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Two pedogenic models for paleoclimatic records of magnetic susceptibility from Chinese and Siberian loess

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dc.title Two pedogenic models for paleoclimatic records of magnetic susceptibility from Chinese and Siberian loess en
dc.contributor.author Liu, X. M.
dc.contributor.author Liu, T. S.
dc.contributor.author Hesse, P.
dc.contributor.author Xia, D. S.
dc.contributor.author Chlachula, Jiří
dc.relation.ispartof Science in China Series D: Earth Science
dc.identifier.issn 1674-7313 Scopus Sources, Sherpa/RoMEO, JCR
dc.date.issued 2008
utb.relation.volume 51
utb.relation.issue 2
dc.citation.spage 284
dc.citation.epage 293
dc.type article
dc.language.iso en
dc.publisher Science China Press Ltd. Co. en
dc.identifier.doi 10.1007/s11430-007-0145-2
dc.relation.uri http://www.springerlink.com/content/r8304620j3082674/
dc.subject Siberian loess en
dc.subject Chinese loess en
dc.subject climate change en
dc.subject magnetic mineralogy en
dc.description.abstract Magnetic susceptibility has been used as a vital tool for reconstruction of the past climate change and understanding present environments. The in-situ enhancement of ferromagnetic content is believed to be the main reason for increase of MS in soil units. The present study of Siberian samples suggests that the notable differences in magnetic properties of the Siberian loess and paleosols reflect variations of grain size as well as mineralogy of the parent material. Ferrimagnetic minerals are destroyed during wet and warm periods resulting in MS reduction opposite to MS increase in the Chinese loess due to different climatic conditions and monsoonal atmospheric circulations. en
utb.faculty Faculty of Logistics and Crisis Management
dc.identifier.uri http://hdl.handle.net/10563/1001623
utb.identifier.rivid RIV/70883521:28160/09:63508842!RIV10-MSM-28160___
utb.identifier.obdid 43861830
utb.identifier.scopus 2-s2.0-38549170447
utb.identifier.wok 000252470400013
utb.source j-riv
utb.contributor.internalauthor Chlachula, Jiří
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