Magnetic Susceptibility of Chernozems

Among other forms, iron contained in soil is a component of magnetic minerals, both primary and secondary ones, produced by various soil forming processes. The composition of the soil magnetic fraction, characterised by a magnetic susceptibility, is the consequence of its origin. The character of su...

Full description

Bibliographic Details
Main Authors: Hasso-Agopsowicz Agata, Jeleńska Maria, Wicik Bogumił
Format: Article
Language:English
Published: Sciendo 2004-12-01
Series:Miscellanea Geographica: Regional Studies on Development
Subjects:
Online Access:https://doi.org/10.2478/mgrsd-2004-0007
_version_ 1818585572810162176
author Hasso-Agopsowicz Agata
Jeleńska Maria
Wicik Bogumił
author_facet Hasso-Agopsowicz Agata
Jeleńska Maria
Wicik Bogumił
author_sort Hasso-Agopsowicz Agata
collection DOAJ
description Among other forms, iron contained in soil is a component of magnetic minerals, both primary and secondary ones, produced by various soil forming processes. The composition of the soil magnetic fraction, characterised by a magnetic susceptibility, is the consequence of its origin. The character of susceptibility changes along the analysed chernozems’ profiles indicates a similarity of the parent rock, as well as the pedogenic processes forming the chernozems from the territories of Poland and the Ukraine. The influence of anthropogenic factors could be seen in the increased susceptibility within the humus horizon of the degraded chernozem.
first_indexed 2024-12-16T08:39:12Z
format Article
id doaj.art-af022a1791764c14bb75757264c5d969
institution Directory Open Access Journal
issn 2084-6118
language English
last_indexed 2024-12-16T08:39:12Z
publishDate 2004-12-01
publisher Sciendo
record_format Article
series Miscellanea Geographica: Regional Studies on Development
spelling doaj.art-af022a1791764c14bb75757264c5d9692022-12-21T22:37:43ZengSciendoMiscellanea Geographica: Regional Studies on Development2084-61182004-12-01111576110.2478/mgrsd-2004-0007Magnetic Susceptibility of ChernozemsHasso-Agopsowicz AgataJeleńska MariaWicik BogumiłAmong other forms, iron contained in soil is a component of magnetic minerals, both primary and secondary ones, produced by various soil forming processes. The composition of the soil magnetic fraction, characterised by a magnetic susceptibility, is the consequence of its origin. The character of susceptibility changes along the analysed chernozems’ profiles indicates a similarity of the parent rock, as well as the pedogenic processes forming the chernozems from the territories of Poland and the Ukraine. The influence of anthropogenic factors could be seen in the increased susceptibility within the humus horizon of the degraded chernozem.https://doi.org/10.2478/mgrsd-2004-0007soil magnetismchernozems
spellingShingle Hasso-Agopsowicz Agata
Jeleńska Maria
Wicik Bogumił
Magnetic Susceptibility of Chernozems
Miscellanea Geographica: Regional Studies on Development
soil magnetism
chernozems
title Magnetic Susceptibility of Chernozems
title_full Magnetic Susceptibility of Chernozems
title_fullStr Magnetic Susceptibility of Chernozems
title_full_unstemmed Magnetic Susceptibility of Chernozems
title_short Magnetic Susceptibility of Chernozems
title_sort magnetic susceptibility of chernozems
topic soil magnetism
chernozems
url https://doi.org/10.2478/mgrsd-2004-0007
work_keys_str_mv AT hassoagopsowiczagata magneticsusceptibilityofchernozems
AT jelenskamaria magneticsusceptibilityofchernozems
AT wicikbogumił magneticsusceptibilityofchernozems