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The Atmospheric Distributions of Trace Metals, Trace Organics and Nitrogen Species over the North Sea [and Discussion]
A 15 month survey was carried out into the distributions of trace metals, trace organics and nitrogen species in particulate and rainwater samples collected from the atmosphere over the southern North Sea. This is the first time a comprehensive and reliable data-set of this kind has been obtained fo...
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Published in: | Philosophical transactions of the Royal Society of London. Series A: Mathematical, physical, and engineering sciences physical, and engineering sciences, 1993-06, Vol.343 (1669), p.543-556 |
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creator | Chester, R. Bradshaw, G. F. Ottley, C. J. Harrison, R. M. Merrett, J. L. Preston, M. R. Rendell, A. R. Kane, M. M. Jickells, T. D. Millward, G. E. Simpson, J. H. Hydes, D. J. |
description | A 15 month survey was carried out into the distributions of trace metals, trace organics and nitrogen species in particulate
and rainwater samples collected from the atmosphere over the southern North Sea. This is the first time a comprehensive and
reliable data-set of this kind has been obtained for a coastal region from collections made at sea. Trace metals. There is
a south-north decrease in the emission of trace metals to the atmosphere from the land masses surrounding the North Sea. `End-member'
aerosol trace metal concentrations have been identified for the three major source regions; i.e. continental Europe, U.K.
and the open-sea, and indicate that, in general, aerosols from air masses which have crossed continental Europe are richer
in some trace metals (e.g. Zn and Pb) than those from air masses which have crossed the U.K. There are short-term variations
in the concentrations of trace metals in aerosols over the North Sea; however, on an integrated long-term basis the concentrations
reflect land-based source emission strengths, and increase towards the south of the region. There is also pronounced short
term variability in the concentrations of trace metals in rainwaters collected over the North Sea, but separate contributions
from marine, crustal and anthropogenic sources can be identified. Atmospheric fluxes contribute substantially to the total
inputs of trace metals to the North Sea, with both `wet' and `dry' deposition processes being important. Particulate trace
organics. The distributions of three main hydrocarbon classes were studied; i.e. saturated hydrocarbons (n-alkanes), PAH (polynuclear
aromatic hydrocarbons) and UCM (uncharacterized complex material). Carbon preference indices of n-alkanes suggest that terrestrial
sources dominate, with marine sources being insignificant. In terms of air mass origins, trace organic concentrations are
ranked in the order: continental Europe > U.K. > open sea. In terms of air mass origins, the concentrations of trace organics
and some trace metals (e.g. Zn and Pb) are higher in aerosols having a continental European than U.K. source. However, on
the basis of predominant air mass trajectories over the survey period, the major source of both trace organics and trace metals
to the North Sea atmosphere was air which had recently crossed over the U.K. Nitrogen species. Compared to the North Atlantic
sea water inflow, the atmosphere is a minor source of nitrogen species to the North Sea. However, atmospheric |
doi_str_mv | 10.1098/rsta.1993.0065 |
format | article |
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and rainwater samples collected from the atmosphere over the southern North Sea. This is the first time a comprehensive and
reliable data-set of this kind has been obtained for a coastal region from collections made at sea. Trace metals. There is
a south-north decrease in the emission of trace metals to the atmosphere from the land masses surrounding the North Sea. `End-member'
aerosol trace metal concentrations have been identified for the three major source regions; i.e. continental Europe, U.K.
and the open-sea, and indicate that, in general, aerosols from air masses which have crossed continental Europe are richer
in some trace metals (e.g. Zn and Pb) than those from air masses which have crossed the U.K. There are short-term variations
in the concentrations of trace metals in aerosols over the North Sea; however, on an integrated long-term basis the concentrations
reflect land-based source emission strengths, and increase towards the south of the region. There is also pronounced short
term variability in the concentrations of trace metals in rainwaters collected over the North Sea, but separate contributions
from marine, crustal and anthropogenic sources can be identified. Atmospheric fluxes contribute substantially to the total
inputs of trace metals to the North Sea, with both `wet' and `dry' deposition processes being important. Particulate trace
organics. The distributions of three main hydrocarbon classes were studied; i.e. saturated hydrocarbons (n-alkanes), PAH (polynuclear
aromatic hydrocarbons) and UCM (uncharacterized complex material). Carbon preference indices of n-alkanes suggest that terrestrial
sources dominate, with marine sources being insignificant. In terms of air mass origins, trace organic concentrations are
ranked in the order: continental Europe > U.K. > open sea. In terms of air mass origins, the concentrations of trace organics
and some trace metals (e.g. Zn and Pb) are higher in aerosols having a continental European than U.K. source. However, on
the basis of predominant air mass trajectories over the survey period, the major source of both trace organics and trace metals
to the North Sea atmosphere was air which had recently crossed over the U.K. Nitrogen species. Compared to the North Atlantic
sea water inflow, the atmosphere is a minor source of nitrogen species to the North Sea. However, atmospheric nitrogen inputs
constitute at least 25% of the terrestrial inputs, and may provide the dominant source of nitrogen in stratified areas of
the North Sea remote from riverine inputs. `Wet' deposition processes dominate the total nitrogen flux to the sea surface,
but `dry' deposition of gaseous and particulate species contributes significantly.</description><identifier>ISSN: 1364-503X</identifier><identifier>ISSN: 0962-8428</identifier><identifier>EISSN: 1471-2962</identifier><identifier>EISSN: 2054-0299</identifier><identifier>DOI: 10.1098/rsta.1993.0065</identifier><language>eng</language><publisher>London: The Royal Society</publisher><subject>Aerosols ; Air masses ; Atmospherics ; Land ; Nitrogen ; Particulate matter ; Polycyclic aromatic hydrocarbons ; Rain ; Seas ; Wet atmospheric deposition</subject><ispartof>Philosophical transactions of the Royal Society of London. Series A: Mathematical, physical, and engineering sciences, 1993-06, Vol.343 (1669), p.543-556</ispartof><rights>Copyright 1993 The Royal Society</rights><rights>Scanned images copyright © 2017, Royal Society</rights><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a526t-fbf0474ef087cacc54da75fc8fd87c31ac8d81c6270c025112aea3ecd73fca2e3</citedby><cites>FETCH-LOGICAL-a526t-fbf0474ef087cacc54da75fc8fd87c31ac8d81c6270c025112aea3ecd73fca2e3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/54052$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/54052$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>314,777,781,27905,27906,58219,58452</link.rule.ids></links><search><creatorcontrib>Chester, R.</creatorcontrib><creatorcontrib>Bradshaw, G. F.</creatorcontrib><creatorcontrib>Ottley, C. J.</creatorcontrib><creatorcontrib>Harrison, R. M.</creatorcontrib><creatorcontrib>Merrett, J. L.</creatorcontrib><creatorcontrib>Preston, M. R.</creatorcontrib><creatorcontrib>Rendell, A. R.</creatorcontrib><creatorcontrib>Kane, M. M.</creatorcontrib><creatorcontrib>Jickells, T. D.</creatorcontrib><creatorcontrib>Millward, G. E.</creatorcontrib><creatorcontrib>Simpson, J. H.</creatorcontrib><creatorcontrib>Hydes, D. J.</creatorcontrib><title>The Atmospheric Distributions of Trace Metals, Trace Organics and Nitrogen Species over the North Sea [and Discussion]</title><title>Philosophical transactions of the Royal Society of London. Series A: Mathematical, physical, and engineering sciences</title><addtitle>Phil. Trans. R. Soc. Lond. A</addtitle><description>A 15 month survey was carried out into the distributions of trace metals, trace organics and nitrogen species in particulate
and rainwater samples collected from the atmosphere over the southern North Sea. This is the first time a comprehensive and
reliable data-set of this kind has been obtained for a coastal region from collections made at sea. Trace metals. There is
a south-north decrease in the emission of trace metals to the atmosphere from the land masses surrounding the North Sea. `End-member'
aerosol trace metal concentrations have been identified for the three major source regions; i.e. continental Europe, U.K.
and the open-sea, and indicate that, in general, aerosols from air masses which have crossed continental Europe are richer
in some trace metals (e.g. Zn and Pb) than those from air masses which have crossed the U.K. There are short-term variations
in the concentrations of trace metals in aerosols over the North Sea; however, on an integrated long-term basis the concentrations
reflect land-based source emission strengths, and increase towards the south of the region. There is also pronounced short
term variability in the concentrations of trace metals in rainwaters collected over the North Sea, but separate contributions
from marine, crustal and anthropogenic sources can be identified. Atmospheric fluxes contribute substantially to the total
inputs of trace metals to the North Sea, with both `wet' and `dry' deposition processes being important. Particulate trace
organics. The distributions of three main hydrocarbon classes were studied; i.e. saturated hydrocarbons (n-alkanes), PAH (polynuclear
aromatic hydrocarbons) and UCM (uncharacterized complex material). Carbon preference indices of n-alkanes suggest that terrestrial
sources dominate, with marine sources being insignificant. In terms of air mass origins, trace organic concentrations are
ranked in the order: continental Europe > U.K. > open sea. In terms of air mass origins, the concentrations of trace organics
and some trace metals (e.g. Zn and Pb) are higher in aerosols having a continental European than U.K. source. However, on
the basis of predominant air mass trajectories over the survey period, the major source of both trace organics and trace metals
to the North Sea atmosphere was air which had recently crossed over the U.K. Nitrogen species. Compared to the North Atlantic
sea water inflow, the atmosphere is a minor source of nitrogen species to the North Sea. However, atmospheric nitrogen inputs
constitute at least 25% of the terrestrial inputs, and may provide the dominant source of nitrogen in stratified areas of
the North Sea remote from riverine inputs. `Wet' deposition processes dominate the total nitrogen flux to the sea surface,
but `dry' deposition of gaseous and particulate species contributes significantly.</description><subject>Aerosols</subject><subject>Air masses</subject><subject>Atmospherics</subject><subject>Land</subject><subject>Nitrogen</subject><subject>Particulate matter</subject><subject>Polycyclic aromatic hydrocarbons</subject><subject>Rain</subject><subject>Seas</subject><subject>Wet atmospheric deposition</subject><issn>1364-503X</issn><issn>0962-8428</issn><issn>1471-2962</issn><issn>2054-0299</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1993</creationdate><recordtype>article</recordtype><recordid>eNp9kF1rFDEUhgdRsFZvvfAqP8DZnkyS-biSpVYr1BbcFQSRkGZOdrJsJ0OSWVl_vZnZIhaxVzkn532f85FlryksKDT1mQ9RLWjTsAVAKZ5kJ5RXNC-asniaYlbyXAD79jx7EcIWgNJSFCfZft0hWcY7F4YOvdXkvQ3R29sxWtcH4gxZe6WRfMaoduHtfXbjN6q3OhDVt-TaRu822JPVgNpiMu3Rk5i4187HjqxQke-TMKH1GEIC_3iZPTOJh6_u39Ps64eL9fllfnXz8dP58ipXoihjbm4N8IqjgbrSSmvBW1UJo2vTpg9Gla7bmuqyqEBDISgtFCqGuq2Y0apAdpotjlztXQgejRy8vVP-ICnI6WpyupqcrianqyVDOBq8O6TBXFooHuTWjb5PqfyyWi-TGPaMM0vLspFQMwoV5xzkLzvMuEkgk0DaEEaUs-xhm3-7sse6_nfWN0fXNkTn_2wmOIgiFd8di53ddD-tR_mAPaO06yP2cZ51nlKkwIy7nRxakwjwKMEdhsT428t-Ay5kyrk</recordid><startdate>19930615</startdate><enddate>19930615</enddate><creator>Chester, R.</creator><creator>Bradshaw, G. F.</creator><creator>Ottley, C. J.</creator><creator>Harrison, R. M.</creator><creator>Merrett, J. L.</creator><creator>Preston, M. R.</creator><creator>Rendell, A. R.</creator><creator>Kane, M. M.</creator><creator>Jickells, T. D.</creator><creator>Millward, G. E.</creator><creator>Simpson, J. H.</creator><creator>Hydes, D. J.</creator><general>The Royal Society</general><scope>AAYXX</scope><scope>CITATION</scope></search><sort><creationdate>19930615</creationdate><title>The Atmospheric Distributions of Trace Metals, Trace Organics and Nitrogen Species over the North Sea [and Discussion]</title><author>Chester, R. ; Bradshaw, G. F. ; Ottley, C. J. ; Harrison, R. M. ; Merrett, J. L. ; Preston, M. R. ; Rendell, A. R. ; Kane, M. M. ; Jickells, T. D. ; Millward, G. E. ; Simpson, J. H. ; Hydes, D. J.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a526t-fbf0474ef087cacc54da75fc8fd87c31ac8d81c6270c025112aea3ecd73fca2e3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1993</creationdate><topic>Aerosols</topic><topic>Air masses</topic><topic>Atmospherics</topic><topic>Land</topic><topic>Nitrogen</topic><topic>Particulate matter</topic><topic>Polycyclic aromatic hydrocarbons</topic><topic>Rain</topic><topic>Seas</topic><topic>Wet atmospheric deposition</topic><toplevel>online_resources</toplevel><creatorcontrib>Chester, R.</creatorcontrib><creatorcontrib>Bradshaw, G. F.</creatorcontrib><creatorcontrib>Ottley, C. J.</creatorcontrib><creatorcontrib>Harrison, R. M.</creatorcontrib><creatorcontrib>Merrett, J. L.</creatorcontrib><creatorcontrib>Preston, M. R.</creatorcontrib><creatorcontrib>Rendell, A. R.</creatorcontrib><creatorcontrib>Kane, M. M.</creatorcontrib><creatorcontrib>Jickells, T. D.</creatorcontrib><creatorcontrib>Millward, G. E.</creatorcontrib><creatorcontrib>Simpson, J. H.</creatorcontrib><creatorcontrib>Hydes, D. J.</creatorcontrib><collection>CrossRef</collection><jtitle>Philosophical transactions of the Royal Society of London. Series A: Mathematical, physical, and engineering sciences</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Chester, R.</au><au>Bradshaw, G. F.</au><au>Ottley, C. J.</au><au>Harrison, R. M.</au><au>Merrett, J. L.</au><au>Preston, M. R.</au><au>Rendell, A. R.</au><au>Kane, M. M.</au><au>Jickells, T. D.</au><au>Millward, G. E.</au><au>Simpson, J. H.</au><au>Hydes, D. J.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>The Atmospheric Distributions of Trace Metals, Trace Organics and Nitrogen Species over the North Sea [and Discussion]</atitle><jtitle>Philosophical transactions of the Royal Society of London. Series A: Mathematical, physical, and engineering sciences</jtitle><stitle>Phil. Trans. R. Soc. Lond. A</stitle><date>1993-06-15</date><risdate>1993</risdate><volume>343</volume><issue>1669</issue><spage>543</spage><epage>556</epage><pages>543-556</pages><issn>1364-503X</issn><issn>0962-8428</issn><eissn>1471-2962</eissn><eissn>2054-0299</eissn><abstract>A 15 month survey was carried out into the distributions of trace metals, trace organics and nitrogen species in particulate
and rainwater samples collected from the atmosphere over the southern North Sea. This is the first time a comprehensive and
reliable data-set of this kind has been obtained for a coastal region from collections made at sea. Trace metals. There is
a south-north decrease in the emission of trace metals to the atmosphere from the land masses surrounding the North Sea. `End-member'
aerosol trace metal concentrations have been identified for the three major source regions; i.e. continental Europe, U.K.
and the open-sea, and indicate that, in general, aerosols from air masses which have crossed continental Europe are richer
in some trace metals (e.g. Zn and Pb) than those from air masses which have crossed the U.K. There are short-term variations
in the concentrations of trace metals in aerosols over the North Sea; however, on an integrated long-term basis the concentrations
reflect land-based source emission strengths, and increase towards the south of the region. There is also pronounced short
term variability in the concentrations of trace metals in rainwaters collected over the North Sea, but separate contributions
from marine, crustal and anthropogenic sources can be identified. Atmospheric fluxes contribute substantially to the total
inputs of trace metals to the North Sea, with both `wet' and `dry' deposition processes being important. Particulate trace
organics. The distributions of three main hydrocarbon classes were studied; i.e. saturated hydrocarbons (n-alkanes), PAH (polynuclear
aromatic hydrocarbons) and UCM (uncharacterized complex material). Carbon preference indices of n-alkanes suggest that terrestrial
sources dominate, with marine sources being insignificant. In terms of air mass origins, trace organic concentrations are
ranked in the order: continental Europe > U.K. > open sea. In terms of air mass origins, the concentrations of trace organics
and some trace metals (e.g. Zn and Pb) are higher in aerosols having a continental European than U.K. source. However, on
the basis of predominant air mass trajectories over the survey period, the major source of both trace organics and trace metals
to the North Sea atmosphere was air which had recently crossed over the U.K. Nitrogen species. Compared to the North Atlantic
sea water inflow, the atmosphere is a minor source of nitrogen species to the North Sea. However, atmospheric nitrogen inputs
constitute at least 25% of the terrestrial inputs, and may provide the dominant source of nitrogen in stratified areas of
the North Sea remote from riverine inputs. `Wet' deposition processes dominate the total nitrogen flux to the sea surface,
but `dry' deposition of gaseous and particulate species contributes significantly.</abstract><cop>London</cop><pub>The Royal Society</pub><doi>10.1098/rsta.1993.0065</doi><tpages>14</tpages></addata></record> |
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ispartof | Philosophical transactions of the Royal Society of London. Series A: Mathematical, physical, and engineering sciences, 1993-06, Vol.343 (1669), p.543-556 |
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language | eng |
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source | JSTOR Archival Journals and Primary Sources Collection; Royal Society Publishing Jisc Collections Royal Society Journals Read & Publish Transitional Agreement 2025 (reading list) |
subjects | Aerosols Air masses Atmospherics Land Nitrogen Particulate matter Polycyclic aromatic hydrocarbons Rain Seas Wet atmospheric deposition |
title | The Atmospheric Distributions of Trace Metals, Trace Organics and Nitrogen Species over the North Sea [and Discussion] |
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