Geophysical Survey: How Does It Work?
Over the last few weeks our students (see fig.1) have been undertaking
geophysical surveys of the castle grounds under field technician Dr. Philip
Rowe using Ground Penetrating Radar. GPR is a non-invasive
technique which was selected to gain access to the areas of Berkeley Castle
which cannot be excavated.
High frequency radio waves are used by the GPR to detect
subsurface features such as walls, buildings and ditches. The GPR system consists
of an antenna with wheels, an interface display, a battery and a radar control
unit (see fig. 2). The GPR detects buried features by emitting electromagnetic
waves from the antenna. The transmitted waves bounce off buried objects, causing
them to be reflected back to the GPR (see fig. 3), where the control unit
transmits the data from the antenna to the user interface display where it can
be viewed. It is commonly thought that GPR allows you to see through the ground
like an X-ray. This is a common misconception – in reality GPR data can be
difficult to interpret and only suggests the location of potential archaeological
structures, where electromagnetic waves are being reflected off a buried feature.
An example of the data received through GPR surveys can be seen in fig. 4 –
potential structures are seen in the data as curves (these are indicated by
arrows). The vertical axis represents the depth of the features – the deeper
they are, the older they are. The horizontal axis shows where the features are
in space.
Figure 2. An labelled digram of a GPR. |
Figure 3. The basic principles of GPR. |
Figure 4. Example of the data which results from GPR survey. |
GPR can be heavily affected by soil type and weather, as
moisture in the soil reduces the accuracy of the data – luckily we’ve had
lovely weather the last few weeks. GPR has been especially useful in areas such
as the inner keep of the castle and the carpark, while are covered in stone or
tarmac and can therefore not be excavated. See fig. 5 for a guide to where GPR
surveys have been carried out around the castle.
Figure 5. Map showing the areas of the castle which have been surveyed using GPR |
So far this year, geophysical survey using GPR has revealed
several structures around the castle, which may include a well, a drain, and Victorian
houses. However, we cannot know for certain
what features are present until they are excavated, and this is unfortunately impossible
in some areas of the castle. Advanced techniques such as GPR can hopefully be employed throughout the castle and grounds to help unravel more of Berkeley's rich history in the future.
References:
Global GPR Services Inc. (Unknown). How a geophysical survey
works. [Image]. Available at: http://www.global-gpr.com/gpr-technology/how-gpr-works.html.
[Accessed on 06/06/16]
Google Earth. (2016). Satellite
image of the Berkeley area with annotations. [Image]. Available at: https://www.google.co.uk/maps/@51.6895798,-2.4574207,421m/data=!3m1!1e3
[Accessed on 06/06/16]
Lambert Locations Pty Ltd. (2016). Labelled diagram of a GPR. [Image]. Available
at: http://www.lambertlocations.com.au/ground-penetrating-radar/groundpenetratingradar/.
[Accessed on 06/06/16]
Tapatio. (2007). Example of geophysics data with annotations.
[Image] Available at: https://en.wikipedia.org/wiki/Ground-penetrating_radar. [Accessed
on 06/06/16]
-Hattie Ford
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