Linking Barbados Mineral Dust Aerosols to North African Sources Using Elemental Composition and Radiogenic Sr, Nd, and Pb Isotope Signatures
Large quantities of African dust are carried across the Atlantic to the Caribbean Basin and southern United States where it plays an important role in the biogeochemistry of soils and waters and in air quality. Dusts' elemental and isotopic composition was comprehensively characterized in Barba...
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Veröffentlicht in: | Journal of geophysical research. Atmospheres 2018-01, Vol.123 (2), p.1384-1400 |
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description | Large quantities of African dust are carried across the Atlantic to the Caribbean Basin and southern United States where it plays an important role in the biogeochemistry of soils and waters and in air quality. Dusts' elemental and isotopic composition was comprehensively characterized in Barbados during the summers of 2013 and 2014, the season of maximum dust transport. Although total suspended insoluble particulate matter (TSIP) mass concentrations varied significantly daily and between the two summers, the abundances (μg element/g TSIP) of 50 elements during “high‐dust days” (HDD) were similar. Aerosols were regularly enriched in Na, Cu, Zn, As, Se, Mo, Cd, Sn, Sb, and W relative to the upper continental crust. Enrichment of these elements, many of which are anthropogenically emitted, was significantly reduced during HDD, attributed to mixing and dilution with desert dust over source regions. Generally, Ti/Al, Si/Al, Ca/Al, Ti/Fe, Si/Fe, and Ca/Fe ratios during HDD differed from their respective values in hypothesized North African source regions. Nd isotope composition was relatively invariant for “low‐dust days” (LDD) and HDD. In contrast, HDD‐aerosols were more radiogenic exhibiting higher 87Sr/86Sr, 206Pb/204Pb, 207Pb/204Pb, and 208Pb/204Pb ratios compared to LDD. Generally, Barbados aerosols' composition ranged within narrow limits and was much more homogeneous than that of hypothesized African source soils. Our results suggest that summertime Barbados aerosols are dominated by a mixture of particles originating from sources in the Sahara‐Sahel regions. The Bodélé Depression, long suspected as a major source, appears to be an insignificant contributor of summertime western Atlantic dust.
Key Points
Composition of Barbados summer dust was relatively uniform compared to the variability reported for hypothesized African dust sources
Contrary to expectations, the Bodélé Depression appears to make an insignificant contribution to summertime western Atlantic dust
The elemental and isotopic composition of Barbados summer dust suggests that they are predominantly derived from the Sahara‐Sahel region |
doi_str_mv | 10.1002/2017JD027505 |
format | Article |
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Key Points
Composition of Barbados summer dust was relatively uniform compared to the variability reported for hypothesized African dust sources
Contrary to expectations, the Bodélé Depression appears to make an insignificant contribution to summertime western Atlantic dust
The elemental and isotopic composition of Barbados summer dust suggests that they are predominantly derived from the Sahara‐Sahel region</description><identifier>ISSN: 2169-897X</identifier><identifier>EISSN: 2169-8996</identifier><identifier>DOI: 10.1002/2017JD027505</identifier><language>eng</language><publisher>Washington: Blackwell Publishing Ltd</publisher><subject>Aerosols ; Air quality ; Aluminum ; Anthropogenic factors ; Antimony ; Atmospheric particulates ; Barbados ; Biogeochemistry ; Cadmium ; Chemical composition ; Continental crust ; Copper ; Dilution ; Dust ; Dust storms ; Dust transport ; elemental composition ; Geologic depressions ; Geophysics ; Iron ; Isotope composition ; Isotopes ; Lead isotopes ; long‐range transport ; Particulate emissions ; Particulate matter ; radiogenic isotopes ; Ratios ; Regions ; Sahara‐Sahel ; Selenium ; Silicon ; Soil ; Strontium 87 ; Strontium isotopes ; Suspended particulate matter ; Tin ; Titanium ; Zinc</subject><ispartof>Journal of geophysical research. Atmospheres, 2018-01, Vol.123 (2), p.1384-1400</ispartof><rights>2017. American Geophysical Union. All Rights Reserved.</rights><rights>2018. American Geophysical Union. All Rights Reserved.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c4119-665b4559cd7d8e9176bdd332e5294c9be530187fdf9a73a08575990fdc3079593</citedby><cites>FETCH-LOGICAL-c4119-665b4559cd7d8e9176bdd332e5294c9be530187fdf9a73a08575990fdc3079593</cites><orcidid>0000-0003-2169-1181 ; 0000-0001-9173-1439</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1002%2F2017JD027505$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1002%2F2017JD027505$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,776,780,1411,1427,27901,27902,45550,45551,46384,46808</link.rule.ids></links><search><creatorcontrib>Bozlaker, Ayse</creatorcontrib><creatorcontrib>Prospero, Joseph M.</creatorcontrib><creatorcontrib>Price, Jim</creatorcontrib><creatorcontrib>Chellam, Shankararaman</creatorcontrib><title>Linking Barbados Mineral Dust Aerosols to North African Sources Using Elemental Composition and Radiogenic Sr, Nd, and Pb Isotope Signatures</title><title>Journal of geophysical research. Atmospheres</title><description>Large quantities of African dust are carried across the Atlantic to the Caribbean Basin and southern United States where it plays an important role in the biogeochemistry of soils and waters and in air quality. Dusts' elemental and isotopic composition was comprehensively characterized in Barbados during the summers of 2013 and 2014, the season of maximum dust transport. Although total suspended insoluble particulate matter (TSIP) mass concentrations varied significantly daily and between the two summers, the abundances (μg element/g TSIP) of 50 elements during “high‐dust days” (HDD) were similar. Aerosols were regularly enriched in Na, Cu, Zn, As, Se, Mo, Cd, Sn, Sb, and W relative to the upper continental crust. Enrichment of these elements, many of which are anthropogenically emitted, was significantly reduced during HDD, attributed to mixing and dilution with desert dust over source regions. Generally, Ti/Al, Si/Al, Ca/Al, Ti/Fe, Si/Fe, and Ca/Fe ratios during HDD differed from their respective values in hypothesized North African source regions. Nd isotope composition was relatively invariant for “low‐dust days” (LDD) and HDD. In contrast, HDD‐aerosols were more radiogenic exhibiting higher 87Sr/86Sr, 206Pb/204Pb, 207Pb/204Pb, and 208Pb/204Pb ratios compared to LDD. Generally, Barbados aerosols' composition ranged within narrow limits and was much more homogeneous than that of hypothesized African source soils. Our results suggest that summertime Barbados aerosols are dominated by a mixture of particles originating from sources in the Sahara‐Sahel regions. The Bodélé Depression, long suspected as a major source, appears to be an insignificant contributor of summertime western Atlantic dust.
Key Points
Composition of Barbados summer dust was relatively uniform compared to the variability reported for hypothesized African dust sources
Contrary to expectations, the Bodélé Depression appears to make an insignificant contribution to summertime western Atlantic dust
The elemental and isotopic composition of Barbados summer dust suggests that they are predominantly derived from the Sahara‐Sahel region</description><subject>Aerosols</subject><subject>Air quality</subject><subject>Aluminum</subject><subject>Anthropogenic factors</subject><subject>Antimony</subject><subject>Atmospheric particulates</subject><subject>Barbados</subject><subject>Biogeochemistry</subject><subject>Cadmium</subject><subject>Chemical composition</subject><subject>Continental crust</subject><subject>Copper</subject><subject>Dilution</subject><subject>Dust</subject><subject>Dust storms</subject><subject>Dust transport</subject><subject>elemental composition</subject><subject>Geologic depressions</subject><subject>Geophysics</subject><subject>Iron</subject><subject>Isotope composition</subject><subject>Isotopes</subject><subject>Lead isotopes</subject><subject>long‐range transport</subject><subject>Particulate emissions</subject><subject>Particulate matter</subject><subject>radiogenic isotopes</subject><subject>Ratios</subject><subject>Regions</subject><subject>Sahara‐Sahel</subject><subject>Selenium</subject><subject>Silicon</subject><subject>Soil</subject><subject>Strontium 87</subject><subject>Strontium isotopes</subject><subject>Suspended particulate matter</subject><subject>Tin</subject><subject>Titanium</subject><subject>Zinc</subject><issn>2169-897X</issn><issn>2169-8996</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2018</creationdate><recordtype>article</recordtype><recordid>eNp9kNFOwjAUhhejiQS58wGaeMu0Xdd1vURAhCAakMS7pVs7LI52tl0M7-BDO8QYrzw35-Tk-8-f8wfBJYLXCMLoJoKIzkYwogSSk6AToYSFKWPJ6e9MX86DnnNb2FYKcUziTvA5V_pN6Q245TbnwjjwoLS0vAKjxnkwkNY4UzngDVgY61_BoLSq4BqsTGML6cDaHdTjSu6k9q1saHa1ccorowHXAiy5UGYjtSrAyvbBQvS_1085mDrjTS3BSm00942V7iI4K3nlZO-nd4P13fh5eB_OHyfT4WAeFjFCLEwSkseEsEJQkUqGaJILgXEkScTiguWSYIhSWoqScYo5TAkljMFSFBhSRhjuBlfHu7U17410Ptu23-jWMosgJAgmlKCW6h-pos3AWVlmtVU7bvcZgtkh8uxv5C2Oj_iHquT-XzabTZYjEmPE8Bfx5YGi</recordid><startdate>20180127</startdate><enddate>20180127</enddate><creator>Bozlaker, Ayse</creator><creator>Prospero, Joseph M.</creator><creator>Price, Jim</creator><creator>Chellam, Shankararaman</creator><general>Blackwell Publishing Ltd</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>7UA</scope><scope>8FD</scope><scope>C1K</scope><scope>F1W</scope><scope>FR3</scope><scope>H8D</scope><scope>H96</scope><scope>KL.</scope><scope>KR7</scope><scope>L.G</scope><scope>L7M</scope><orcidid>https://orcid.org/0000-0003-2169-1181</orcidid><orcidid>https://orcid.org/0000-0001-9173-1439</orcidid></search><sort><creationdate>20180127</creationdate><title>Linking Barbados Mineral Dust Aerosols to North African Sources Using Elemental Composition and Radiogenic Sr, Nd, and Pb Isotope Signatures</title><author>Bozlaker, Ayse ; Prospero, Joseph M. ; Price, Jim ; Chellam, Shankararaman</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c4119-665b4559cd7d8e9176bdd332e5294c9be530187fdf9a73a08575990fdc3079593</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2018</creationdate><topic>Aerosols</topic><topic>Air quality</topic><topic>Aluminum</topic><topic>Anthropogenic factors</topic><topic>Antimony</topic><topic>Atmospheric particulates</topic><topic>Barbados</topic><topic>Biogeochemistry</topic><topic>Cadmium</topic><topic>Chemical composition</topic><topic>Continental crust</topic><topic>Copper</topic><topic>Dilution</topic><topic>Dust</topic><topic>Dust storms</topic><topic>Dust transport</topic><topic>elemental composition</topic><topic>Geologic depressions</topic><topic>Geophysics</topic><topic>Iron</topic><topic>Isotope composition</topic><topic>Isotopes</topic><topic>Lead isotopes</topic><topic>long‐range transport</topic><topic>Particulate emissions</topic><topic>Particulate matter</topic><topic>radiogenic isotopes</topic><topic>Ratios</topic><topic>Regions</topic><topic>Sahara‐Sahel</topic><topic>Selenium</topic><topic>Silicon</topic><topic>Soil</topic><topic>Strontium 87</topic><topic>Strontium isotopes</topic><topic>Suspended particulate matter</topic><topic>Tin</topic><topic>Titanium</topic><topic>Zinc</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Bozlaker, Ayse</creatorcontrib><creatorcontrib>Prospero, Joseph M.</creatorcontrib><creatorcontrib>Price, Jim</creatorcontrib><creatorcontrib>Chellam, Shankararaman</creatorcontrib><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Technology Research Database</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>Aerospace Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Journal of geophysical research. Atmospheres</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Bozlaker, Ayse</au><au>Prospero, Joseph M.</au><au>Price, Jim</au><au>Chellam, Shankararaman</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Linking Barbados Mineral Dust Aerosols to North African Sources Using Elemental Composition and Radiogenic Sr, Nd, and Pb Isotope Signatures</atitle><jtitle>Journal of geophysical research. Atmospheres</jtitle><date>2018-01-27</date><risdate>2018</risdate><volume>123</volume><issue>2</issue><spage>1384</spage><epage>1400</epage><pages>1384-1400</pages><issn>2169-897X</issn><eissn>2169-8996</eissn><abstract>Large quantities of African dust are carried across the Atlantic to the Caribbean Basin and southern United States where it plays an important role in the biogeochemistry of soils and waters and in air quality. Dusts' elemental and isotopic composition was comprehensively characterized in Barbados during the summers of 2013 and 2014, the season of maximum dust transport. Although total suspended insoluble particulate matter (TSIP) mass concentrations varied significantly daily and between the two summers, the abundances (μg element/g TSIP) of 50 elements during “high‐dust days” (HDD) were similar. Aerosols were regularly enriched in Na, Cu, Zn, As, Se, Mo, Cd, Sn, Sb, and W relative to the upper continental crust. Enrichment of these elements, many of which are anthropogenically emitted, was significantly reduced during HDD, attributed to mixing and dilution with desert dust over source regions. Generally, Ti/Al, Si/Al, Ca/Al, Ti/Fe, Si/Fe, and Ca/Fe ratios during HDD differed from their respective values in hypothesized North African source regions. Nd isotope composition was relatively invariant for “low‐dust days” (LDD) and HDD. In contrast, HDD‐aerosols were more radiogenic exhibiting higher 87Sr/86Sr, 206Pb/204Pb, 207Pb/204Pb, and 208Pb/204Pb ratios compared to LDD. Generally, Barbados aerosols' composition ranged within narrow limits and was much more homogeneous than that of hypothesized African source soils. Our results suggest that summertime Barbados aerosols are dominated by a mixture of particles originating from sources in the Sahara‐Sahel regions. The Bodélé Depression, long suspected as a major source, appears to be an insignificant contributor of summertime western Atlantic dust.
Key Points
Composition of Barbados summer dust was relatively uniform compared to the variability reported for hypothesized African dust sources
Contrary to expectations, the Bodélé Depression appears to make an insignificant contribution to summertime western Atlantic dust
The elemental and isotopic composition of Barbados summer dust suggests that they are predominantly derived from the Sahara‐Sahel region</abstract><cop>Washington</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1002/2017JD027505</doi><tpages>17</tpages><orcidid>https://orcid.org/0000-0003-2169-1181</orcidid><orcidid>https://orcid.org/0000-0001-9173-1439</orcidid><oa>free_for_read</oa></addata></record> |
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subjects | Aerosols Air quality Aluminum Anthropogenic factors Antimony Atmospheric particulates Barbados Biogeochemistry Cadmium Chemical composition Continental crust Copper Dilution Dust Dust storms Dust transport elemental composition Geologic depressions Geophysics Iron Isotope composition Isotopes Lead isotopes long‐range transport Particulate emissions Particulate matter radiogenic isotopes Ratios Regions Sahara‐Sahel Selenium Silicon Soil Strontium 87 Strontium isotopes Suspended particulate matter Tin Titanium Zinc |
title | Linking Barbados Mineral Dust Aerosols to North African Sources Using Elemental Composition and Radiogenic Sr, Nd, and Pb Isotope Signatures |
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