology characterization and radon exhalation rate ²²²Rn, the Porphyritic Olivine Diabase presents the requirements of use as dimension stones. |
publishDate |
2022 |
dc.date.none.fl_str_mv |
2022-04-29T08:40:06Z 2022-04-29T08:40:06Z 2022-01-01 |
dc.type.status.fl_str_mv |
info:eu-repo/semantics/publishedVersion |
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/article |
format |
article |
status_str |
publishedVersion |
dc.identifier.uri.fl_str_mv |
http://dx.doi.org/10.11137/1982-3908_2022_45_39354 Anuario do Instituto de Geociencias, v. 45. 1982-3908 0101-9759 http://hdl.handle.net/11449/230467 10.11137/1982-3908_2022_45_39354 2-s2.0-85125385147 |
url |
http://dx.doi.org/10.11137/1982-3908_2022_45_39354 http://hdl.handle.net/11449/230467 |
identifier_str_mv |
Anuario do Instituto de Geociencias, v. 45. 1982-3908 0101-9759 10.11137/1982-3908_2022_45_39354 2-s2.0-85125385147 |
dc.language.iso.fl_str_mv |
por |
language |
por |
dc.relation.none.fl_str_mv |
Anuario do Instituto de Geociencias |
dc.rights.driver.fl_str_mv |
info:eu-repo/semantics/openAccess |
eu_rights_str_mv |
openAccess |
dc.source.none.fl_str_mv |
Scopus reponame:Repositório Institucional da UNESP instname:Universidade Estadual Paulista (UNESP) instacron:UNESP |
instname_str |
Universidade Estadual Paulista (UNESP) |
instacron_str |
UNESP |
institution |
UNESP |
reponame_str |
Repositório Institucional da UNESP |
collection |
Repositório Institucional da UNESP |
repository.name.fl_str_mv |
Repositório Institucional da UNESP - Universidade Estadual Paulista (UNESP) |
repository.mail.fl_str_mv |
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1808128750309605376 |