Post 17th-Century Changes of European PAH Emissions Recorded in High-Altitude Alpine Snow and Ice
International audience The occurrence of organic pollutants in European Alpine snow/ice has been reconstructed over the past three centuries using a new online extraction method for polycyclic aromatic hydrocarbons (PAH) followed by liquid chromatographic determination. The meltwater flow from a con...
Published in: | Environmental Science & Technology |
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Main Authors: | , , , , , , , , , , , |
Other Authors: | , , , , , , , , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
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HAL CCSD
2010
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Online Access: | https://hal-insu.archives-ouvertes.fr/insu-00562406 https://doi.org/10.1021/es903365s |
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Université de Nantes: HAL-UNIV-NANTES |
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English |
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[SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology |
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[SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology Gabrieli, J. Vallelonga, P. Cozzi, G. Gabrielli, P. Gambaro, A. Sigl, M. Decet, F. Schwikowski, M. Gggeler, H. Boutron, C. Cescon, P. Barbante, C. Post 17th-Century Changes of European PAH Emissions Recorded in High-Altitude Alpine Snow and Ice |
topic_facet |
[SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology |
description |
International audience The occurrence of organic pollutants in European Alpine snow/ice has been reconstructed over the past three centuries using a new online extraction method for polycyclic aromatic hydrocarbons (PAH) followed by liquid chromatographic determination. The meltwater flow from a continuous ice core melting system was split into two aliquots, with one aliquot directed to an inductively coupled plasma quadrupole mass spectrometer for continuous trace elements determinations and the second introduced into a solid phase C18 (SPE) cartridge for semicontinuous PAH extraction. The depth resolution for PAH extractions ranged from 40 to 70 cm, and corresponds to 0.7−5 years per sample. The concentrations of 11 PAH were determined in dated snow/ice samples to reconstruct the atmospheric concentration of these compounds in Europe for the last 300 years. The PAH pattern is dominated by phenanthrene (Phe), fluoranthene (Fla), and pyrene (Pyr), which represent 60−80% of the total PAH mass. Before 1875 the sum of PAH concentration (ΣPAH) was very low with total mean concentrations less than 2 ng/kg and 0.08 ng/kg for the heavier compounds (ΣPAH*, more than four aromatic rings). During the first phase of the industrial revolution (1770−1830) the PAH deposition showed a weak increase which became much greater from the start of the second phase of the industrial revolution at the end of 19th Century. In the 1920s, economic recession in Europe decreased PAH emissions until the 1930s when they increased again and reached a maximum concentration of 32 ng/kg from 1945 to 1955. From 1955 to 1975 the PAH concentrations decreased significantly, reflecting improvements in emission controls especially from major point sources, while from 1975 to 2003 they rose to levels equivalent to those in 1910. The Fla/(Fla+Pyr) ratio is often used for source assignment and here indicates an increase in the relative contribution of gasoline and diesel combustion with respect to coal and wood burning from 1860 to the 1980s. This ... |
author2 |
Environmental Sciences Department University of Ca’ Foscari Venice, Italy Institute for the Dynamics of Environmental Processes-CNR Environmental Protection Agency of Veneto (ARPAV) Environmental Protection Agency of Veneto 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) Paul Scherrer Institute (PSI) Department of Chemistry and Biochemistry University of Bern Oeschger Centre for Climate Change Research (OCCR) CHANG (CHANG) Laboratoire d'étude des transferts en hydrologie et environnement (LTHE) 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)-Institut National Polytechnique de Grenoble (INPG)-Centre National de la Recherche Scientifique (CNRS)-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)-Institut National Polytechnique de Grenoble (INPG)-Centre National de la Recherche Scientifique (CNRS) Department of Environmental Sciences Università degli Studi di Milano-Bicocca = University of Milano-Bicocca (UNIMIB) European Project: |
format |
Article in Journal/Newspaper |
author |
Gabrieli, J. Vallelonga, P. Cozzi, G. Gabrielli, P. Gambaro, A. Sigl, M. Decet, F. Schwikowski, M. Gggeler, H. Boutron, C. Cescon, P. Barbante, C. |
author_facet |
Gabrieli, J. Vallelonga, P. Cozzi, G. Gabrielli, P. Gambaro, A. Sigl, M. Decet, F. Schwikowski, M. Gggeler, H. Boutron, C. Cescon, P. Barbante, C. |
author_sort |
Gabrieli, J. |
title |
Post 17th-Century Changes of European PAH Emissions Recorded in High-Altitude Alpine Snow and Ice |
title_short |
Post 17th-Century Changes of European PAH Emissions Recorded in High-Altitude Alpine Snow and Ice |
title_full |
Post 17th-Century Changes of European PAH Emissions Recorded in High-Altitude Alpine Snow and Ice |
title_fullStr |
Post 17th-Century Changes of European PAH Emissions Recorded in High-Altitude Alpine Snow and Ice |
title_full_unstemmed |
Post 17th-Century Changes of European PAH Emissions Recorded in High-Altitude Alpine Snow and Ice |
title_sort |
post 17th-century changes of european pah emissions recorded in high-altitude alpine snow and ice |
publisher |
HAL CCSD |
publishDate |
2010 |
url |
https://hal-insu.archives-ouvertes.fr/insu-00562406 https://doi.org/10.1021/es903365s |
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ENVELOPE(-55.731,-55.731,49.933,49.933) |
geographic |
Major Point |
geographic_facet |
Major Point |
genre |
ice core |
genre_facet |
ice core |
op_source |
ISSN: 0013-936X EISSN: 1520-5851 Environmental Science and Technology https://hal-insu.archives-ouvertes.fr/insu-00562406 Environmental Science and Technology, 2010, 44 (9), pp.3260-3266. ⟨10.1021/es903365s⟩ |
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info:eu-repo/semantics/altIdentifier/doi/10.1021/es903365s insu-00562406 https://hal-insu.archives-ouvertes.fr/insu-00562406 BIBCODE: 10.1021/es903365s doi:10.1021/es903365s |
op_doi |
https://doi.org/10.1021/es903365s |
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Environmental Science & Technology |
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ftunivnantes:oai:HAL:insu-00562406v1 2023-05-15T16:39:27+02:00 Post 17th-Century Changes of European PAH Emissions Recorded in High-Altitude Alpine Snow and Ice Gabrieli, J. Vallelonga, P. Cozzi, G. Gabrielli, P. Gambaro, A. Sigl, M. Decet, F. Schwikowski, M. Gggeler, H. Boutron, C. Cescon, P. Barbante, C. Environmental Sciences Department University of Ca’ Foscari Venice, Italy Institute for the Dynamics of Environmental Processes-CNR Environmental Protection Agency of Veneto (ARPAV) Environmental Protection Agency of Veneto 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) Paul Scherrer Institute (PSI) Department of Chemistry and Biochemistry University of Bern Oeschger Centre for Climate Change Research (OCCR) CHANG (CHANG) Laboratoire d'étude des transferts en hydrologie et environnement (LTHE) 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)-Institut National Polytechnique de Grenoble (INPG)-Centre National de la Recherche Scientifique (CNRS)-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)-Institut National Polytechnique de Grenoble (INPG)-Centre National de la Recherche Scientifique (CNRS) Department of Environmental Sciences Università degli Studi di Milano-Bicocca = University of Milano-Bicocca (UNIMIB) European Project: 2010-05 https://hal-insu.archives-ouvertes.fr/insu-00562406 https://doi.org/10.1021/es903365s en eng HAL CCSD American Chemical Society info:eu-repo/semantics/altIdentifier/doi/10.1021/es903365s insu-00562406 https://hal-insu.archives-ouvertes.fr/insu-00562406 BIBCODE: 10.1021/es903365s doi:10.1021/es903365s ISSN: 0013-936X EISSN: 1520-5851 Environmental Science and Technology https://hal-insu.archives-ouvertes.fr/insu-00562406 Environmental Science and Technology, 2010, 44 (9), pp.3260-3266. ⟨10.1021/es903365s⟩ [SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology info:eu-repo/semantics/article Journal articles 2010 ftunivnantes https://doi.org/10.1021/es903365s 2023-03-01T00:30:58Z International audience The occurrence of organic pollutants in European Alpine snow/ice has been reconstructed over the past three centuries using a new online extraction method for polycyclic aromatic hydrocarbons (PAH) followed by liquid chromatographic determination. The meltwater flow from a continuous ice core melting system was split into two aliquots, with one aliquot directed to an inductively coupled plasma quadrupole mass spectrometer for continuous trace elements determinations and the second introduced into a solid phase C18 (SPE) cartridge for semicontinuous PAH extraction. The depth resolution for PAH extractions ranged from 40 to 70 cm, and corresponds to 0.7−5 years per sample. The concentrations of 11 PAH were determined in dated snow/ice samples to reconstruct the atmospheric concentration of these compounds in Europe for the last 300 years. The PAH pattern is dominated by phenanthrene (Phe), fluoranthene (Fla), and pyrene (Pyr), which represent 60−80% of the total PAH mass. Before 1875 the sum of PAH concentration (ΣPAH) was very low with total mean concentrations less than 2 ng/kg and 0.08 ng/kg for the heavier compounds (ΣPAH*, more than four aromatic rings). During the first phase of the industrial revolution (1770−1830) the PAH deposition showed a weak increase which became much greater from the start of the second phase of the industrial revolution at the end of 19th Century. In the 1920s, economic recession in Europe decreased PAH emissions until the 1930s when they increased again and reached a maximum concentration of 32 ng/kg from 1945 to 1955. From 1955 to 1975 the PAH concentrations decreased significantly, reflecting improvements in emission controls especially from major point sources, while from 1975 to 2003 they rose to levels equivalent to those in 1910. The Fla/(Fla+Pyr) ratio is often used for source assignment and here indicates an increase in the relative contribution of gasoline and diesel combustion with respect to coal and wood burning from 1860 to the 1980s. This ... Article in Journal/Newspaper ice core Université de Nantes: HAL-UNIV-NANTES Major Point ENVELOPE(-55.731,-55.731,49.933,49.933) Environmental Science & Technology 44 9 3260 3266 |