Contribution of natural uranium isotopes to the study of groundwater flow
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Publication Date: | 2021 |
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Format: | Article |
Language: | por |
Source: | Derbyana |
Download full: | https://revistaig.emnuvens.com.br/derbyana/article/view/746 |
Summary: | Uranium is a lithophile element that is preferentially concentrated in acid rather than basic/ultrabasic igneous rocks. Its average crustal abundance corresponds to 2.5 μg/g, composed of two primary isotopes, 238U (~99.3%) and 235U (~0.7%). Despite the technological importance of 235U, as it is the fissile isotope that is the basis of nuclear energy production, it appears that its contribution as a natural source of radioactivity is small, since the specific activity of 238U is about 20 times greater than 235U. Isotopes 238U and 235U are progenitors of radioactive decay series, the greater number of descendants corresponding to 238U, many of which possessing a long half-life, such as 234U formed in the 238U decay series from the following sequence: 238U (4.49 Ga, α) → 234Th (24.1 days, β-) → 234Pa (1.18 min, β-) → 234U (248 ka, α) →... Both 238U and 234U are emitters of alpha particles and, in groundwater, the assessment of the extent of radioactive imbalance between these uranium isotopes has allowed the development of numerous studies of hydrogeological interest since the 1960’s. The main mechanisms that explain such disequilibrium are the 234U selective leaching relatively to 238U from the crystalline lattice of minerals and alpha recoil that introduces 234Th into the liquid phase, which forms 234Pa by beta decay, radionuclide that produces 234U, also by beta decay, causing 234U-enrichment in groundwaters, i.e., 234U/238U activity ratios greater than unity. These ratios, together with the dissolved uranium concentration, have been extensively utilized in hydrological applications, such as those described in this paper. |
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Contribution of natural uranium isotopes to the study of groundwater flowContribuição dos isótopos naturais de urânio no estudo da movimentação das águas subterrâneasIsótopos de urânio; U-238 e U-234; Águas subterrâneas; Datação; MisturaUranium isotopes; U-238 and U-234; Groundwater; Dating; MixingUranium is a lithophile element that is preferentially concentrated in acid rather than basic/ultrabasic igneous rocks. Its average crustal abundance corresponds to 2.5 μg/g, composed of two primary isotopes, 238U (~99.3%) and 235U (~0.7%). Despite the technological importance of 235U, as it is the fissile isotope that is the basis of nuclear energy production, it appears that its contribution as a natural source of radioactivity is small, since the specific activity of 238U is about 20 times greater than 235U. Isotopes 238U and 235U are progenitors of radioactive decay series, the greater number of descendants corresponding to 238U, many of which possessing a long half-life, such as 234U formed in the 238U decay series from the following sequence: 238U (4.49 Ga, α) → 234Th (24.1 days, β-) → 234Pa (1.18 min, β-) → 234U (248 ka, α) →... Both 238U and 234U are emitters of alpha particles and, in groundwater, the assessment of the extent of radioactive imbalance between these uranium isotopes has allowed the development of numerous studies of hydrogeological interest since the 1960’s. The main mechanisms that explain such disequilibrium are the 234U selective leaching relatively to 238U from the crystalline lattice of minerals and alpha recoil that introduces 234Th into the liquid phase, which forms 234Pa by beta decay, radionuclide that produces 234U, also by beta decay, causing 234U-enrichment in groundwaters, i.e., 234U/238U activity ratios greater than unity. These ratios, together with the dissolved uranium concentration, have been extensively utilized in hydrological applications, such as those described in this paper.O urânio é um elemento litófilo, concentrando-se preferencialmente nas rochas ígneas ácidas ao invés das básicas/ultrabásicas. Sua abundância crustal média corresponde a 2,5 μg/g, possuindo dois isótopos primários, o 238U (~99,3%) e o 235U (~0,7%). Apesar da importância tecnológica do 235U, por ser o isótopo físsil que forma a base de produção de energia nuclear, verifica-se que a sua contribuição como fonte natural de radioatividade é pequena, pois a atividade específica do 238U é cerca de 20 vezes maior que a do 235U. Os isótopos 238U e 235U são geradores de séries de decaimento radioativo, possuindo o 238U um número maior de descendentes, muitos dos quais de longa meia-vida, como é o caso do 234U, que é formado na série do 238U a partir da seguinte sequência: 238U (4,49 Ga, α) → 234Th (24,1 dias, β-) → 234Pa (1,18 min, β-) → 234U (248 ka, α) →... Tanto 238U quanto 234U são emissores de partículas alfa e, nas águas subterrâneas, a avaliação da extensão do desequilíbrio radioativo entre esses isótopos de urânio, a partir da década de 1960, tem permitido o desenvolvimento de inúmeras pesquisas de interesse hidrogeológico. Os mecanismos principais que explicam esse desequilíbrio são a lixiviação seletiva de 234U em relação a 238U no retículo cristalino dos minerais e o processo de recuo alfa que introduz 234Th na fase líquida, o qual decai por emissão beta para 234Pa e este para 234U, também por emissão beta, ocasionando enriquecimento de 234U nas águas subterrâneas, isto é, razões de atividade 234U/238U superiores à unidade. Essas razões, juntamente com a concentração do urânio dissolvido, têm sido consideravelmente utilizadas em aplicações hidrológicas, como será descrito neste trabalho.Instituto de Pesquisas Ambientais, Secretaria de Infraestrutura e Meio Ambiente/SP2021-10-24info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://revistaig.emnuvens.com.br/derbyana/article/view/74610.14295/derb.v42.746Derbyana; Vol. 42 (2021)Derbyana; Vol. 42 (2021)Derbyana; v. 42 (2021)2764-1465reponame:Derbyanainstname:Secretaria de Infraestrutura e Meio Ambiente do Estado de São Pauloinstacron:SIMAESPporhttps://revistaig.emnuvens.com.br/derbyana/article/view/746/725Copyright (c) 2021 Luís Henrique Mancini, Daniel Marcos Bonottoinfo:eu-repo/semantics/openAccessMancini, Luís HenriqueBonotto, Daniel Marcos2021-10-25T14:09:03Zoai:ojs.revistaig.emnuvens.com.br:article/746Revistahttps://revistaig.emnuvens.com.br/derbyanaPUBhttps://revistaig.emnuvens.com.br/derbyana/oaiderbyana.journal@gmail.com | shiruma@sp.gov.br2764-14652764-1465opendoar:2021-10-25T14:09:03Derbyana - Secretaria de Infraestrutura e Meio Ambiente do Estado de São Paulofalse |
dc.title.none.fl_str_mv |
Contribution of natural uranium isotopes to the study of groundwater flow Contribuição dos isótopos naturais de urânio no estudo da movimentação das águas subterrâneas |
title |
Contribution of natural uranium isotopes to the study of groundwater flow |
spellingShingle |
Contribution of natural uranium isotopes to the study of groundwater flow Mancini, Luís Henrique Isótopos de urânio; U-238 e U-234; Águas subterrâneas; Datação; Mistura Uranium isotopes; U-238 and U-234; Groundwater; Dating; Mixing |
title_short |
Contribution of natural uranium isotopes to the study of groundwater flow |
title_full |
Contribution of natural uranium isotopes to the study of groundwater flow |
title_fullStr |
Contribution of natural uranium isotopes to the study of groundwater flow |
title_full_unstemmed |
Contribution of natural uranium isotopes to the study of groundwater flow |
title_sort |
Contribution of natural uranium isotopes to the study of groundwater flow |
author |
Mancini, Luís Henrique |
author_facet |
Mancini, Luís Henrique Bonotto, Daniel Marcos |
author_role |
author |
author2 |
Bonotto, Daniel Marcos |
author2_role |
author |
dc.contributor.author.fl_str_mv |
Mancini, Luís Henrique Bonotto, Daniel Marcos |
dc.subject.por.fl_str_mv |
Isótopos de urânio; U-238 e U-234; Águas subterrâneas; Datação; Mistura Uranium isotopes; U-238 and U-234; Groundwater; Dating; Mixing |
topic |
Isótopos de urânio; U-238 e U-234; Águas subterrâneas; Datação; Mistura Uranium isotopes; U-238 and U-234; Groundwater; Dating; Mixing |
description |
Uranium is a lithophile element that is preferentially concentrated in acid rather than basic/ultrabasic igneous rocks. Its average crustal abundance corresponds to 2.5 μg/g, composed of two primary isotopes, 238U (~99.3%) and 235U (~0.7%). Despite the technological importance of 235U, as it is the fissile isotope that is the basis of nuclear energy production, it appears that its contribution as a natural source of radioactivity is small, since the specific activity of 238U is about 20 times greater than 235U. Isotopes 238U and 235U are progenitors of radioactive decay series, the greater number of descendants corresponding to 238U, many of which possessing a long half-life, such as 234U formed in the 238U decay series from the following sequence: 238U (4.49 Ga, α) → 234Th (24.1 days, β-) → 234Pa (1.18 min, β-) → 234U (248 ka, α) →... Both 238U and 234U are emitters of alpha particles and, in groundwater, the assessment of the extent of radioactive imbalance between these uranium isotopes has allowed the development of numerous studies of hydrogeological interest since the 1960’s. The main mechanisms that explain such disequilibrium are the 234U selective leaching relatively to 238U from the crystalline lattice of minerals and alpha recoil that introduces 234Th into the liquid phase, which forms 234Pa by beta decay, radionuclide that produces 234U, also by beta decay, causing 234U-enrichment in groundwaters, i.e., 234U/238U activity ratios greater than unity. These ratios, together with the dissolved uranium concentration, have been extensively utilized in hydrological applications, such as those described in this paper. |
publishDate |
2021 |
dc.date.none.fl_str_mv |
2021-10-24 |
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://revistaig.emnuvens.com.br/derbyana/article/view/746 10.14295/derb.v42.746 |
url |
https://revistaig.emnuvens.com.br/derbyana/article/view/746 |
identifier_str_mv |
10.14295/derb.v42.746 |
dc.language.iso.fl_str_mv |
por |
language |
por |
dc.relation.none.fl_str_mv |
https://revistaig.emnuvens.com.br/derbyana/article/view/746/725 |
dc.rights.driver.fl_str_mv |
Copyright (c) 2021 Luís Henrique Mancini, Daniel Marcos Bonotto info:eu-repo/semantics/openAccess |
rights_invalid_str_mv |
Copyright (c) 2021 Luís Henrique Mancini, Daniel Marcos Bonotto |
eu_rights_str_mv |
openAccess |
dc.format.none.fl_str_mv |
application/pdf |
dc.publisher.none.fl_str_mv |
Instituto de Pesquisas Ambientais, Secretaria de Infraestrutura e Meio Ambiente/SP |
publisher.none.fl_str_mv |
Instituto de Pesquisas Ambientais, Secretaria de Infraestrutura e Meio Ambiente/SP |
dc.source.none.fl_str_mv |
Derbyana; Vol. 42 (2021) Derbyana; Vol. 42 (2021) Derbyana; v. 42 (2021) 2764-1465 reponame:Derbyana instname:Secretaria de Infraestrutura e Meio Ambiente do Estado de São Paulo instacron:SIMAESP |
instname_str |
Secretaria de Infraestrutura e Meio Ambiente do Estado de São Paulo |
instacron_str |
SIMAESP |
institution |
SIMAESP |
reponame_str |
Derbyana |
collection |
Derbyana |
repository.name.fl_str_mv |
Derbyana - Secretaria de Infraestrutura e Meio Ambiente do Estado de São Paulo |
repository.mail.fl_str_mv |
derbyana.journal@gmail.com | shiruma@sp.gov.br |
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1838465476117659648 |