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	<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>5</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/acpd-9-19683-2009</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/9/19683/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/9/19683/2009/acpd-9-19683-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/9/19683/2009/acpd-9-19683-2009.pdf</fulltext_pdf>
	<start_page>19683</start_page>
	<end_page>19712</end_page>
	<publication_date>2009-09-23</publication_date>
	<article_title content_type="html">Acetaldehyde in the Alaskan subarctic snow pack</article_title>
	<authors>
		<author numeration="1" affiliations="1,2">
			<name>F. Domine</name>
			<email>florent@lgge.obs.ujf-grenoble.fr</email>
		</author>
		<author numeration="2" affiliations="1,2">
			<name>S. Houdier</name>
		</author>
		<author numeration="3" affiliations="1,2">
			<name>A.-S. Taillandier</name>
		</author>
		<author numeration="4" affiliations="3,4">
			<name>W. R. Simpson</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">CNRS-INSU, Laboratoire de Glaciologie et Géophysique de l&apos;Environnement, BP 96, 38402 Saint-Martin d&apos;Hères Cedex, France</affiliation>
		<affiliation numeration="2" content_type="html">Université Joseph Fourier – Grenoble I, France</affiliation>
		<affiliation numeration="3" content_type="html">Geophysical Institute, University of Alaska Fairbanks, Alaska, USA</affiliation>
		<affiliation numeration="4" content_type="html">Department of Chemistry, University of Alaska Fairbanks, USA</affiliation>
	</affiliations>
	<abstract content_type="html">Acetaldehyde is a reactive intermediate in hydrocarbon oxidation. It is both emitted and
      taken up by snowpacks and photochemical and physical processes are probably
      involved. Understanding the reactivity of acetaldehyde in snow and its processes of physical
      and chemical exchanges requires the knowledge of its incorporation mechanism in snow
      crystals. We have performed a season-long study of the evolution of acetaldehyde
      concentrations in the subarctic snowpack near Fairbanks (65&amp;deg; N), central Alaska,
      which is subjected to a vigorous metamorphism due to persistent elevated temperature
      gradients in the snowpack, between 20 and 200&amp;deg;C m&lt;sup&gt;&amp;minus;1&lt;/sup&gt;. The snowpack
      therefore almost entirely transforms into depth hoar. We have also analyzed acetaldehyde in
      a manipulated snowpack where temperature gradients were suppressed. Snow crystals there
      transformed much more slowly and their original shapes remained recognizable for months. The
      specific surface area of snow layers in both types of snowpacks was also measured. We deduce
      that acetaldehyde is not adsorbed onto the surface of snow crystals and that most of the
      acetaldehyde is probably not dissolved in the ice lattice of the snow crystals. We propose
      that most of the acetaldehyde measured is either trapped or dissolved within organic
      aerosol particles trapped in snow, or that acetaldehyde is formed by the hydrolysis of
      organic precursors contained in organic aerosols trapped in the snow, when the snow is
      melted for analysis. These precursors are probably aldehyde polymers formed within the
      aerosol particles by acid catalysis, but might also be biological molecules. In a laboratory
      experiment, acetaldehyde-di-n-hexyl acetal, representing a potential acetaldehyde precursor,
      was subjected to our analytical procedure and reacted to form acetaldehyde. This confirms
      our suggestion that acetaldehyde in snow could be produced during the melting of snow for
      analysis.</abstract>
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