Visible and near-infrared luminescent Eu3+ or Er3+ doped laponite-derived xerogels and thick films: structural and spectroscopic properties

Detalhes bibliográficos
Autor(a) principal: Tronto, Jairo
Data de Publicação: 2009
Outros Autores: Ribeiro, Sidney José Lima, Valim, João Barros, Gonçalves, Rogéria Rocha
Tipo de documento: Artigo
Idioma: eng
Título da fonte: LOCUS Repositório Institucional da UFV
Texto Completo: https://doi.org/10.1016/j.matchemphys.2008.07.030
http://www.locus.ufv.br/handle/123456789/22312
Resumo: Laponite-derived materials represent promising materials for optical applications. In this work, Eu^3+- or Er^3+-doped laponite xerogels and films were prepared from colloidal dispersion. Homogeneous, crack-free and transparent single layers were deposited on soda-lime substrates with a thickness of 10 μm. Structural and spectroscopic properties were analyzed by thermal analyses, X-ray diffractometry, transmission electron microscopy, infrared spectroscopy, and luminescence spectroscopy. The addition of a rare earth ion to the laponite does not promote any changes in thermal stability or phase transition. Laponite clay was identified after annealing up to 500 °C, with a decrease in basal spacing when the annealing temperature is changed from 100 °C to 500 °C. Enstatite polymorphs and amorphous silicate phases were observed after heat treatment at 700 °C and 900 °C. Stationary and time-dependent luminescence spectra in the visible region for Eu^3+, and 5D0 lifetime are discussed in terms of thermal treatment and structural evolution. In the layered host, the Eu^3+ ions are distributed in many different local environments. However, Eu^3+ ions were found to occupy at least two symmetry sites, and the ions are preferentially incorporated into the crystalline enstatite for the materials annealed at 700 °C and 900 °C. A 5D0 lifetime of 1.3 ms and 3.1 ms was obtained for Eu^3+ ions in an amorphous silicate and crystalline MgSiO3 local environment, respectively. Strong Er^3+ emission at the 1550 nm region was observed for the materials annealed at 900 °C, with a bandwidth of 44 nm.
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spelling Visible and near-infrared luminescent Eu3+ or Er3+ doped laponite-derived xerogels and thick films: structural and spectroscopic propertiesClaysLaponiteRare earthEuropiumErbiumXerogelsFilms and silicateLaponite-derived materials represent promising materials for optical applications. In this work, Eu^3+- or Er^3+-doped laponite xerogels and films were prepared from colloidal dispersion. Homogeneous, crack-free and transparent single layers were deposited on soda-lime substrates with a thickness of 10 μm. Structural and spectroscopic properties were analyzed by thermal analyses, X-ray diffractometry, transmission electron microscopy, infrared spectroscopy, and luminescence spectroscopy. The addition of a rare earth ion to the laponite does not promote any changes in thermal stability or phase transition. Laponite clay was identified after annealing up to 500 °C, with a decrease in basal spacing when the annealing temperature is changed from 100 °C to 500 °C. Enstatite polymorphs and amorphous silicate phases were observed after heat treatment at 700 °C and 900 °C. Stationary and time-dependent luminescence spectra in the visible region for Eu^3+, and 5D0 lifetime are discussed in terms of thermal treatment and structural evolution. In the layered host, the Eu^3+ ions are distributed in many different local environments. However, Eu^3+ ions were found to occupy at least two symmetry sites, and the ions are preferentially incorporated into the crystalline enstatite for the materials annealed at 700 °C and 900 °C. A 5D0 lifetime of 1.3 ms and 3.1 ms was obtained for Eu^3+ ions in an amorphous silicate and crystalline MgSiO3 local environment, respectively. Strong Er^3+ emission at the 1550 nm region was observed for the materials annealed at 900 °C, with a bandwidth of 44 nm.Materials Chemistry and Physics2018-10-17T11:08:24Z2018-10-17T11:08:24Z2009-01-15info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articlepdfapplication/pdf02540584https://doi.org/10.1016/j.matchemphys.2008.07.030http://www.locus.ufv.br/handle/123456789/22312engv. 113, n. 1, p. 71- 77, jan. 2009Elsevier B.V.info:eu-repo/semantics/openAccessTronto, JairoRibeiro, Sidney José LimaValim, João BarrosGonçalves, Rogéria Rochareponame:LOCUS Repositório Institucional da UFVinstname:Universidade Federal de Viçosa (UFV)instacron:UFV2024-07-12T06:23:45Zoai:locus.ufv.br:123456789/22312Repositório InstitucionalPUBhttps://www.locus.ufv.br/oai/requestfabiojreis@ufv.bropendoar:21452024-07-12T06:23:45LOCUS Repositório Institucional da UFV - Universidade Federal de Viçosa (UFV)false
dc.title.none.fl_str_mv Visible and near-infrared luminescent Eu3+ or Er3+ doped laponite-derived xerogels and thick films: structural and spectroscopic properties
title Visible and near-infrared luminescent Eu3+ or Er3+ doped laponite-derived xerogels and thick films: structural and spectroscopic properties
spellingShingle Visible and near-infrared luminescent Eu3+ or Er3+ doped laponite-derived xerogels and thick films: structural and spectroscopic properties
Tronto, Jairo
Clays
Laponite
Rare earth
Europium
Erbium
Xerogels
Films and silicate
title_short Visible and near-infrared luminescent Eu3+ or Er3+ doped laponite-derived xerogels and thick films: structural and spectroscopic properties
title_full Visible and near-infrared luminescent Eu3+ or Er3+ doped laponite-derived xerogels and thick films: structural and spectroscopic properties
title_fullStr Visible and near-infrared luminescent Eu3+ or Er3+ doped laponite-derived xerogels and thick films: structural and spectroscopic properties
title_full_unstemmed Visible and near-infrared luminescent Eu3+ or Er3+ doped laponite-derived xerogels and thick films: structural and spectroscopic properties
title_sort Visible and near-infrared luminescent Eu3+ or Er3+ doped laponite-derived xerogels and thick films: structural and spectroscopic properties
author Tronto, Jairo
author_facet Tronto, Jairo
Ribeiro, Sidney José Lima
Valim, João Barros
Gonçalves, Rogéria Rocha
author_role author
author2 Ribeiro, Sidney José Lima
Valim, João Barros
Gonçalves, Rogéria Rocha
author2_role author
author
author
dc.contributor.author.fl_str_mv Tronto, Jairo
Ribeiro, Sidney José Lima
Valim, João Barros
Gonçalves, Rogéria Rocha
dc.subject.por.fl_str_mv Clays
Laponite
Rare earth
Europium
Erbium
Xerogels
Films and silicate
topic Clays
Laponite
Rare earth
Europium
Erbium
Xerogels
Films and silicate
description Laponite-derived materials represent promising materials for optical applications. In this work, Eu^3+- or Er^3+-doped laponite xerogels and films were prepared from colloidal dispersion. Homogeneous, crack-free and transparent single layers were deposited on soda-lime substrates with a thickness of 10 μm. Structural and spectroscopic properties were analyzed by thermal analyses, X-ray diffractometry, transmission electron microscopy, infrared spectroscopy, and luminescence spectroscopy. The addition of a rare earth ion to the laponite does not promote any changes in thermal stability or phase transition. Laponite clay was identified after annealing up to 500 °C, with a decrease in basal spacing when the annealing temperature is changed from 100 °C to 500 °C. Enstatite polymorphs and amorphous silicate phases were observed after heat treatment at 700 °C and 900 °C. Stationary and time-dependent luminescence spectra in the visible region for Eu^3+, and 5D0 lifetime are discussed in terms of thermal treatment and structural evolution. In the layered host, the Eu^3+ ions are distributed in many different local environments. However, Eu^3+ ions were found to occupy at least two symmetry sites, and the ions are preferentially incorporated into the crystalline enstatite for the materials annealed at 700 °C and 900 °C. A 5D0 lifetime of 1.3 ms and 3.1 ms was obtained for Eu^3+ ions in an amorphous silicate and crystalline MgSiO3 local environment, respectively. Strong Er^3+ emission at the 1550 nm region was observed for the materials annealed at 900 °C, with a bandwidth of 44 nm.
publishDate 2009
dc.date.none.fl_str_mv 2009-01-15
2018-10-17T11:08:24Z
2018-10-17T11:08:24Z
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 02540584
https://doi.org/10.1016/j.matchemphys.2008.07.030
http://www.locus.ufv.br/handle/123456789/22312
identifier_str_mv 02540584
url https://doi.org/10.1016/j.matchemphys.2008.07.030
http://www.locus.ufv.br/handle/123456789/22312
dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv v. 113, n. 1, p. 71- 77, jan. 2009
dc.rights.driver.fl_str_mv Elsevier B.V.
info:eu-repo/semantics/openAccess
rights_invalid_str_mv Elsevier B.V.
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv pdf
application/pdf
dc.publisher.none.fl_str_mv Materials Chemistry and Physics
publisher.none.fl_str_mv Materials Chemistry and Physics
dc.source.none.fl_str_mv reponame:LOCUS Repositório Institucional da UFV
instname:Universidade Federal de Viçosa (UFV)
instacron:UFV
instname_str Universidade Federal de Viçosa (UFV)
instacron_str UFV
institution UFV
reponame_str LOCUS Repositório Institucional da UFV
collection LOCUS Repositório Institucional da UFV
repository.name.fl_str_mv LOCUS Repositório Institucional da UFV - Universidade Federal de Viçosa (UFV)
repository.mail.fl_str_mv fabiojreis@ufv.br
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