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<article language="en">
	<journal>
		<journal_title>Hydrology and Earth System Sciences Discussions</journal_title>
		<journal_url>www.hydrol-earth-syst-sci-discuss.net</journal_url>
		<issn>1812-2108</issn>
		<eissn>1812-2116</eissn>
		<volume_number>5</volume_number>
		<issue_number>4</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/hessd-5-2409-2008</doi>
	<article_url>http://www.hydrol-earth-syst-sci-discuss.net/5/2409/2008/</article_url>
	<abstract_html>http://www.hydrol-earth-syst-sci-discuss.net/5/2409/2008/hessd-5-2409-2008.html</abstract_html>
	<fulltext_pdf>http://www.hydrol-earth-syst-sci-discuss.net/5/2409/2008/hessd-5-2409-2008.pdf</fulltext_pdf>
	<start_page>2409</start_page>
	<end_page>2423</end_page>
	<publication_date>2008-08-28</publication_date>
	<article_title content_type="html">Thermal conductivity of unsaturated clay-rocks</article_title>
	<authors>
		<author numeration="1" affiliations="1,2,3">
			<name>D. Jougnot</name>
		</author>
		<author numeration="2" affiliations="1,3">
			<name>A. Revil</name>
			<email>arevil@mines.edu</email>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Colorado School of Mines, Green Center, Department of Geophysics, Golden, CO, USA</affiliation>
		<affiliation numeration="2" content_type="html">ANDRA, Chatenay-Malabry, France</affiliation>
		<affiliation numeration="3" content_type="html">CNRS-LGIT (UMR 5559), University of Savoie, Equipe Volcan, Le Bourget-du-Lac, France</affiliation>
	</affiliations>
	<abstract content_type="html">The thermal conductivity of porous materials can be related to the
electrical conductivity and therefore electrical resistivity tomography can
be used to map the thermal conductivity of porous rocks. In this paper, a
relationship is developed to connect the thermal conductivity of unsaturated
clay-rocks to the thermal conductivity of the different phases of the porous
composite, a textural parameter called the thermal formation factor, and the
tortuosity of the water phase. The thermal formation factor is related to
the electrical formation factor and to the first Archie&apos;s first exponent m.
The tortuosity of the water phase is related to the second Archie&apos;s exponent
n and to the relative saturation of the water phase. A very good agreement
is obtained between the new model and thermal conductivity measurements of
packs of glass beads and cores of the Callovo-Oxfordian argillite at
different saturations of the water phase. Anisotropy of the effective
thermal conductivity is mainly due to the anisotropy of the thermal
conductivity of the solid phase.</abstract>
	<references>
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</article>
