Visible and near-infrared luminescent Eu3+ or Er3+ doped laponite-derived xerogels and thick films: structural and spectroscopic properties
Autor(a) principal: | |
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Data de Publicação: | 2009 |
Outros Autores: | , , |
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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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 |
_version_ |
1822610549911846912 |