Magnetization of polar ice: a measurement of terrestrial dust and extraterrestrial fallout

Laboratory-induced remanent magnetization of polar ice constitutes a measurement of the magnetization carried by the ferromagnetic dust particles in the ice. This non-destructive technique provides a novel kind of information on the dust deposited on the surface of polar ice sheets. Measurements mad...

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Published in:Quaternary Science Reviews
Main Authors: LANCI, LUCA, B. Delmonte, D. V. Kent, V. Maggi, P. E. Biscaye, J. R. Petit
Other Authors: Lanci, Luca, B., Delmonte, D. V., Kent, V., Maggi, P. E., Biscaye, J. R., Petit
Format: Article in Journal/Newspaper
Language:English
Published: 2012
Subjects:
Online Access:http://hdl.handle.net/11576/2513530
https://doi.org/10.1016/j.quascirev.2011.11.023
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spelling ftunivurbino:oai:ora.uniurb.it:11576/2513530 2024-04-14T08:01:30+00:00 Magnetization of polar ice: a measurement of terrestrial dust and extraterrestrial fallout LANCI, LUCA B. Delmonte D. V. Kent V. Maggi P. E. Biscaye J. R. Petit Lanci, Luca B., Delmonte D. V., Kent V., Maggi P. E., Biscaye J. R., Petit 2012 STAMPA http://hdl.handle.net/11576/2513530 https://doi.org/10.1016/j.quascirev.2011.11.023 eng eng info:eu-repo/semantics/altIdentifier/wos/000300926700003 volume:33 firstpage:20 lastpage:31 numberofpages:12 journal:QUATERNARY SCIENCE REVIEWS http://hdl.handle.net/11576/2513530 doi:10.1016/j.quascirev.2011.11.023 info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-84856214017 info:eu-repo/semantics/article 2012 ftunivurbino https://doi.org/10.1016/j.quascirev.2011.11.023 2024-03-21T17:01:51Z Laboratory-induced remanent magnetization of polar ice constitutes a measurement of the magnetization carried by the ferromagnetic dust particles in the ice. This non-destructive technique provides a novel kind of information on the dust deposited on the surface of polar ice sheets. Measurements made on ice samples from Greenland (North GRIP ice core) and Antarctica (Vostok and EPICA-Dome C ice cores) allowed the recognition of a fraction of magnetic minerals in ice whose concentration and magnetic properties are directly related to that of insoluble dust. The source of this fraction of magnetic minerals thus appears closely related to terrestrial dust transport and deposition and its magnetic properties are informative of the dust provenance areas. The rock-magnetic properties of the dust may reflect distinct changes of dust source areas from glacial to interglacial periods in agreement with and adding further information to the isotopic (87Sr/86Sr and 143Nd/144Nd) analyses. A second magnetic fraction consists of particles of nanometric size, which are superparamagnetic at freezer temperature and whose concen- tration is independent of the mass of aerosol dust found in the ice. The source of these nanometric-sized magnetic particles is ascribed to fallout of “meteoric smoke” and their concentration in ice was found to be compatible with the extraterrestrial fallout inferred from Ir concentrations. The diameter of the smoke particles as inferred from magnetic measurements is in the range of about 7-20 nm. Article in Journal/Newspaper Antarc* Antarctica EPICA Greenland GRIP ice core Università degli Studi di Urbino: CINECA IRIS Greenland Quaternary Science Reviews 33 20 31
institution Open Polar
collection Università degli Studi di Urbino: CINECA IRIS
op_collection_id ftunivurbino
language English
description Laboratory-induced remanent magnetization of polar ice constitutes a measurement of the magnetization carried by the ferromagnetic dust particles in the ice. This non-destructive technique provides a novel kind of information on the dust deposited on the surface of polar ice sheets. Measurements made on ice samples from Greenland (North GRIP ice core) and Antarctica (Vostok and EPICA-Dome C ice cores) allowed the recognition of a fraction of magnetic minerals in ice whose concentration and magnetic properties are directly related to that of insoluble dust. The source of this fraction of magnetic minerals thus appears closely related to terrestrial dust transport and deposition and its magnetic properties are informative of the dust provenance areas. The rock-magnetic properties of the dust may reflect distinct changes of dust source areas from glacial to interglacial periods in agreement with and adding further information to the isotopic (87Sr/86Sr and 143Nd/144Nd) analyses. A second magnetic fraction consists of particles of nanometric size, which are superparamagnetic at freezer temperature and whose concen- tration is independent of the mass of aerosol dust found in the ice. The source of these nanometric-sized magnetic particles is ascribed to fallout of “meteoric smoke” and their concentration in ice was found to be compatible with the extraterrestrial fallout inferred from Ir concentrations. The diameter of the smoke particles as inferred from magnetic measurements is in the range of about 7-20 nm.
author2 Lanci, Luca
B., Delmonte
D. V., Kent
V., Maggi
P. E., Biscaye
J. R., Petit
format Article in Journal/Newspaper
author LANCI, LUCA
B. Delmonte
D. V. Kent
V. Maggi
P. E. Biscaye
J. R. Petit
spellingShingle LANCI, LUCA
B. Delmonte
D. V. Kent
V. Maggi
P. E. Biscaye
J. R. Petit
Magnetization of polar ice: a measurement of terrestrial dust and extraterrestrial fallout
author_facet LANCI, LUCA
B. Delmonte
D. V. Kent
V. Maggi
P. E. Biscaye
J. R. Petit
author_sort LANCI, LUCA
title Magnetization of polar ice: a measurement of terrestrial dust and extraterrestrial fallout
title_short Magnetization of polar ice: a measurement of terrestrial dust and extraterrestrial fallout
title_full Magnetization of polar ice: a measurement of terrestrial dust and extraterrestrial fallout
title_fullStr Magnetization of polar ice: a measurement of terrestrial dust and extraterrestrial fallout
title_full_unstemmed Magnetization of polar ice: a measurement of terrestrial dust and extraterrestrial fallout
title_sort magnetization of polar ice: a measurement of terrestrial dust and extraterrestrial fallout
publishDate 2012
url http://hdl.handle.net/11576/2513530
https://doi.org/10.1016/j.quascirev.2011.11.023
geographic Greenland
geographic_facet Greenland
genre Antarc*
Antarctica
EPICA
Greenland
GRIP
ice core
genre_facet Antarc*
Antarctica
EPICA
Greenland
GRIP
ice core
op_relation info:eu-repo/semantics/altIdentifier/wos/000300926700003
volume:33
firstpage:20
lastpage:31
numberofpages:12
journal:QUATERNARY SCIENCE REVIEWS
http://hdl.handle.net/11576/2513530
doi:10.1016/j.quascirev.2011.11.023
info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-84856214017
op_doi https://doi.org/10.1016/j.quascirev.2011.11.023
container_title Quaternary Science Reviews
container_volume 33
container_start_page 20
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