Direct Determination of Rare Earth Elements at the Subpicogram per Gram Level in Antarctic Ice by ICP-SFMS Using a Desolvation System

International audience A method, based on inductively coupled plasma sector field mass spectrometry coupled with a microflow nebulizer and a desolvation system, has been developed for the direct determination of rare earth elements (REE) (La, Ce, Pr, Nd, Sm, Eu, Gd, Tb, Dy, Ho, Er, Tm, Yb, Lu) down...

Full description

Bibliographic Details
Published in:Analytical Chemistry
Main Authors: Gabrielli, Paolo, Barbante, Carlo, Turetta, Clara, Marteel, Alexandrine, Boutron, Claude, F., Cozzi, Giulio, Cairns, Warren, R. L., Ferrari, Christophe, P., Paolo Cescon, And
Other Authors: Environmental Sciences Department, University of Ca’ Foscari Venice, Italy, Institute for the Dynamics of Environmental Processes-CNR, Laboratoire de glaciologie et géophysique de l'environnement (LGGE), Observatoire des Sciences de l'Univers de Grenoble (OSUG), Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS), Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS), Polytech Grenoble, European Project for Ice Coring in Antarctica (EPICA)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2006
Subjects:
Dy
Online Access:https://insu.hal.science/insu-00375470
https://doi.org/10.1021/ac0518957
id ftunigrenoble:oai:HAL:insu-00375470v1
record_format openpolar
spelling ftunigrenoble:oai:HAL:insu-00375470v1 2024-05-12T07:53:13+00:00 Direct Determination of Rare Earth Elements at the Subpicogram per Gram Level in Antarctic Ice by ICP-SFMS Using a Desolvation System Gabrielli, Paolo Barbante, Carlo Turetta, Clara Marteel, Alexandrine Boutron, Claude, F. Cozzi, Giulio Cairns, Warren, R. L. Ferrari, Christophe, P. Paolo Cescon, And Environmental Sciences Department University of Ca’ Foscari Venice, Italy Institute for the Dynamics of Environmental Processes-CNR Laboratoire de glaciologie et géophysique de l'environnement (LGGE) Observatoire des Sciences de l'Univers de Grenoble (OSUG) Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS) Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS) Polytech Grenoble European Project for Ice Coring in Antarctica (EPICA) 2006 https://insu.hal.science/insu-00375470 https://doi.org/10.1021/ac0518957 en eng HAL CCSD American Chemical Society info:eu-repo/semantics/altIdentifier/doi/10.1021/ac0518957 insu-00375470 https://insu.hal.science/insu-00375470 doi:10.1021/ac0518957 ISSN: 0003-2700 EISSN: 1520-6882 Analytical Chemistry https://insu.hal.science/insu-00375470 Analytical Chemistry, 2006, 78 (6), pp.1883 à 1889. ⟨10.1021/ac0518957⟩ [SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology info:eu-repo/semantics/article Journal articles 2006 ftunigrenoble https://doi.org/10.1021/ac0518957 2024-04-18T03:03:14Z International audience A method, based on inductively coupled plasma sector field mass spectrometry coupled with a microflow nebulizer and a desolvation system, has been developed for the direct determination of rare earth elements (REE) (La, Ce, Pr, Nd, Sm, Eu, Gd, Tb, Dy, Ho, Er, Tm, Yb, Lu) down to the subpicogram per gram level (1 pg/g = 10-12 g g-1) in 1 mL of molten Antarctic ice. Contamination problems were carefully taken into account by adopting ultraclean procedures during the sample pretreatment phases. The use of a desolvation system for sample introduction during the analysis greatly reduced spectral interferences from oxide formation; the residual interfering contributions were calculated and subtracted whenever necessary. A matched calibration curve method was used for the quantification of the analytes. Instrumental detection limits ranged from 0.001 pg/g for Ho, Tm, and Lu to 0.03 pg/g for Gd. The precision, in terms of relative standard deviation on 10 replicates, ranged from 2% for La, Ce, Pr, and Lu, up to 10% for Er, Tm, and Yb. This methodology allowed the direct determination of REE in a 1-mL sample of ancient Antarctic ice with concentration ranges between 0.006 and 0.4 pg/g for Tm and 0.9−60 pg/g for Ce. Article in Journal/Newspaper Antarc* Antarctic Université Grenoble Alpes: HAL Antarctic Dy ENVELOPE(11.369,11.369,64.834,64.834) Analytical Chemistry 78 6 1883 1889
institution Open Polar
collection Université Grenoble Alpes: HAL
op_collection_id ftunigrenoble
language English
topic [SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology
spellingShingle [SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology
Gabrielli, Paolo
Barbante, Carlo
Turetta, Clara
Marteel, Alexandrine
Boutron, Claude, F.
Cozzi, Giulio
Cairns, Warren, R. L.
Ferrari, Christophe, P.
Paolo Cescon, And
Direct Determination of Rare Earth Elements at the Subpicogram per Gram Level in Antarctic Ice by ICP-SFMS Using a Desolvation System
topic_facet [SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology
description International audience A method, based on inductively coupled plasma sector field mass spectrometry coupled with a microflow nebulizer and a desolvation system, has been developed for the direct determination of rare earth elements (REE) (La, Ce, Pr, Nd, Sm, Eu, Gd, Tb, Dy, Ho, Er, Tm, Yb, Lu) down to the subpicogram per gram level (1 pg/g = 10-12 g g-1) in 1 mL of molten Antarctic ice. Contamination problems were carefully taken into account by adopting ultraclean procedures during the sample pretreatment phases. The use of a desolvation system for sample introduction during the analysis greatly reduced spectral interferences from oxide formation; the residual interfering contributions were calculated and subtracted whenever necessary. A matched calibration curve method was used for the quantification of the analytes. Instrumental detection limits ranged from 0.001 pg/g for Ho, Tm, and Lu to 0.03 pg/g for Gd. The precision, in terms of relative standard deviation on 10 replicates, ranged from 2% for La, Ce, Pr, and Lu, up to 10% for Er, Tm, and Yb. This methodology allowed the direct determination of REE in a 1-mL sample of ancient Antarctic ice with concentration ranges between 0.006 and 0.4 pg/g for Tm and 0.9−60 pg/g for Ce.
author2 Environmental Sciences Department
University of Ca’ Foscari Venice, Italy
Institute for the Dynamics of Environmental Processes-CNR
Laboratoire de glaciologie et géophysique de l'environnement (LGGE)
Observatoire des Sciences de l'Univers de Grenoble (OSUG)
Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS)
Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)
Polytech Grenoble
European Project for Ice Coring in Antarctica (EPICA)
format Article in Journal/Newspaper
author Gabrielli, Paolo
Barbante, Carlo
Turetta, Clara
Marteel, Alexandrine
Boutron, Claude, F.
Cozzi, Giulio
Cairns, Warren, R. L.
Ferrari, Christophe, P.
Paolo Cescon, And
author_facet Gabrielli, Paolo
Barbante, Carlo
Turetta, Clara
Marteel, Alexandrine
Boutron, Claude, F.
Cozzi, Giulio
Cairns, Warren, R. L.
Ferrari, Christophe, P.
Paolo Cescon, And
author_sort Gabrielli, Paolo
title Direct Determination of Rare Earth Elements at the Subpicogram per Gram Level in Antarctic Ice by ICP-SFMS Using a Desolvation System
title_short Direct Determination of Rare Earth Elements at the Subpicogram per Gram Level in Antarctic Ice by ICP-SFMS Using a Desolvation System
title_full Direct Determination of Rare Earth Elements at the Subpicogram per Gram Level in Antarctic Ice by ICP-SFMS Using a Desolvation System
title_fullStr Direct Determination of Rare Earth Elements at the Subpicogram per Gram Level in Antarctic Ice by ICP-SFMS Using a Desolvation System
title_full_unstemmed Direct Determination of Rare Earth Elements at the Subpicogram per Gram Level in Antarctic Ice by ICP-SFMS Using a Desolvation System
title_sort direct determination of rare earth elements at the subpicogram per gram level in antarctic ice by icp-sfms using a desolvation system
publisher HAL CCSD
publishDate 2006
url https://insu.hal.science/insu-00375470
https://doi.org/10.1021/ac0518957
long_lat ENVELOPE(11.369,11.369,64.834,64.834)
geographic Antarctic
Dy
geographic_facet Antarctic
Dy
genre Antarc*
Antarctic
genre_facet Antarc*
Antarctic
op_source ISSN: 0003-2700
EISSN: 1520-6882
Analytical Chemistry
https://insu.hal.science/insu-00375470
Analytical Chemistry, 2006, 78 (6), pp.1883 à 1889. ⟨10.1021/ac0518957⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1021/ac0518957
insu-00375470
https://insu.hal.science/insu-00375470
doi:10.1021/ac0518957
op_doi https://doi.org/10.1021/ac0518957
container_title Analytical Chemistry
container_volume 78
container_issue 6
container_start_page 1883
op_container_end_page 1889
_version_ 1798841574593921024