<?xml version="1.0" encoding="utf-8" standalone="no"?>
<!DOCTYPE article SYSTEM "http://www.atmos-chem-phys-discuss.net/inc/acpd/copernicus.dtd">
<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>5</volume_number>
		<issue_number>5</issue_number>
		<publication_year>2005</publication_year>
	</journal>
	<doi>10.5194/acpd-5-9801-2005</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/5/9801/2005/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/5/9801/2005/acpd-5-9801-2005.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/5/9801/2005/acpd-5-9801-2005.pdf</fulltext_pdf>
	<start_page>9801</start_page>
	<end_page>9860</end_page>
	<publication_date>2005-10-11</publication_date>
	<article_title content_type="html">Atmospheric HULIS: how humic-like are they? A comprehensive and critical review</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>E. R. Graber</name>
		</author>
		<author numeration="2" affiliations="2">
			<name>Y. Rudich</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Institute of Soil, Water and Environmental Sciences, The Volcani Center, Agricultural Research Organization, Bet Dagan, 50250, Israel</affiliation>
		<affiliation numeration="2" content_type="html">Department of Environmental Sciences and Energy Research, The Weizmann Institute of Science, Rehovot, 76100, Israel</affiliation>
	</affiliations>
	<abstract content_type="html">A class of organic molecules extracted from atmospheric aerosol particles and
isolated from fog and cloud water has been termed humic-like substances
(HULIS) due to certain resemblance to terrestrial and aquatic humic and
fulvic acids. In light of the interest that this class of atmospheric
compounds currently attracts, we comprehensively review HULIS properties, as
well as laboratory and field investigations concerning their formation and
characterization in atmospheric samples. While sharing some basic features,
accumulating evidence suggests that atmospheric HULIS differ substantially
from terrestrial and aquatic humic substances. Major differences between
HULIS and humic substances, including smaller average molecular weight, lower
aromatic moiety content and higher aliphatic moiety and polysaccharide
contents, as well as others, are highlighted. Several alternatives are
proposed that may explain such differences: (1) the possibility that mono-
and di-carboxylic acids and mineral acids abundant in the atmosphere prevent
the formation of large humic &apos;&apos;supramolecular associations&apos;&apos;; (2) that large
humic macromolecules are destroyed in the atmosphere by UV radiation, O&lt;sub&gt;3&lt;/sub&gt;, and
OH-radicals; (3) that &apos;&apos;HULIS&apos;&apos; actually consists of a complex, unresolved
mixture of relatively small molecules rather than macromolecular entities;
and (4) that HULIS formed via abiotic and short-lived oxidative reaction
pathways differs substantially from humic substances formed over long time
periods via biologically-mediated reactions. It is concluded that a
significant effort towards adopting standard extraction and characterization
methods is required to develop a better and more meaningful comparison between
different HULIS samples. The essential differences as denoted throughout,
point to the possibility that HULIS may not be nearly as humic-like as
hitherto believed.</abstract>
	<references>
	</references>
</article>

