2021
DOI: 10.4000/archeosciences.8580
|View full text |Cite
|
Sign up to set email alerts
|

The Effect of Remanence in Magnetometer Prospection

Abstract: – Comparison of synthetic magnetograms of dipoles with an illustrative case study.– Remanence explains different anomaly patterns of magnetic dipoles.– The remanence, therefore the total magnetisation, can point in any direction if not acquired in-situ.

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1

Citation Types

0
2
0

Year Published

2022
2022
2023
2023

Publication Types

Select...
2

Relationship

0
2

Authors

Journals

citations
Cited by 2 publications
(2 citation statements)
references
References 5 publications
0
2
0
Order By: Relevance
“…The diurnal variations of the Earth's magnetic field, whose range may be identical to the magnetic anomalies caused by buried anthropologic remains, are removed in the post‐processing (for details, see Hahn et al, 2022). As a complementary method, magnetic susceptibility measurements with the portable kappameter SM 30 (ZH instruments) were performed in situ soil samples and on excavated rocks of the burials and used as a reference for the interpretation of the magnetograms (Bondar et al, 2022; Hahn & Fassbinder, 2021; Hahn et al, 2021).…”
Section: Methodsmentioning
confidence: 99%
“…The diurnal variations of the Earth's magnetic field, whose range may be identical to the magnetic anomalies caused by buried anthropologic remains, are removed in the post‐processing (for details, see Hahn et al, 2022). As a complementary method, magnetic susceptibility measurements with the portable kappameter SM 30 (ZH instruments) were performed in situ soil samples and on excavated rocks of the burials and used as a reference for the interpretation of the magnetograms (Bondar et al, 2022; Hahn & Fassbinder, 2021; Hahn et al, 2021).…”
Section: Methodsmentioning
confidence: 99%
“…Magnetometer prospection relies on the difference in susceptibility and remanent magnetization between soil and archaeological features (Fassbinder, 2015). The shape of the detected anomalies depend on the shape of the feature, its orientation of the total magnetization (Hahn & Fassbinder, 2021) and the direction of the ambient Earth's magnetic field (Ostner et al, 2019). Instruments commonly used for magnetometer surveys include total field and vertical gradiometers.…”
Section: Introductionmentioning
confidence: 99%