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SERVICETECHNOLOGYABOUT USREFERENCESPROJECTS
 NEWS
2 February, 2017
Presentation of Ullastret Monography
MAC Barcelona


March 14, 2014:
Bradford West Yorkshire

Commercial Archaeological
Geophysics Seminar


February 3, 2014: BDG confirmed quality in professional geophysics

January 2014: Book release: Good Practice in Archaeological Diagnostics
Non-invasive Survey of Complex Archaeological Sites. Editors: C. Corsi, B. Slapsak, F. Vermeulen. Springer








 PARTNERS
COOPERATIVE PARTNERS
Archaeology
RADIO PAST
www.radiopast.eu
EU funded project
in the 7th FWP at the
University of Evora (Portugal)


Exzellenzcluster TOPOI

www.topoi.org
Freie Universität Berlin /
Humboldt-Universität
zu Berlin

Grupo ánfora, G.I.P.
www.anforagip.com
Huelva, Spain

Topographical Survey

arqueocad, S.L., Córdoba, Spain
www.arqueocad.com

Geophysical Modelling
Dr. Thomas Günther;
Hannover
www.resistivity.net

Prof. Dr. Andreas Weller,
TU Clausthal
www.ifg.tu-clausthal.de

3D models
cdmb architects, Berlin www.barlieb.com
Video: Geomagnetic test measurements with an 8-channel fluxgate array mounted on a self-developed boat driven by an electric motor (near Potsdam).

Magnetic survey
Spatial deviations of the natural magnetic field can be registered with the help of geomagnetic measurements. These deviations occur due to magnetic embeddings in the top soil which affect the magnetic field characteristics locally. The natural magnetic field is a three dimensional vector field measured in Tesla [T ] (SI unit describing magnetic field strength). It is composed of the actual Earth's magnetic field (ca. 50.000 nT), distortions caused by solar storms and a local anomaly field (up to several 100 nT). When it comes to industrial and archaeological prospection the latter is the component of main interest. Geomagnetic prospection is often the most effective survey method for non-destructive investigation of archaeological sites. Herein two techniques can be used to obtain the data of interest. Either the field components are separated during the measurement using orientated gradiometers, or the total field is measured and the components are separated in subsequent data processing.

Magnetic anomalies of archaeological features result from induced or remanent magnetism. Induced magnetism is caused by the Earth's magnetic field and is very much dependent on the susceptibility of the material. The susceptibility describes the degree of magnetization of a material in response to an applied magnetic field and can be either positive or negative. Magnetic anomalies of pits, ditches and postholes for instance are often detectable through positive induced magnetisation of a few nT. Remanent magnetisations have various causes, a well known one being thermoremanent magnetisation. This occurs when ferromagnetic materials are heated above the Curie-Point and cool down again, causing the magnetic moments to partially align within magnetic domains. Thus, fireplaces, burnt clay, fired ceramics and bricks can easily be detected on account of their special magnetic characteristics.

Ammaia Magnetic Data and Interpretation

Roman city of Ammaia (Portugal), eastern suburbs: magnetic mapping (+/-30 nT) and GIS-based interpretation. Project RADIOPAST.

Eastern atlas’ aim to produce high quality magnetic maps necessitates high resolution. Therefore dense measure grids are chosen in the field. Data points are collected every few cm in the direction of the profile, the sensor separation being 50 cm. With the help of a multi-sensor cart system up to 10 sensors can be carried at a time. The special design allows the cart system to be operated even over complex and rough terrain. In this way, non-destructive magnetic investigations of large areas can be completed in reasonable times. Between 2 and 10 ha per day can be surveyed depending on terrain conditions (steepness, soil, vegetation especially trees, modern obstacles etc.). Furthermore the system is set up with real-time GPS-positioning and special hardware and software that makes it possible to visualize and interpret the magnetic data whilst still in the field. Our team is continuously developing new hard- and software solutions with a view to offering the best magnetic maps technically possible. We also offer bespoke solutions for special or difficult investigation areas (eg. geomagnetic in olive groves with retractable probes).

Systems and configurations

Wheeled fluxgate gradiometer array with 10-channel data logger, driven by hand or by ATV
10-Sonden-Fluxgate-Array 10 channel fluxgate array driven by ATV
Mobile fluxgate gradiometer array with 6-channel data logger, applicable in plantations and oliven groves.
Cart system setup with 4 caesium-sensoren and two 2-channel data logger (Geometrics) measuring the magnetic total field respectively magnetic gradient.
Portable fluxgate gradiometer array, in hilly terrain with swivel-mounted sensors
Prospection in shallow water: Multi-channel fluxgate gradiometer array fitted to lightweight boat - combinable with GPR and sonar investigations
31. Mag_Wasser8_small.jpg 32. Mag_Wasser10_small.jpg
 DOWNLOAD
ARCHAEOPROSPECTION
Brochure (German)
download


TECHNOLOGY
Geomagnetics (German)
download
IP geoelectrics at slag heaps (English)
download
(Poster at Conference on "Early Iron in Europe – Prehistoric and Roman Iron Production", Hüttenberg, Austria, Sept. 2008)


ENGINEERING AND
ENVIRONMENTAL GEOPHYSICS

Geophysics in civil engineering
download
(Excerpt of a dissertation at
TU Berlin by Dipl.-Ing. Holger Böhm, in German)


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