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<article language="en">
	<journal>
		<journal_title>Atmospheric Chemistry and Physics Discussions</journal_title>
		<journal_url>www.atmos-chem-phys-discuss.net</journal_url>
		<issn>1680-7367</issn>
		<eissn>1680-7375</eissn>
		<volume_number>9</volume_number>
		<issue_number>3</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/acpd-9-13739-2009</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/9/13739/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/9/13739/2009/acpd-9-13739-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/9/13739/2009/acpd-9-13739-2009.pdf</fulltext_pdf>
	<start_page>13739</start_page>
	<end_page>13773</end_page>
	<publication_date>2009-06-22</publication_date>
	<article_title content_type="html">Positive sampling artifact of carbonaceous aerosols and its influence on the thermal-optical split of OC/EC</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>Y. Cheng</name>
			<email>chengyuan02@gmail.com</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>K. B. He</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>F. K. Duan</name>
		</author>
		<author numeration="4" affiliations="2">
			<name>M. Zheng</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>Y. L. Ma</name>
		</author>
		<author numeration="6" affiliations="1">
			<name>J. H. Tan</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Environmental Science and Engineering, Tsinghua University, China</affiliation>
		<affiliation numeration="2" content_type="html">School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, GA, USA</affiliation>
	</affiliations>
	<abstract content_type="html">Accurate measurement of carbonaceous aerosols is challenging, due to
      the sampling artifact and the problems of the split of OC/EC. Two
      approaches have been used to account for the positive artifact: backup
      quartz approach in which a backup quartz filter is placed either
      behind a front quartz filter (QBQ) or in a parallel port behind
      a Teflon filter (QBT), and organic denuder approach in which an
      organic denuder is placed upstream of the quartz filter. Both
      approaches were evaluated in Beijing, China, from January to February
      2009. 10% of the OC captured by the bare quartz filter was from the
      positive artifact. The origin of backup OC was quantitatively
      evaluated by the denuder-based method. All of the QBQ-OC was from
      gaseous organics passing through the front filter, but the QBQ had not
      reached equilibrium with gas phase due to the relative small sampling
      volume resulting in an undercorrection of the positive artifact by
      3.7%. QBT-OC was from both gaseous organics passing through the
      front filter (82%) and the evaporated organic carbon (18%), thus
      overcorrecting the positive artifact by 6.3%. Even the positive
      artifact-contributed QBT-OC was found to overestimate the positive
      artifact, perhaps due to the difference in the adsorption properties
      of the loaded filter and the filter without particle
      loading. Re-partitioning of PC and EC was performed by the multiple
      linear regression approach. The attenuation coefficient of PC was
      twofold higher than that of EC, indicating PC was darker than EC,
      resulting in the underestimation of native EC by TOT-split-EC. It was
      also found that PC formed on the bare quartz filter
      (45.56 m&lt;sup&gt;2&lt;/sup&gt;/g) was darker than that formed on the denuded
      filter (38.64 m&lt;sup&gt;2&lt;/sup&gt;/g), indicating that the underestimation
      for the bare quartz filter was more significant.</abstract>
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