EGU26-4948, updated on 13 Mar 2026
https://doi.org/10.5194/egusphere-egu26-4948
EGU General Assembly 2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Poster | Wednesday, 06 May, 10:45–12:30 (CEST), Display time Wednesday, 06 May, 08:30–12:30
 
Hall X2, X2.154
Spatial Structure of Surface Soil Magnetic Susceptibility Measured with MS2D across Multiple Soil Types in Poland and the Czech Republic
Piotr Fabijańczyk1, Jarosław Zawadzki1, Michał Bućko2, Hana Grison3, Michał Jankowski4, Tadeusz Magiera2, Eduard Petrovsky3, Vilém Podrázský5, Marcin Sykuła4, Marcin Szuszkiewicz2, and Zdeněk Vacek5
Piotr Fabijańczyk et al.
  • 1Warsaw University of Technology, Faculty Environmental of Engineering, Nowowiejska 20, 00-653 Warsaw, Poland
  • 2Institute of Environmental Engineering Polish Academy of Sciences, M. Skłodowskiej-Curie 34, 41-819 Zabrze, Poland
  • 3Institute of Geophysics of the Czech Academy of Sciences, Boční II 1401, 141 31 Praha, Czech Republic
  • 4Nicolaus Copernicus University in Toruń, Faculty of Earth Sciences and Spatial Management, Gagarina 11, 87-100 Toruń, Poland
  • 5Czech University of Life Sciences Prague, Kamýcká 129, 165 00 Praha, Czech Republic

This study examines the spatial variability of soil magnetic susceptibility measured on the soil surface across multiple sites in Poland and the Czech Republic. The investigated areas encompass a broad range of soil types, including Podzol, Gleysol enriched with iron ore, Rubic Arenosol, Ranker‑Cambisol, Cambisol, Luvisol, Brown acidic soil, and Podzolic brown soil. Surface magnetic susceptibility was measured with Bartington MS2D to capture both natural pedogenic patterns and potential anthropogenic magnetic enhancement. Spatial correlations were quantified using experimental variograms and their parameters to assess the scale and structure of spatial variability of soil magnetic susceptibility. Among these parameters, nugget effects varied substantially between soil types, indicating differences in micro-scale heterogeneity and surface disturbance.

The results demonstrate that surface magnetic susceptibility, combined with geostatistical analysis, is a sensitive indicator of both natural soil-forming processes and anthropogenic pollution.

How to cite: Fabijańczyk, P., Zawadzki, J., Bućko, M., Grison, H., Jankowski, M., Magiera, T., Petrovsky, E., Podrázský, V., Sykuła, M., Szuszkiewicz, M., and Vacek, Z.: Spatial Structure of Surface Soil Magnetic Susceptibility Measured with MS2D across Multiple Soil Types in Poland and the Czech Republic, EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-4948, https://doi.org/10.5194/egusphere-egu26-4948, 2026.