Loading…

Dynamic light absorption of biomass-burning organic carbon photochemically aged under natural sunlight

Wood-burning aerosol produced under smoldering conditions was photochemically aged with different relative humidity (RH) and NOx conditions using a 104 m3 dual outdoor chamber under natural sunlight. Light absorption of organic carbon (OC) was measured over the course of photooxidation using a UV-vi...

Full description

Saved in:
Bibliographic Details
Published in:Atmospheric chemistry and physics 2014-02, Vol.14 (3), p.1517-1525
Main Authors: Zhong, M, Jang, M
Format: Article
Language:English
Subjects:
Citations: Items that this one cites
Items that cite this one
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
cited_by cdi_FETCH-LOGICAL-c584t-a3559b457c5a75785fa4d5fcb6312baa986fd8277d103c46a3e27d5ad97aeb4f3
cites cdi_FETCH-LOGICAL-c584t-a3559b457c5a75785fa4d5fcb6312baa986fd8277d103c46a3e27d5ad97aeb4f3
container_end_page 1525
container_issue 3
container_start_page 1517
container_title Atmospheric chemistry and physics
container_volume 14
creator Zhong, M
Jang, M
description Wood-burning aerosol produced under smoldering conditions was photochemically aged with different relative humidity (RH) and NOx conditions using a 104 m3 dual outdoor chamber under natural sunlight. Light absorption of organic carbon (OC) was measured over the course of photooxidation using a UV-visible spectrometer connected to an integrating sphere. At high RH, the color decayed rapidly. NOx slightly prolonged the color of wood smoke, suggesting that NOx promotes the formation of chromophores via secondary processes. Overall, the mass absorption cross section (integrated between 280 and 600 nm) of OC increased by 11-54% (except high RH) in the morning and then gradually decreased by 19-68% in the afternoon. This dynamic change in light absorption of wood-burning OC can be explained by two mechanisms: chromophore formation and sunlight bleaching. To investigate the effect of chemical transformation on light absorption, wood smoke particles were characterized using various spectrometers. The intensity of fluorescence, which is mainly related to polycyclic aromatic hydrocarbons (PAHs), rapidly decreased with time, indicating the potential bleaching of PAHs. A decline of levoglucosan concentrations evinced the change of primary organic aerosol with time. The aerosol water content measured by Fourier transform infrared spectroscopy showed that wood-burning aerosol became less hygroscopic as photooxidation proceeded. A similar trend in light absorption changes has been observed in ambient smoke aerosol originating from the 2012 County Line wildfire in Florida. We conclude that the biomass-burning OC becomes less light absorbing after 8-9 h sunlight exposure compared to fresh wood-burning OC.
doi_str_mv 10.5194/acp-14-1517-2014
format article
fullrecord <record><control><sourceid>gale_doaj_</sourceid><recordid>TN_cdi_doaj_primary_oai_doaj_org_article_19ffa925fa62436b8da4e0c0f33a4673</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><galeid>A481418149</galeid><doaj_id>oai_doaj_org_article_19ffa925fa62436b8da4e0c0f33a4673</doaj_id><sourcerecordid>A481418149</sourcerecordid><originalsourceid>FETCH-LOGICAL-c584t-a3559b457c5a75785fa4d5fcb6312baa986fd8277d103c46a3e27d5ad97aeb4f3</originalsourceid><addsrcrecordid>eNqNks2L3SAUxUNpodNp910GumkXmWq8arIcph_zYKDQj7XcGM1zyNNUDfT99zXzSpkHXRQR5fI75-rlVNVrSq447eE96qWh0FBOZdMSCk-qCyo60kjWwtNH9-fVi5TuCWl5gS4q--Ho8eB0Pbtpn2scUohLdsHXwdaDCwdMqRnW6J2f6hAn9IXVGIdCLPuQg96bIsd5PtY4mbFe_Whi7TGvEec6rf7B-GX1zOKczKs_52X149PH7ze3zd2Xz7ub67tG8w5yg4zzfgAuNUfJZcctwsitHgSj7YDYd8KOXSvlSAnTIJCZVo4cx16iGcCyy2p38h0D3qslugPGowro1EOhfEBhzE7PRtHeWuzb0kK0wMTQjQiGaGIZQxCSFa-3J68lhp-rSVkdXNJmntGbsCZFOwFcCGjJf6AggEAPoqBvTuiE5RHO25Aj6g1X19BRoGX3hbr6B1XWuE07eGNdqZ8J3p0JCpPNrzzhmpLafft6zpITq2NIKRr7d1CUqC1MqoRJUVBbmNQWJvYb1LO8Cg</addsrcrecordid><sourcetype>Open Website</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>1846404946</pqid></control><display><type>article</type><title>Dynamic light absorption of biomass-burning organic carbon photochemically aged under natural sunlight</title><source>Publicly Available Content (ProQuest)</source><source>Directory of Open Access Journals</source><source>Alma/SFX Local Collection</source><creator>Zhong, M ; Jang, M</creator><creatorcontrib>Zhong, M ; Jang, M</creatorcontrib><description>Wood-burning aerosol produced under smoldering conditions was photochemically aged with different relative humidity (RH) and NOx conditions using a 104 m3 dual outdoor chamber under natural sunlight. Light absorption of organic carbon (OC) was measured over the course of photooxidation using a UV-visible spectrometer connected to an integrating sphere. At high RH, the color decayed rapidly. NOx slightly prolonged the color of wood smoke, suggesting that NOx promotes the formation of chromophores via secondary processes. Overall, the mass absorption cross section (integrated between 280 and 600 nm) of OC increased by 11-54% (except high RH) in the morning and then gradually decreased by 19-68% in the afternoon. This dynamic change in light absorption of wood-burning OC can be explained by two mechanisms: chromophore formation and sunlight bleaching. To investigate the effect of chemical transformation on light absorption, wood smoke particles were characterized using various spectrometers. The intensity of fluorescence, which is mainly related to polycyclic aromatic hydrocarbons (PAHs), rapidly decreased with time, indicating the potential bleaching of PAHs. A decline of levoglucosan concentrations evinced the change of primary organic aerosol with time. The aerosol water content measured by Fourier transform infrared spectroscopy showed that wood-burning aerosol became less hygroscopic as photooxidation proceeded. A similar trend in light absorption changes has been observed in ambient smoke aerosol originating from the 2012 County Line wildfire in Florida. We conclude that the biomass-burning OC becomes less light absorbing after 8-9 h sunlight exposure compared to fresh wood-burning OC.</description><identifier>ISSN: 1680-7324</identifier><identifier>ISSN: 1680-7316</identifier><identifier>EISSN: 1680-7324</identifier><identifier>DOI: 10.5194/acp-14-1517-2014</identifier><language>eng</language><publisher>Copernicus GmbH</publisher><subject>Aerosols ; Carbon ; Light absorption ; Polycyclic aromatic hydrocarbons ; Smoke ; Spectrometers ; Sunlight ; Ultraviolet-visible spectroscopy ; Wood</subject><ispartof>Atmospheric chemistry and physics, 2014-02, Vol.14 (3), p.1517-1525</ispartof><rights>COPYRIGHT 2014 Copernicus GmbH</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c584t-a3559b457c5a75785fa4d5fcb6312baa986fd8277d103c46a3e27d5ad97aeb4f3</citedby><cites>FETCH-LOGICAL-c584t-a3559b457c5a75785fa4d5fcb6312baa986fd8277d103c46a3e27d5ad97aeb4f3</cites><orcidid>0000-0003-4211-7883</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780,860,2095,27903,27904,36992</link.rule.ids></links><search><creatorcontrib>Zhong, M</creatorcontrib><creatorcontrib>Jang, M</creatorcontrib><title>Dynamic light absorption of biomass-burning organic carbon photochemically aged under natural sunlight</title><title>Atmospheric chemistry and physics</title><description>Wood-burning aerosol produced under smoldering conditions was photochemically aged with different relative humidity (RH) and NOx conditions using a 104 m3 dual outdoor chamber under natural sunlight. Light absorption of organic carbon (OC) was measured over the course of photooxidation using a UV-visible spectrometer connected to an integrating sphere. At high RH, the color decayed rapidly. NOx slightly prolonged the color of wood smoke, suggesting that NOx promotes the formation of chromophores via secondary processes. Overall, the mass absorption cross section (integrated between 280 and 600 nm) of OC increased by 11-54% (except high RH) in the morning and then gradually decreased by 19-68% in the afternoon. This dynamic change in light absorption of wood-burning OC can be explained by two mechanisms: chromophore formation and sunlight bleaching. To investigate the effect of chemical transformation on light absorption, wood smoke particles were characterized using various spectrometers. The intensity of fluorescence, which is mainly related to polycyclic aromatic hydrocarbons (PAHs), rapidly decreased with time, indicating the potential bleaching of PAHs. A decline of levoglucosan concentrations evinced the change of primary organic aerosol with time. The aerosol water content measured by Fourier transform infrared spectroscopy showed that wood-burning aerosol became less hygroscopic as photooxidation proceeded. A similar trend in light absorption changes has been observed in ambient smoke aerosol originating from the 2012 County Line wildfire in Florida. We conclude that the biomass-burning OC becomes less light absorbing after 8-9 h sunlight exposure compared to fresh wood-burning OC.</description><subject>Aerosols</subject><subject>Carbon</subject><subject>Light absorption</subject><subject>Polycyclic aromatic hydrocarbons</subject><subject>Smoke</subject><subject>Spectrometers</subject><subject>Sunlight</subject><subject>Ultraviolet-visible spectroscopy</subject><subject>Wood</subject><issn>1680-7324</issn><issn>1680-7316</issn><issn>1680-7324</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2014</creationdate><recordtype>article</recordtype><sourceid>DOA</sourceid><recordid>eNqNks2L3SAUxUNpodNp910GumkXmWq8arIcph_zYKDQj7XcGM1zyNNUDfT99zXzSpkHXRQR5fI75-rlVNVrSq447eE96qWh0FBOZdMSCk-qCyo60kjWwtNH9-fVi5TuCWl5gS4q--Ho8eB0Pbtpn2scUohLdsHXwdaDCwdMqRnW6J2f6hAn9IXVGIdCLPuQg96bIsd5PtY4mbFe_Whi7TGvEec6rf7B-GX1zOKczKs_52X149PH7ze3zd2Xz7ub67tG8w5yg4zzfgAuNUfJZcctwsitHgSj7YDYd8KOXSvlSAnTIJCZVo4cx16iGcCyy2p38h0D3qslugPGowro1EOhfEBhzE7PRtHeWuzb0kK0wMTQjQiGaGIZQxCSFa-3J68lhp-rSVkdXNJmntGbsCZFOwFcCGjJf6AggEAPoqBvTuiE5RHO25Aj6g1X19BRoGX3hbr6B1XWuE07eGNdqZ8J3p0JCpPNrzzhmpLafft6zpITq2NIKRr7d1CUqC1MqoRJUVBbmNQWJvYb1LO8Cg</recordid><startdate>20140211</startdate><enddate>20140211</enddate><creator>Zhong, M</creator><creator>Jang, M</creator><general>Copernicus GmbH</general><general>Copernicus Publications</general><scope>AAYXX</scope><scope>CITATION</scope><scope>ISR</scope><scope>7QH</scope><scope>7TG</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope><scope>7U5</scope><scope>8FD</scope><scope>H8D</scope><scope>L7M</scope><scope>DOA</scope><orcidid>https://orcid.org/0000-0003-4211-7883</orcidid></search><sort><creationdate>20140211</creationdate><title>Dynamic light absorption of biomass-burning organic carbon photochemically aged under natural sunlight</title><author>Zhong, M ; Jang, M</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c584t-a3559b457c5a75785fa4d5fcb6312baa986fd8277d103c46a3e27d5ad97aeb4f3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2014</creationdate><topic>Aerosols</topic><topic>Carbon</topic><topic>Light absorption</topic><topic>Polycyclic aromatic hydrocarbons</topic><topic>Smoke</topic><topic>Spectrometers</topic><topic>Sunlight</topic><topic>Ultraviolet-visible spectroscopy</topic><topic>Wood</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Zhong, M</creatorcontrib><creatorcontrib>Jang, M</creatorcontrib><collection>CrossRef</collection><collection>Gale In Context: Science</collection><collection>Aqualine</collection><collection>Meteorological &amp; Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy &amp; Non-Living Resources</collection><collection>Meteorological &amp; Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) Professional</collection><collection>Solid State and Superconductivity Abstracts</collection><collection>Technology Research Database</collection><collection>Aerospace Database</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>Directory of Open Access Journals</collection><jtitle>Atmospheric chemistry and physics</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Zhong, M</au><au>Jang, M</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Dynamic light absorption of biomass-burning organic carbon photochemically aged under natural sunlight</atitle><jtitle>Atmospheric chemistry and physics</jtitle><date>2014-02-11</date><risdate>2014</risdate><volume>14</volume><issue>3</issue><spage>1517</spage><epage>1525</epage><pages>1517-1525</pages><issn>1680-7324</issn><issn>1680-7316</issn><eissn>1680-7324</eissn><abstract>Wood-burning aerosol produced under smoldering conditions was photochemically aged with different relative humidity (RH) and NOx conditions using a 104 m3 dual outdoor chamber under natural sunlight. Light absorption of organic carbon (OC) was measured over the course of photooxidation using a UV-visible spectrometer connected to an integrating sphere. At high RH, the color decayed rapidly. NOx slightly prolonged the color of wood smoke, suggesting that NOx promotes the formation of chromophores via secondary processes. Overall, the mass absorption cross section (integrated between 280 and 600 nm) of OC increased by 11-54% (except high RH) in the morning and then gradually decreased by 19-68% in the afternoon. This dynamic change in light absorption of wood-burning OC can be explained by two mechanisms: chromophore formation and sunlight bleaching. To investigate the effect of chemical transformation on light absorption, wood smoke particles were characterized using various spectrometers. The intensity of fluorescence, which is mainly related to polycyclic aromatic hydrocarbons (PAHs), rapidly decreased with time, indicating the potential bleaching of PAHs. A decline of levoglucosan concentrations evinced the change of primary organic aerosol with time. The aerosol water content measured by Fourier transform infrared spectroscopy showed that wood-burning aerosol became less hygroscopic as photooxidation proceeded. A similar trend in light absorption changes has been observed in ambient smoke aerosol originating from the 2012 County Line wildfire in Florida. We conclude that the biomass-burning OC becomes less light absorbing after 8-9 h sunlight exposure compared to fresh wood-burning OC.</abstract><pub>Copernicus GmbH</pub><doi>10.5194/acp-14-1517-2014</doi><tpages>9</tpages><orcidid>https://orcid.org/0000-0003-4211-7883</orcidid><oa>free_for_read</oa></addata></record>
fulltext fulltext
identifier ISSN: 1680-7324
ispartof Atmospheric chemistry and physics, 2014-02, Vol.14 (3), p.1517-1525
issn 1680-7324
1680-7316
1680-7324
language eng
recordid cdi_doaj_primary_oai_doaj_org_article_19ffa925fa62436b8da4e0c0f33a4673
source Publicly Available Content (ProQuest); Directory of Open Access Journals; Alma/SFX Local Collection
subjects Aerosols
Carbon
Light absorption
Polycyclic aromatic hydrocarbons
Smoke
Spectrometers
Sunlight
Ultraviolet-visible spectroscopy
Wood
title Dynamic light absorption of biomass-burning organic carbon photochemically aged under natural sunlight
url http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-21T14%3A56%3A26IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-gale_doaj_&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Dynamic%20light%20absorption%20of%20biomass-burning%20organic%20carbon%20photochemically%20aged%20under%20natural%20sunlight&rft.jtitle=Atmospheric%20chemistry%20and%20physics&rft.au=Zhong,%20M&rft.date=2014-02-11&rft.volume=14&rft.issue=3&rft.spage=1517&rft.epage=1525&rft.pages=1517-1525&rft.issn=1680-7324&rft.eissn=1680-7324&rft_id=info:doi/10.5194/acp-14-1517-2014&rft_dat=%3Cgale_doaj_%3EA481418149%3C/gale_doaj_%3E%3Cgrp_id%3Ecdi_FETCH-LOGICAL-c584t-a3559b457c5a75785fa4d5fcb6312baa986fd8277d103c46a3e27d5ad97aeb4f3%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_pqid=1846404946&rft_id=info:pmid/&rft_galeid=A481418149&rfr_iscdi=true