Magnetic iron oxides occurring in chernozem soil from Ukraine and Poland as indicators of pedogenic processes
作者： M Jeleńska , A Hasso-Agopsowicz , M Kądziałko-Hofmokl , A Sukhorada , K Bondar
DOI: 10.1007/S11200-008-0017-Z
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摘要: The paper concerns the complex study of pedogenic and magnetic characteristics unpolluted soil profiles from Ukraine (3 profiles, which two represent chernozem one kastanozem) Poland (1 profile chernozem), all with loess parent material. Two were situated further south than other two. “southern” zone is characterized by lower precipitation rate higher annual temperatures “northern” zone. Depth variations properties obtained various methods compared characteristics. common characteristic enhancement susceptibility in their upper parts related to presence superparamagnetic/ single-domain grains maghemite/oxidized magnetite origin. However, measured down depth differ between probably due differences climatic conditions and, perhaps, loess.
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