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Identification of Remnants of World War Ii Air Campaign for Spatial Management Using Geophysical Methods (KoźLe Basin, Southern Poland) Cover

Identification of Remnants of World War Ii Air Campaign for Spatial Management Using Geophysical Methods (KoźLe Basin, Southern Poland)

Open Access
|Dec 2025

Figures & Tables

Fig. 1.

Bomb fragments collected from construction site excavations. Exhibits owned by the “Blechhammer 1944” Museum of the Silesian Battle for Fuel in Kędzierzyn-Koźle. (photo: J.M. Waga).
Bomb fragments collected from construction site excavations. Exhibits owned by the “Blechhammer 1944” Museum of the Silesian Battle for Fuel in Kędzierzyn-Koźle. (photo: J.M. Waga).

Fig. 2.

A – Location of the study area; B – Synthetic geological cross-section of the study area: a – experimental areas, b – pre-Vistulian sands and gravels, c – massive silts and clays, d – glacial tills with erratic boulders, e – Vistulian sands and gravels, locally organic silts and peats in valleys, f – boulder horizon, locally with erratic boulders, g – “black oaks”, h – water table, i – zones prone to UXB risks.
A – Location of the study area; B – Synthetic geological cross-section of the study area: a – experimental areas, b – pre-Vistulian sands and gravels, c – massive silts and clays, d – glacial tills with erratic boulders, e – Vistulian sands and gravels, locally organic silts and peats in valleys, f – boulder horizon, locally with erratic boulders, g – “black oaks”, h – water table, i – zones prone to UXB risks.

Fig. 3.

A – Glacitectonically disturbed series of marginal sediments with massive silts at experimental area 1; B – Erratic boulder resting on silt, removed from a shallow excavation in experimental area 3 (photo: J.M. Waga).
A – Glacitectonically disturbed series of marginal sediments with massive silts at experimental area 1; B – Erratic boulder resting on silt, removed from a shallow excavation in experimental area 3 (photo: J.M. Waga).

Fig. 4.

A – Ground scanning with a proton magnetometer in the vicinity of a flooded UXB intake crater (in the foreground); B – Ground scanning with a Geonics EM31-MK2 conductivity meter; C – Ground profiling in difficult forest terrain using the Mala RAMAC X3M GPR (photo: J.M. Waga).
A – Ground scanning with a proton magnetometer in the vicinity of a flooded UXB intake crater (in the foreground); B – Ground scanning with a Geonics EM31-MK2 conductivity meter; C – Ground profiling in difficult forest terrain using the Mala RAMAC X3M GPR (photo: J.M. Waga).

Fig. 5.

Electrical resistivity tomography using ABEM’s LUND Imaging System (photo: J.M. Waga).
Electrical resistivity tomography using ABEM’s LUND Imaging System (photo: J.M. Waga).

Fig. 6.

Characteristics of methods used to locate UXBs (in SWOT terms).
Characteristics of methods used to locate UXBs (in SWOT terms).

Fig. 7.

Examples of surface finds identified using the proton magnetometer: A – tail base plug of 500 lb bomb with tail fuse fragments and a peg made of steel pipe lying on the concrete base of a 75mm Flak 97 gun that was part of Schwere Heimat-Flak-Batterie 212/VIII Alt Cosel; next to those, an orange stake marking a future development project (photo: J.M. Waga); B – fragments of bombs, of a power line and possibly of a B-24 plane (photo: B. Szypuła); C – Rock fragment with ferromagnetic properties (photo: J.M. Waga).
Examples of surface finds identified using the proton magnetometer: A – tail base plug of 500 lb bomb with tail fuse fragments and a peg made of steel pipe lying on the concrete base of a 75mm Flak 97 gun that was part of Schwere Heimat-Flak-Batterie 212/VIII Alt Cosel; next to those, an orange stake marking a future development project (photo: J.M. Waga); B – fragments of bombs, of a power line and possibly of a B-24 plane (photo: B. Szypuła); C – Rock fragment with ferromagnetic properties (photo: J.M. Waga).

Fig. 8.

Conductivity profiles from measurements performed using the Geonics EM31-MK2 instrument. Serie 1 – apparent conductivity, Series 2 – magnetic component – in-phase. Anomalies indicating: A – the presence of a steel pipe from a former water pipeline; B – presence of shrapnels in a buried crater after a detonated bomb; C – the potential presence of UXB; D – likely drift channel trace (anomaly indicated by a red arrow) located between the UXB inlet crater and its location.
Conductivity profiles from measurements performed using the Geonics EM31-MK2 instrument. Serie 1 – apparent conductivity, Series 2 – magnetic component – in-phase. Anomalies indicating: A – the presence of a steel pipe from a former water pipeline; B – presence of shrapnels in a buried crater after a detonated bomb; C – the potential presence of UXB; D – likely drift channel trace (anomaly indicated by a red arrow) located between the UXB inlet crater and its location.

Fig. 9.

Layered map generated from CMD-Explorer conductivity meter readings with a potential UXB identified (location marked with a square).
Layered map generated from CMD-Explorer conductivity meter readings with a potential UXB identified (location marked with a square).

Fig. 10.

GPR profiling in a forest area: 1 – UXB fall site remodeled by later earthworks, 2 – subsurface object zones, 11–20 – profile lines.
GPR profiling in a forest area: 1 – UXB fall site remodeled by later earthworks, 2 – subsurface object zones, 11–20 – profile lines.

Fig. 11.

Experimental area 3: A – diagram presenting electrical resistivity tomography results obtained in a wetland; B – profiles lines ECM1, GPR, ER and two concentrations of PM signal occurrence (red circles). Large yellow circles – probable remnants of the UXB fall. The profile described as ECM1 is shown in Fig. 8B.
Experimental area 3: A – diagram presenting electrical resistivity tomography results obtained in a wetland; B – profiles lines ECM1, GPR, ER and two concentrations of PM signal occurrence (red circles). Large yellow circles – probable remnants of the UXB fall. The profile described as ECM1 is shown in Fig. 8B.

Fig. 12.

Authors in the vicinity of a crater formed as a result of a spontaneous UXB explosion in late 2021/early 2022 (photo: J.M. Waga).
Authors in the vicinity of a crater formed as a result of a spontaneous UXB explosion in late 2021/early 2022 (photo: J.M. Waga).

Methods and equipment used in the study_

Abbrev.TechnologyDeviceManufacturerDepth (m)
MADMagnetic anomaly detectionPioneer VLFBounty Hunter0–0.65
PMProton magnetometryMaggie magnetometerSchonstedt0–5.5
ECM1Electromagnetic conductivityEM31-MK2 meterGeonics0–6.0
ECM2Electromagnetic conductivityCMD Explorer meterGF Instruments0–6.7
GPRGround penetration radarPro Ex RAMAC X3MMALÅ0–4.8 or 0–11.5 (recording range 97.94 or 229.62 ns depending on the antenna used)
ERElectrical resistivityABEM Terrameter SAS 4000 with ABEM LUND Imaging SystemABEM Instrument0–7.2 or 0–14.4 (recording range depending on the electrode spacing: 1 or 2 m)

Areas and lengths of the profiles investigated by different geophysical methods_

Experimental areasMAD [m2]PM [m2]ECM1 [m2 or *m]ECM2 [m2]GPR [m]ER [m]
1a38003800600800
2a1000010000400112080
3a3150315024029040
3b22502250370
3c1200012000*40370
3d43004300960
4a15001500*52
4b18001800*74
4c30503050*69
4d950950*65
4e22002200
Total45000450002200 + *3008002150120
DOI: https://doi.org/10.14746/quageo-2026-0004 | Journal eISSN: 2081-6383 | Journal ISSN: 2082-2103
Language: English
Submitted on: Apr 8, 2025
Published on: Dec 16, 2025
Published by: Adam Mickiewicz University
In partnership with: Paradigm Publishing Services
Publication frequency: 4 issues per year
Related subjects:

© 2025 Jan M. Waga, Kazimierz Sendobry, Krzysztof Jochymczyk, Jolanta Pierwoła, Mariusz Grabiec, Bartłomiej Szypuła, Martin Dolejš, Maria Fajer, published by Adam Mickiewicz University
This work is licensed under the Creative Commons Attribution 4.0 License.

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