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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-4-1449-2010</doi>
	<article_url>http://www.the-cryosphere-discuss.net/4/1449/2010/</article_url>
	<abstract_html>http://www.the-cryosphere-discuss.net/4/1449/2010/tcd-4-1449-2010.html</abstract_html>
	<fulltext_pdf>http://www.the-cryosphere-discuss.net/4/1449/2010/tcd-4-1449-2010.pdf</fulltext_pdf>
	<start_page>1449</start_page>
	<end_page>1465</end_page>
	<publication_date>2010-08-26</publication_date>
	<article_title content_type="html">Isotope hydrological studies on the perennial ice deposit of Saarhalle, Mammuthöhle, Dachstein Mts, Austria</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>Z. Kern</name>
			<email>kern@geochem.hu</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>I. Fórizs</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>M. Molnár</name>
		</author>
		<author numeration="4" affiliations="3">
			<name>B. Nagy</name>
		</author>
		<author numeration="5" affiliations="4">
			<name>R. Pavuza</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Institute for Geochemical Research, Hungarian Academy of Sciences, Budapest, Hungary</affiliation>
		<affiliation numeration="2" content_type="html">Institute of Nuclear Research of the Hungarian Academy of Sciences, Debrecen, Hungary</affiliation>
		<affiliation numeration="3" content_type="html">Department of Physical Geography, Eötvös Loránd University, Budapest, Hungary</affiliation>
		<affiliation numeration="4" content_type="html">Department of Karst and Cave Science at the Museum of Natural History, Vienna, Austria</affiliation>
	</affiliations>
	<abstract content_type="html">A 5.28 m long ice core was extracted from the major cave ice block of the
Mammuthöhle cave system. Tritium concentration in eight samples from the
upper 1.2 m of the core was measured. Electrical conductivity measurements
were achieved on molten water samples and stable oxygen and hydrogen
isotopic compositions were also analysed. The upper ~1.2 m of ice has
been deposited from precipitation fallen before the 1960s (based on tritium
&amp;lt; 8.5 TU). The Saarhalle ice block is build from atmospheric precipitation
and the water perfectly preserved the isotopic composition; however the mean
&lt;sup&gt;18&lt;/sup&gt;O/&lt;sup&gt;16&lt;/sup&gt;O ratio of the ice is less depleted compared to the
long-term (1973–1983) &lt;sup&gt;18&lt;/sup&gt;O/&lt;sup&gt;16&lt;/sup&gt;O ratio of precipitation at Feuerkogel
the nearest (~32 km) reference station situated in the same elevation
like Mammuthöhle cave. Characteristic fluctuation was observed in the
conductivity along the studied cave ice profile. The conductivity
oscillations seem to mirror the changing partition of karstic water and
surface meltwater in the water supply of the ice accumulation. The ice
layers with low conductivity seem to archive past events when more
meltwater-like water have been drained and frozen onto the ice block.</abstract>
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</article>

