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<article language="en">
	<journal>
		<journal_title>Drinking Water Engineering and Science Discussions</journal_title>
		<journal_url>www.drink-water-eng-sci-discuss.net</journal_url>
		<issn>1996-9473</issn>
		<eissn>1996-9481</eissn>
		<volume_number>3</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/dwesd-3-107-2010</doi>
	<article_url>http://www.drink-water-eng-sci-discuss.net/3/107/2010/</article_url>
	<abstract_html>http://www.drink-water-eng-sci-discuss.net/3/107/2010/dwesd-3-107-2010.html</abstract_html>
	<fulltext_pdf>http://www.drink-water-eng-sci-discuss.net/3/107/2010/dwesd-3-107-2010.pdf</fulltext_pdf>
	<start_page>107</start_page>
	<end_page>132</end_page>
	<publication_date>2010-02-01</publication_date>
	<article_title content_type="html">Effects of ozonation and temperature on biodegradation of natural organic matter in biological granular activated carbon filters</article_title>
	<authors>
		<author numeration="1" affiliations="1,2">
			<name>L. T. J. van der Aa</name>
		</author>
		<author numeration="2" affiliations="2">
			<name>L. C. Rietveld</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>J. C. van Dijk</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Waternet, P.O. Box 94370, 1090 GJ Amsterdam, The Netherlands</affiliation>
		<affiliation numeration="2" content_type="html">Delft University of Technology, P.O. Box 5048, 2600 GA Delft, The Netherlands</affiliation>
	</affiliations>
	<abstract content_type="html">Four pilot (biological) granular activated carbon ((B)GAC) filters were
operated to quantify the effects of ozonation and water temperature on the
biodegradation of natural organic matter (NOM) in (B)GAC filters. Removal of
dissolved organic carbon (DOC), assimilable organic carbon (AOC) and oxygen
and the production of carbon dioxide were taken as indicators for NOM
biodegradation. Ozonation stimulated DOC and AOC removal in the BGAC
filters, but had no significant effect on oxygen removal and carbon dioxide
production. The temperature had no significant effect on DOC and AOC
removal, while oxygen removal and carbon dioxide production increased with
increasing temperature. Multivariate linear regression was used to quantify
these relations. In summer the ratio between oxygen consumption and DOC
removal exceeded the theoretical maximum of 2.5 g O&lt;sub&gt;2&lt;/sub&gt;&amp;middot;g C&lt;sup&gt;&amp;minus;1&lt;/sup&gt;
and the ratio between carbon dioxide production and DOC removal exceeded the
theoretical maximum of 3.7 g CO&lt;sub&gt;2&lt;/sub&gt;&amp;middot;g C&lt;sup&gt;&amp;minus;1&lt;/sup&gt;. Bioregeneration of
large NOM molecules could explain this excesses and the non-correlation
between DOC and AOC removal and oxygen removal and carbon dioxide
production. However bioregeneration of large NOM molecules was considered
not likely to happen, due to sequestration.</abstract>
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</article>

