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Details of Grant 

EPSRC Reference: EP/N508391/1
Title: Ultra-Low Frequency Magnetic Induction Tomography with Atomic Magnetometers for Security and Defence applications
Principal Investigator: Renzoni, Professor F
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Department: Physics and Astronomy
Organisation: UCL
Scheme: Technology Programme
Starts: 01 April 2015 Ends: 30 November 2015 Value (£): 76,135
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Summary on Grant Application Form
Imaging large objects hidden underground and underwater is a central problem in defence and security. This proposal aims

to investigate the potential for imaging and tomography based on atomic magnetometers in this context, as well as to

provide a proof-of-principle in the case of metallic objects underwater.

Magnetic Induction Tomography (MIT) is a non-contact technique which allows imaging of conductive objects. It relies on

the generation of eddy currents by an oscillating magnetic field in the object of interest and on the detection of the magnetic

field produced by those eddy currents. Position resolved measurements allow then the reconstruction of the image of the

object under the form of a conductivity map.

MIT allows the detection of conductive objects hidden underground/underwater, given the low conductivity of the soil/water.

The depth at which objects can be detected depends on the frequency of the driving magnetic field, as well as on the

sensitivity of the sensors. While very low frequency, of the order of Hz, allows penetration depths of a few kilometres, the

sensitivity of conventional coil-based detectors is very low at such frequencies. The use of atomic magnetometers for MIT

systems, as recently demonstrated by the UCL team, provides an effective solution, as atomic magnetometers are very

sensitive at low frequency, and precisely up to 7 orders of magnitude more sensitive than a coil based sensor of the same

volume. In addition, the technique developed at UCL is suitable for use in an unscreened environment and does not require

any calibration because the atomic magnetometer response is linked to the magnetic field by fundamental physical

constants.
Key Findings
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Summary
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