Glacial morphogenesis of uplands of the Warta Glaciation in Poland as a control on heavy metal distribution in deposits

The investigations were carried out to determine the relationship between Cr, Co, Cd, Cu, Zn and Pb content and glacial morphogenesis that implies the geomorphological position of outcrops of Quaternary deposits. The analysis deals with parts of two glacial uplands whose relief developed during degl...

Full description

Bibliographic Details
Main Author: Falkowska, Ewa
Format: Article in Journal/Newspaper
Language:English
Published: Polish Geological Institute-National Research Institute 2010
Subjects:
Online Access:https://gq.pgi.gov.pl/article/view/7520
id ftjgq:oai:geojournals.pgi.gov.pl:article/7520
record_format openpolar
spelling ftjgq:oai:geojournals.pgi.gov.pl:article/7520 2024-09-15T18:12:30+00:00 Glacial morphogenesis of uplands of the Warta Glaciation in Poland as a control on heavy metal distribution in deposits Falkowska, Ewa 2010-03-27 application/pdf https://gq.pgi.gov.pl/article/view/7520 eng eng Polish Geological Institute-National Research Institute https://gq.pgi.gov.pl/article/view/7520/6170 10.7306/gq.v53i3.7520.g6170 https://gq.pgi.gov.pl/article/view/7520 Geological Quarterly; Vol. 53 No. 3 (2009); 293-304 Geological Quarterly; Tom 53 Nr 3 (2009); 293-304 1641-7291 10.7306/gq.v53i3 morphogenesis areal deglaciation geomorphological units heavy metals info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2010 ftjgq https://doi.org/10.7306/gq.v53i3 2024-07-30T03:29:08Z The investigations were carried out to determine the relationship between Cr, Co, Cd, Cu, Zn and Pb content and glacial morphogenesis that implies the geomorphological position of outcrops of Quaternary deposits. The analysis deals with parts of two glacial uplands whose relief developed during deglaciation of the Warta ice sheet and which are characterized by similar relief and lithology of surface deposits. These are the Nidzica Upland near Grzebsk and the Bielsk Plain near Bielsk Podlaski. These areas show distinct regularity in pattern of geomorphological units, proving their areal deglaciation. Melt-out depressions, side valleys, ablation covers, kame terraces and kames as well as glaciofluvial plains are observed. The typical geomorphological element is isolated morainic hills (mesas). The investigations enabled determinations of regularity in the distribution of chemical elements in the soil environment of the geomorphological units. Among mineral sediments, clay interlayers observed within kame terrace and kame deposits were the most susceptible to concentrations of heavy metals, regardless of the region and the element to be determined. Lower Cd, Cu, Co, Pb, Zn and Cr contents were associated with morainic mesa and ablation cover deposits. The lowest contents of heavy minerals were measured in glaciofluvial plain, kame and kame terrace sands. Among landforms filled with organic deposits, the highest abilities to fix Cr, Co, Cu and Zn were shown by ice-dammed basins within upland deposits (Nidzica Upland) and side valley deposits (Bielsk Plain). Peats and muds of melt-out depressions were found to be most active in retaining Cd and Pb. Article in Journal/Newspaper Ice Sheet Geological Quarterly
institution Open Polar
collection Geological Quarterly
op_collection_id ftjgq
language English
topic morphogenesis
areal deglaciation
geomorphological units
heavy metals
spellingShingle morphogenesis
areal deglaciation
geomorphological units
heavy metals
Falkowska, Ewa
Glacial morphogenesis of uplands of the Warta Glaciation in Poland as a control on heavy metal distribution in deposits
topic_facet morphogenesis
areal deglaciation
geomorphological units
heavy metals
description The investigations were carried out to determine the relationship between Cr, Co, Cd, Cu, Zn and Pb content and glacial morphogenesis that implies the geomorphological position of outcrops of Quaternary deposits. The analysis deals with parts of two glacial uplands whose relief developed during deglaciation of the Warta ice sheet and which are characterized by similar relief and lithology of surface deposits. These are the Nidzica Upland near Grzebsk and the Bielsk Plain near Bielsk Podlaski. These areas show distinct regularity in pattern of geomorphological units, proving their areal deglaciation. Melt-out depressions, side valleys, ablation covers, kame terraces and kames as well as glaciofluvial plains are observed. The typical geomorphological element is isolated morainic hills (mesas). The investigations enabled determinations of regularity in the distribution of chemical elements in the soil environment of the geomorphological units. Among mineral sediments, clay interlayers observed within kame terrace and kame deposits were the most susceptible to concentrations of heavy metals, regardless of the region and the element to be determined. Lower Cd, Cu, Co, Pb, Zn and Cr contents were associated with morainic mesa and ablation cover deposits. The lowest contents of heavy minerals were measured in glaciofluvial plain, kame and kame terrace sands. Among landforms filled with organic deposits, the highest abilities to fix Cr, Co, Cu and Zn were shown by ice-dammed basins within upland deposits (Nidzica Upland) and side valley deposits (Bielsk Plain). Peats and muds of melt-out depressions were found to be most active in retaining Cd and Pb.
format Article in Journal/Newspaper
author Falkowska, Ewa
author_facet Falkowska, Ewa
author_sort Falkowska, Ewa
title Glacial morphogenesis of uplands of the Warta Glaciation in Poland as a control on heavy metal distribution in deposits
title_short Glacial morphogenesis of uplands of the Warta Glaciation in Poland as a control on heavy metal distribution in deposits
title_full Glacial morphogenesis of uplands of the Warta Glaciation in Poland as a control on heavy metal distribution in deposits
title_fullStr Glacial morphogenesis of uplands of the Warta Glaciation in Poland as a control on heavy metal distribution in deposits
title_full_unstemmed Glacial morphogenesis of uplands of the Warta Glaciation in Poland as a control on heavy metal distribution in deposits
title_sort glacial morphogenesis of uplands of the warta glaciation in poland as a control on heavy metal distribution in deposits
publisher Polish Geological Institute-National Research Institute
publishDate 2010
url https://gq.pgi.gov.pl/article/view/7520
genre Ice Sheet
genre_facet Ice Sheet
op_source Geological Quarterly; Vol. 53 No. 3 (2009); 293-304
Geological Quarterly; Tom 53 Nr 3 (2009); 293-304
1641-7291
10.7306/gq.v53i3
op_relation https://gq.pgi.gov.pl/article/view/7520/6170
10.7306/gq.v53i3.7520.g6170
https://gq.pgi.gov.pl/article/view/7520
op_doi https://doi.org/10.7306/gq.v53i3
_version_ 1810450092642009088