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<article language="en">
	<journal>
		<journal_title>Hydrology and Earth System Sciences</journal_title>
		<journal_url>www.hydrol-earth-syst-sci.net</journal_url>
		<issn>1027-5606</issn>
		<eissn>1607-7938</eissn>
		<volume_number>10</volume_number>
		<issue_number>6</issue_number>
		<publication_year>2006</publication_year>
	</journal>
	<doi>10.5194/hess-10-817-2006</doi>
	<article_url>http://www.hydrol-earth-syst-sci.net/10/817/2006/</article_url>
	<abstract_html>http://www.hydrol-earth-syst-sci.net/10/817/2006/hess-10-817-2006.html</abstract_html>
	<fulltext_pdf>http://www.hydrol-earth-syst-sci.net/10/817/2006/hess-10-817-2006.pdf</fulltext_pdf>
	<start_page>817</start_page>
	<end_page>827</end_page>
	<publication_date>2006-11-09</publication_date>
	<article_title content_type="html">Novel evaporation experiment to determine soil hydraulic properties</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>K. Schneider</name>
			<email>klaus.schneider@iup.uni-heidelberg.de</email>
		</author>
		<author numeration="2" affiliations="2,3">
			<name>O. Ippisch</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>K. Roth</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Institute of Environmental Physics, University of Heidelberg, Heidelberg, Germany</affiliation>
		<affiliation numeration="2" content_type="html">Institute of Parallel and Distributed Systems, University of Stuttgart, Stuttgart,  Germany</affiliation>
		<affiliation numeration="3" content_type="html">formerly: Interdisciplinary Center for Scientific Computing, University of  Heidelberg, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">A novel experimental approach to determine soil hydraulic material properties
for the dry and very dry range is presented.
Evaporation from the surface of a soil column is controlled by a constant flux of preconditioned air and the
resulting vapour flux is measured by infrared absorption spectroscopy. The data
are inverted under the assumptions that (i)&amp;nbsp;the simultaneous movement of water
in the liquid and vapour is represented by Richards&apos; equation with an effective
hydraulic conductivity and that (ii)&amp;nbsp;the coupling between the soil and the
well-mixed atmosphere can be modelled by a boundary layer with a constant
transfer resistance. The optimised model fits the data exceptionally well.
Remaining deviations during the initial phase of an experiment are thought to be
well-understood and are attributed to the onset of the heat flow through the
column which compensates the latent heat of evaporation.</abstract>
	<references>
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</article>

