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Optically Stimulated Luminescence Sensitivity of Quartz for Provenance Analysis

Finding the source or provenance of quartz grains occurring in a specific location allows us to constrain their transport pathway, which is crucial information to solve diverse problems in geosciences and related fields. The optically stimulated luminescence (OSL) sensitivity (light intensity per un...

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Autores principales: Sawakuchi, André Oliveira, Rodrigues, Fernanda Costa Gonçalves, Mineli, Thays Desiree, Mendes, Vinícius Ribau, Melo, Dayane Batista, Chiessi, Cristiano Mazur, Giannini, Paulo César Fonseca
Formato: Online Artículo Texto
Lenguaje:English
Publicado: MDPI 2020
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7189674/
https://www.ncbi.nlm.nih.gov/pubmed/31941007
http://dx.doi.org/10.3390/mps3010006
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author Sawakuchi, André Oliveira
Rodrigues, Fernanda Costa Gonçalves
Mineli, Thays Desiree
Mendes, Vinícius Ribau
Melo, Dayane Batista
Chiessi, Cristiano Mazur
Giannini, Paulo César Fonseca
author_facet Sawakuchi, André Oliveira
Rodrigues, Fernanda Costa Gonçalves
Mineli, Thays Desiree
Mendes, Vinícius Ribau
Melo, Dayane Batista
Chiessi, Cristiano Mazur
Giannini, Paulo César Fonseca
author_sort Sawakuchi, André Oliveira
collection PubMed
description Finding the source or provenance of quartz grains occurring in a specific location allows us to constrain their transport pathway, which is crucial information to solve diverse problems in geosciences and related fields. The optically stimulated luminescence (OSL) sensitivity (light intensity per unit mass per unit radiation dose) has a high capacity for discrimination of quartz sediment grains and represents a promising technique for provenance analysis. In this study, we tested the use of quartz OSL sensitivity (ultraviolet emission) measured under different preheating temperatures and with blue light stimulation at room temperature (~20 °C) for sediment provenance analysis. Quartz OSL sensitivity measured at 20 °C is positively correlated with the sensitivity of an OSL signal measured using procedures (preheat at 190 °C for 10 s, blue stimulation at 125 °C and initial 1 s of light emission) to increase the contribution of the fast OSL component, which has been successfully applied for sediment provenance analysis. The higher OSL signal intensity measured without preheating and with light stimulation at room temperature allows the use of lower given doses, thus reducing measurement time. Additionally, the OSL sensitivity measured at 20 °C in polymineral silt samples of a marine sediment core is also suitable for provenance analysis, as demonstrated by comparison with other independent proxies. OSL signals obtained through light stimulation at room temperature have thus the potential to considerably expand measurement possibilities, including in situ measurements using portable OSL readers.
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spelling pubmed-71896742020-05-01 Optically Stimulated Luminescence Sensitivity of Quartz for Provenance Analysis Sawakuchi, André Oliveira Rodrigues, Fernanda Costa Gonçalves Mineli, Thays Desiree Mendes, Vinícius Ribau Melo, Dayane Batista Chiessi, Cristiano Mazur Giannini, Paulo César Fonseca Methods Protoc Article Finding the source or provenance of quartz grains occurring in a specific location allows us to constrain their transport pathway, which is crucial information to solve diverse problems in geosciences and related fields. The optically stimulated luminescence (OSL) sensitivity (light intensity per unit mass per unit radiation dose) has a high capacity for discrimination of quartz sediment grains and represents a promising technique for provenance analysis. In this study, we tested the use of quartz OSL sensitivity (ultraviolet emission) measured under different preheating temperatures and with blue light stimulation at room temperature (~20 °C) for sediment provenance analysis. Quartz OSL sensitivity measured at 20 °C is positively correlated with the sensitivity of an OSL signal measured using procedures (preheat at 190 °C for 10 s, blue stimulation at 125 °C and initial 1 s of light emission) to increase the contribution of the fast OSL component, which has been successfully applied for sediment provenance analysis. The higher OSL signal intensity measured without preheating and with light stimulation at room temperature allows the use of lower given doses, thus reducing measurement time. Additionally, the OSL sensitivity measured at 20 °C in polymineral silt samples of a marine sediment core is also suitable for provenance analysis, as demonstrated by comparison with other independent proxies. OSL signals obtained through light stimulation at room temperature have thus the potential to considerably expand measurement possibilities, including in situ measurements using portable OSL readers. MDPI 2020-01-13 /pmc/articles/PMC7189674/ /pubmed/31941007 http://dx.doi.org/10.3390/mps3010006 Text en © 2020 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (http://creativecommons.org/licenses/by/4.0/).
spellingShingle Article
Sawakuchi, André Oliveira
Rodrigues, Fernanda Costa Gonçalves
Mineli, Thays Desiree
Mendes, Vinícius Ribau
Melo, Dayane Batista
Chiessi, Cristiano Mazur
Giannini, Paulo César Fonseca
Optically Stimulated Luminescence Sensitivity of Quartz for Provenance Analysis
title Optically Stimulated Luminescence Sensitivity of Quartz for Provenance Analysis
title_full Optically Stimulated Luminescence Sensitivity of Quartz for Provenance Analysis
title_fullStr Optically Stimulated Luminescence Sensitivity of Quartz for Provenance Analysis
title_full_unstemmed Optically Stimulated Luminescence Sensitivity of Quartz for Provenance Analysis
title_short Optically Stimulated Luminescence Sensitivity of Quartz for Provenance Analysis
title_sort optically stimulated luminescence sensitivity of quartz for provenance analysis
topic Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7189674/
https://www.ncbi.nlm.nih.gov/pubmed/31941007
http://dx.doi.org/10.3390/mps3010006
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