Please use this identifier to cite or link to this item:
https://open.uns.ac.rs/handle/123456789/9281
DC Field | Value | Language |
---|---|---|
dc.contributor.author | Liu X. | en_US |
dc.contributor.author | Liu Z. | en_US |
dc.contributor.author | Lü B. | en_US |
dc.contributor.author | Marković, Slobodan | en_US |
dc.contributor.author | Chen J. | en_US |
dc.contributor.author | Guo H. | en_US |
dc.contributor.author | Ma M. | en_US |
dc.contributor.author | Zhao G. | en_US |
dc.contributor.author | Feng H. | en_US |
dc.date.accessioned | 2019-09-30T09:14:49Z | - |
dc.date.available | 2019-09-30T09:14:49Z | - |
dc.date.issued | 2013-01-01 | - |
dc.identifier.issn | 10016538 | en_US |
dc.identifier.uri | https://open.uns.ac.rs/handle/123456789/9281 | - |
dc.description.abstract | This paper reports a loess-paleosol sequence located in the Danube River basin, Serbia, which formed at least since the latest part of the early Pleistocene, and before the paleomagnetic B/M boundary. Various magnetic parameters of the Serbian V-L1-V-S4 loess-paleosol sequence have been measured and analyzed in the Titel Loess Plateau. These parameters show a very similar magnetic behavior compared with that of the Chinese loess. There is a general positive relationship between magnetic susceptibility (χ) and pedogenesis. The main contributors to χ are the magnetic grains of SP (superparamagnetic) and SD (single domain) magnetic domains, while MD (multi domain) contributes only a small percentage. The difference in χ between loess and paleosol mainly is caused by pedogenesis. The very fine magnetic minerals increase gradually with increasing soil development (from loess to soil), and they lead to higher χ. The thermomagnetic curves show thatmagnetic minerals in the loess layers are magnetite and maghemite, both providing a major contribution to χ. In contrast the paleosol layers mainly are composed of magnetite, with almost no or a very small amount of maghemite, as implied by a reversible thermomagnetic behavior. This indicates that pedogenic conditions during V-S3 and V-S4 strong soil development have resulted in maghemite that is no longer stable, and has been resolved or converted to other stable phase minerals. This likely indicates that soil moisture during V-S3 and V-S4 development exceeded a critical condition of maghemite stability. © 2012 The Author(s). | en |
dc.relation.ispartof | Chinese Science Bulletin | en |
dc.title | The magnetic properties of Serbian loess and its environmental significance | en_US |
dc.type | Journal/Magazine Article | en_US |
dc.identifier.doi | 10.1007/s11434-012-5383-9 | - |
dc.identifier.scopus | 2-s2.0-84872760230 | - |
dc.identifier.url | https://api.elsevier.com/content/abstract/scopus_id/84872760230 | - |
dc.description.version | Unknown | en_US |
dc.relation.lastpage | 363 | en |
dc.relation.firstpage | 353 | en |
dc.relation.issue | 3 | en |
dc.relation.volume | 58 | en |
item.grantfulltext | none | - |
item.fulltext | No Fulltext | - |
crisitem.author.dept | Prirodno-matematički fakultet, Departman za geografiju, turizam i hotelijerstvo | - |
crisitem.author.orcid | 0000-0002-4977-634X | - |
crisitem.author.parentorg | Prirodno-matematički fakultet | - |
Appears in Collections: | PMF Publikacije/Publications |
SCOPUSTM
Citations
32
checked on May 10, 2024
Page view(s)
14
Last Week
9
9
Last month
0
0
checked on May 3, 2024
Google ScholarTM
Check
Altmetric
Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.