Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
8907821 | Polar Science | 2018 | 37 Pages |
Abstract
Heavy-metal contamination near the PPS originates primarily from local sources. Anthropogenic spherical, magnetite-like particles were found near the station, whereas uncontaminated topsoil is devoid of such particles. Magnetic studies indicate that magnetite and goethite are the primary magnetic phases, with magnetite levels being higher in polluted area. Magnetic fraction of contaminated topsoil includes a mixture of single-domain and multi-domain grains, while uncontaminated topsoil contains smaller grains. Results show a clear correspondence between Pollution Load Index and magnetic susceptibility anomalies, and that the areal extent of PPS impact on the environment has not expanded significantly since 2004 (although a new contamination source, the scrap yard, is now present). A comparison of magnetic susceptibility measurements with metal analyses indicates that magnetic methods can be used as a rapid, inexpensive, non-invasive, and sensitive tool for the evaluation of topsoil contamination.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth and Planetary Sciences (General)
Authors
T. Gonet, B. Górka-Kostrubiec, B. Åuczak-Wilamowska,