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

Result code in IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F70883521%3A28160%2F09%3A63508842" target="_blank" >RIV/70883521:28160/09:63508842 - isvavai.cz</a>

Result on the web

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DOI - Digital Object Identifier

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Result language

angličtina

Original language name

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

Original language description

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 destroyedduring 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.

Czech name

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Czech description

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Type

J_x - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)

CEP classification

DD - Geochemistry

OECD FORD branch

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Project

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Continuities

V - Vyzkumna aktivita podporovana z jinych verejnych zdroju

Publication year

2009

Confidentiality

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Name of the periodical

Science in China Series D: Earth Science

ISSN

1674-7313

e-ISSN

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Volume of the periodical

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Issue of the periodical within the volume

2

Country of publishing house

CN - CHINA

Number of pages

450

Pages from-to

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UT code for WoS article

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EID of the result in the Scopus database

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