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Design and construction of a bespoke system for the detection of buried, iron-rich meteorites in Antarctica

Published online by Cambridge University Press:  22 January 2020

John W. Wilson*
Affiliation:
School of Electronic and Electrical Engineering, University of Manchester, ManchesterM13 9PL, UK
Liam A. Marsh
Affiliation:
School of Electronic and Electrical Engineering, University of Manchester, ManchesterM13 9PL, UK
Wouter Van Verre
Affiliation:
School of Electronic and Electrical Engineering, University of Manchester, ManchesterM13 9PL, UK
Michael C. Rose
Affiliation:
British Antarctic Survey, High Cross, CambridgeCB3 0ET, UK
Geoffrey Evatt
Affiliation:
School of Mathematics, University of Manchester, ManchesterM13 9PL, UK
Andrew R.D. Smedley
Affiliation:
School of Mathematics, University of Manchester, ManchesterM13 9PL, UK
Anthony J. Peyton
Affiliation:
School of Electronic and Electrical Engineering, University of Manchester, ManchesterM13 9PL, UK
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Abstract

Iron-rich meteorites are significantly underrepresented in collection statistics from Antarctica. This has led to a hypothesis that there is a sparse layer of iron-rich meteorites hidden below the surface of the ice, thereby explaining the apparent shortfall. As standard Antarctic meteorite collecting techniques rely upon a visual surface search approach, the need has thus arisen to develop a system that can detect iron objects under a few tens of centimetres of ice, where the expected number density is of the order one per square kilometre. To help answer this hypothesis, a large-scale pulse induction metal detector array has been constructed for deployment in Antarctica. The metal detector array is 6 m wide, able to travel at 15 km h-1 and can scan 1 km2 in ~11 hours. This paper details the construction of the metal detector system with respect to design criteria, notably the ruggedization of the system for Antarctic deployment. Some preliminary results from UK and Antarctic testing are presented. We show that the system performs as specified and should reach the pre-agreed target of the detection of a 100 g iron meteorite at 300 mm when deployed in Antarctica.

Information

Type
Physical Sciences
Copyright
Copyright © Antarctic Science Ltd 2020
Figure 0

Fig. 1. Basic operation of a metal detector.

Figure 1

Fig. 2. Overview of the detector system.

Figure 2

Fig. 3. Coil simulation configuration: a. 1.0 m × 1.0 m coil, b. 1.0 m × 0.5 m coil.

Figure 3

Fig. 4. Simulated response to spherical target at a depth of 30 cm.

Figure 4

Fig. 5. Side view of the channels in a panel encapsulating coils.

Figure 5

Fig. 6. Arrangement for staggering of neighbouring coils to minimize cross-coupling.

Figure 6

Fig. 7. Block diagram of the metal detector.

Figure 7

Fig. 8. Pulse decay with and without metal object present: a. full scale, b. zoomed.

Figure 8

Fig. 9. Pulse sequencing to prevent detector cross-talk.

Figure 9

Fig. 10. Metal detector display box.

Figure 10

Fig. 11. Schematic diagram of the top view of static coil meteorite detection tests.

Figure 11

Fig. 12. a. Plot of signal response with respect to time as a 128.1 g meteorite is moved across the coil at different heights. b. Plot of peak amplitude of the meteorite response with respect to height for all six meteorites.

Figure 12

Fig. 13. Test setup for UK outdoor testing.

Figure 13

Fig. 14. UK outdoor testing: a. detector results, b. environmental sensor data.

Figure 14

Fig. 15. Metal detector tests at Sky-Blu field station, January 2019.

Figure 15

Fig. 16. Sky-Blu field station test: a. detector results, b. environmental sensor data.