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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>3</volume_number>
		<issue_number>5</issue_number>
		<publication_year>2003</publication_year>
	</journal>
	<doi>10.5194/acpd-3-5275-2003</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/3/5275/2003/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/3/5275/2003/acpd-3-5275-2003.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/3/5275/2003/acpd-3-5275-2003.pdf</fulltext_pdf>
	<start_page>5275</start_page>
	<end_page>5288</end_page>
	<publication_date>2003-10-20</publication_date>
	<article_title content_type="html">New insights in the global cycle of acetonitrile: release from the ocean and acetonitrile: release from the ocean and Venezuela</article_title>
	<authors>
		<author numeration="1" affiliations="1,2">
			<name>E. Sanhueza</name>
		</author>
		<author numeration="2" affiliations="1,3">
			<name>R. Holzinger</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>B. Kleiss</name>
		</author>
		<author numeration="4" affiliations="2">
			<name>L. Donoso</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>P. J. Crutzen</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">MPI für Chemie, Luftchemie, Postfach 3060, 55020 Mainz, Germany</affiliation>
		<affiliation numeration="2" content_type="html">IVIC, Atmospheric Chemistry Laboratory, Apartado 21827, Caracas 1020A, Venezuela</affiliation>
		<affiliation numeration="3" content_type="html">now at Univ. Calif. Berkeley, Div. Environm. Sci., Dept. Ecosyst. Sci. Policy &amp; Management, Berkeley, CA 94720, USA</affiliation>
	</affiliations>
	<abstract content_type="html">CUsing the proton transfer reaction mass spectrometry (PTR-MS) technique, acetonitrile was
      measured during the wet season in a Venezuelan woodland savanna. The site was located
      downwind of the Caribbean Sea and no biomass burning events were observed in the
      region. High boundary layer concentrations of&amp;nbsp; 211 &amp;plusmn;36 pmol/mol (median,
      &amp;plusmn; standard deviation) were observed during daytime in the well mixed boundary layer, which is about
      60 pmol/mol above background concentrations recently measured over the Mediterranean
      Sea and the Pacific Ocean. Most likely acetonitrile is released from the warm waters of the
      Caribbean Sea thereby enhancing mixing ratios over Venezuela. Acetonitrile concentrations
      will probably still be much higher in biomass burning plumes, however, the general
      suitability of acetonitrile as a biomass burning marker should be treated with care.&lt;br&gt;
      &lt;br&gt;
      During nights, acetonitrile dropped to levels typically around 120 pmol/mol, which is
      consistent with a dry deposition velocity of ~0.14 cm/s when a nocturnal boundary layer
      height of 100 m is assumed.</abstract>
	<references>
	</references>
</article>

