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<article language="en">
	<journal>
		<journal_title>The Cryosphere Discussions</journal_title>
		<journal_url>www.the-cryosphere-discuss.net</journal_url>
		<issn>1994-0432</issn>
		<eissn>1994-0440</eissn>
		<volume_number>4</volume_number>
		<issue_number>3</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/tcd-4-1243-2010</doi>
	<article_url>http://www.the-cryosphere-discuss.net/4/1243/2010/</article_url>
	<abstract_html>http://www.the-cryosphere-discuss.net/4/1243/2010/tcd-4-1243-2010.html</abstract_html>
	<fulltext_pdf>http://www.the-cryosphere-discuss.net/4/1243/2010/tcd-4-1243-2010.pdf</fulltext_pdf>
	<start_page>1243</start_page>
	<end_page>1276</end_page>
	<publication_date>2010-08-11</publication_date>
	<article_title content_type="html">An energy-conserving model of freezing variably-saturated soil</article_title>
	<authors>
		<author numeration="1" affiliations="1,4">
			<name>M. Dall&apos;Amico</name>
			<email>matteo@mountain-eering.com</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>S. Endrizzi</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>S. Gruber</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>R. Rigon</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Civil and Environmental Engineering, University of Trento, Trento, Italy</affiliation>
		<affiliation numeration="2" content_type="html">Environment Canada â€“ National Hydrology Research Centre, Saskatoon, Saskatchewan, Canada</affiliation>
		<affiliation numeration="3" content_type="html">Department of Geography, University of Zurich, Winterthurerstrasse 190 Zurich, Switzerland</affiliation>
		<affiliation numeration="4" content_type="html">now at: Mountain-eering srl, Via Siemens 19 Bolzano, Italy</affiliation>
	</affiliations>
	<abstract content_type="html">In this paper we provide a method for solving the energy equation in freezing soil. The
      solver is linked with the solution of Richards equation, and therefore able to approximate
      water movement near the liquid-solid phase transition. The equations show non-linear
      characteristics causing oscillatory behavior in the solution close to the phase transition,
      when normal methods of iterative integration, as Newton or Picard, are used. Thus,
      a globally convergent Newton method has been implemented to achieve convergence. The method
      is tested by comparison with an analytical solution to the Stefan problem and by comparison
      with experimental data derived from literature.</abstract>
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</article>

