1. September 2018
Workshop Berlin PROGRAM
EA20.0 Party Invitation
January, 2018
Searching for the first European peasants
Research project with OREA Vienna

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

EU funded project
in the 7th FWP at the
University of Evora (Portugal)

Exzellenzcluster TOPOI
Freie Universität Berlin /
zu Berlin

Grupo ánfora, G.I.P.
Huelva, Spain

Topographical Survey

arqueocad, S.L., Córdoba, Spain

Geophysical Modelling
Dr. Thomas Günther;

Prof. Dr. Andreas Weller,
TU Clausthal

3D models
cdmb architects, Berlin
GPR / Georadar GPR (Ground Penetrating Radar) is a non-destructive geophysical method used to detect subsurface structures and objects of archaeological or modern origin. Transmitting antennas radiate pulses of electromagnetic waves into the ground which are reflected and/or diffracted when changes in the electrical material properties, especially changes of permittivity (ε), occur. This mainly appears along layer boundaries, stones, walls or foundations, but also along anthropogenic features like cable lines and pipes that cause strong reflections. All reflections are registered by a receiver mounted on the antenna. Travel times of waves are mostly less than 100ns (10-7s), therefore the device can be moved relatively quickly whilst recording. There must be good surface contact between the antenna and the ground to ensure good penetration of the transmitted waves. Information about depth and character of anomalies are obtained from travel time and amplitude of signals. Skilled data processing necessitates special software and a profound theoretical knowledge about geophysical wave theories and methods.

Penetration depth and resolution of the GPR measurements depend on wavelength and frequency of the electromagnetic waves. Non-destructive testing (NDT) requires high-frequency antennas, whereas for geological and geotechnical investigations 100 MHz antennas are best suitable. Best results for archaeological prospection are achieved using 200 to 500 MHz antennas.

In some cases archaeological features and surrounding material have very little variances in their geophysical properties. To achieve clear-cut datasets it is important to clean the investigation sites as good as possible and assure surface contact of the antenna. Furthermore dense measuring grids and large connected areas increase data quality and the success of the measurement. Generally GPR is a good and reliable method to detect walls, stone settings, foundations, cavities or similar structures. Results (reflections) are displayed in radargrams, which are vertical sections of the ground, obtained for each profile measured. Because they display the broad archaeological situation much better, horizontal sections are chosen for visualization more often. Therefore all radargrams (best is a dense set of parallel GPR profiles) are transformed into time slices and displayed as horizontal sections of the ground. Simply said a set of vertical sections with physical information about travel times of electromagnetic waves is processed to give horizontal information incl. depth specifications of buried objects and structures.

GPR is a dependable tool for archaeological prospection that enables optimal excavation planning or even spares the latter. Furthermore it is possible to use high quality results (which always depend on the individual surface and soil conditions of the investigated area) for 3D models of virtual reconstructions.

GPR applications and data examples:
GPR under water GPR signal of pipe 21. rad500_vae_min.jpg 18. timeslices_rorman_small.jpg
Shallow in a lake caused by remains of a medieval castle
GPR signal of a historical water pipe, Potsdam, Sanssouci Park
Application of 500 MHz
antenna in Al Madam (U.A.E.)
GPR time slice on Roman municipium (Spain)
SIR 3000 in the Roman town of Xanten (Germany)
Brochure (German)

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


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