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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.

Type
Physical Sciences
Copyright
Copyright © Antarctic Science Ltd 2020

Introduction

Meteorites are found across the globe, with equatorial hot deserts and the cold desert of Antarctica being particularly favourable locations. Despite the inhospitable environment, ~65% of all known meteorites have been retrieved from Antarctica. This is due to the existence of meteorite stranding zones, which are regions of the ice sheet that are tens of square kilometres in size and act to concentrate meteorites together upon their blue ice (i.e. snow-free regions of glacial ice, whose presence is due to the retardation of the ice flow by underlying mountainous terrain; Bintanja Reference Bintanja1999) surfaces (Harvey Reference Harvey2003).

Broadly, meteorites can be separated into ‘iron’ and ‘stony-iron’ (high metallic content or iron-rich) and ‘stony’ (lower metallic content or iron-poor) classifications. The iron-rich samples account for 5% of finds in the rest of the world. However, in Antarctica, iron-rich meteorites occur at a significantly lower proportion, at only 0.5%. This deficit has given rise to the hypothesis of ‘lost’ iron meteorites within the ice sheet (Evatt et al. Reference Evatt, Coughlan, Joy, Smedley, Connolly and Abrahams2016).

The previous work by Evatt et al. (Reference Evatt, Coughlan, Joy, Smedley, Connolly and Abrahams2016) explored this deficit by way of a radiative transfer approach. They showed the underrepresentation could be explained by preferential solar heating of iron meteorites, whose high thermal conductivities and masses allow them to melt faster into the ice than stony meteorites, which are thus more prone to remaining upon the ice surface. Accordingly, this suggests that stony meteorites will be preferentially found by systematic searches, whilst a sparse layer of iron meteorites lies hidden below the surface (Evatt et al. unpublished data 2019). And it is these ‘lost’ englacial iron meteorites that this present study hopes to help locate.

The blue ice of the meteorite stranding zones is formed over a period of many decades from the accumulation of snow and subsequent compression. Blue ice (and generally other forms of land-based frozen water such as snow and firn) has a negligible electrical conductivity (Bradley Reference Bradley1957). By contrast, iron-rich meteorites have a significantly greater electrical conductivity (Ip & Herbert Reference Ip and Herbert1983). Iron-rich meteorites are also magnetic, and thus have a much greater magnetic permeability than the surrounding material. This contrast in electrical conductivity and magnetic permeability allows for the potential to use metal detection technology in order to sense the discontinuity caused when the detector is in the presence of meteorites.

Metal detectors have been used to detect buried or obscured metallic objects for several decades (Nelson Reference Nelson2004). They have been applied to a diverse range of applications, including humanitarian demining, aviation security, food safety, prospecting, archaeology and treasure hunting (Connor & Scott Reference Connor and Scott1998, Bell et al. Reference Bell, Barrow and Miller2001, Craig Reference Craig and Edwards2004, Sweet Reference Sweet2008). The physical principles of detector operation have been understood for many years, and the technology is fairly mature. However, in recent years, metal detector performance has improved significantly as a result of the exploitation of recent advances in electrical engineering; of particular significance is the availability of low-noise analogue devices and the benefits provided through digital signal processing algorithms.

A metal detector exploits Faraday's law of induction to probe a volume for the presence of high-conductivity and/or magnetic materials. Detectors can be implemented using either continuous wave (CW) or pulse induction (PI) configurations (Medek et al. Reference Medek, Nicolics and Schrottmayer2001). Typically, CW detectors operate in the frequency range of 1–100 kHz, depending on the conductivity of the material that the detector is searching for. In this mode of operation, a transmit coil is used to generate a primary magnetic field, as shown in Fig. 1. This primary field causes currents to circulate in nearby metallic materials; these circulating currents produce a secondary magnetic field. The signal in a second coil is continuously monitored and can then be used to detect the changes caused as a result of the interaction of the primary and secondary fields. In contrast, PI detectors transmit an impulse-like magnetic field and use the receiver to monitor the decay of the secondary magnetic fields.

Fig. 1. Basic operation of a metal detector.

Both methods have advantages and disadvantages. Continuous wave detectors offer the greatest sensitivity and are typically used for detection on industrial food processing lines; they also offer the potential to resonate excitation/detection signals, thereby taking advantage of natural filtering to reject out-of-band noise. Pulse induction is preferred for applications where sensors are likely to experience vibration during operation. This is because vibration of the sensor causes variation in the primary magnetic field, which in turn causes potential variation in the signals coupled into the receive coil. However, pulse methods are able to take advantage of the known time domain profiles of signals to ignore the component of the signal relating to the primary field. This allows the potential for implementing signal processing algorithms that look entirely at the decay in the response of the detector (the decay tail), which is used to indicate the presence of a buried object. Therefore, by observing the correct part of the pulse response, much of the noise from vibration can be ignored.

The sensor system described in this paper is designed to be towed behind a snowmobile across an icy surface, with the intention of detecting the conductive meteorites buried beneath the surface. Due to the high levels of vibration that are expected in this application, PI is a better configuration for the detector system described here.

However, after a thorough literature search and discussions with metal detector manufacturers, it was found that no such detection technology was available for use. This has meant the construction of a bespoke meteorite detection system that is both sensitive enough to detect the target objects and able to withstand the Antarctic environment. This paper describes the design and implementation of such a system.

Overview

After discussion between the University of Manchester (UoM) and British Antarctic Survey (BAS), the following system specifications were agreed upon. The system should be able to:

  • Search a wide area effectively. The expected number density is of the order one iron-rich meteorite per square kilometre of blue ice (Evatt et al. Reference Evatt, Coughlan, Joy, Smedley, Connolly and Abrahams2016).

  • Be towed behind a snowmobile at a speed of 10–20 km h-1.

  • Be disassembled and packed into the cargo space of Twin Otter aircraft.

  • Locate an iron-rich meteorite of 30 mm diameter (~100 g) trapped within ice at ≤ 300 mm below the surface.

  • Operate and be stored at temperatures no lower than -40°C.

  • Withstand high wind speeds (up to 50 km h-1) and large amounts of vibration from the scalloped ice surface.

  • Operate with real-time signal processing with visual and audio alarm output to alert the operator and data storage to log position and response.

In order to fulfil the agreed specifications, the configuration shown in Fig. 2 was decided upon. The PI metal detector developed at UoM is a modular design featuring five high-molecular-weight polyethylene panels of the type used to transport fuel in polar regions (Lever & Weale Reference Lever and Weale2012). The panels measure 2.0 m × 1.1 m with a gap of ~0.1 m between each panel, resulting in a detector array with a width of ~6 m. This will allow one detector array travelling at an average speed of 15 km h-1 to search ~1 km2 in 11 h.

Fig. 2. Overview of the detector system.

Each panel contains a coil connected to a self-contained metal detector unit that provides the pulse excitation to the coil, processes the response of the coil to any metal objects within range and transmits a single value derived from the pulse response at a rate of 240 Hz via an Ethernet connection. Ethernet provides a fast and robust connection for two-way data communications between the display box and the metal detectors and has the additional advantage that off-the-shelf solutions for low-temperature and ingress protection (IP) rated cables and connectors are available.

The interconnection box is mounted on one of the two pulk sledges and distributes power from the battery and solar photovoltaic panels mounted on the other pulk sledge to the metal detector units and display unit. The interconnection box also distributes a synchronization pulse to each of the metal detector units and combines the data streams from each detector unit using an Ethernet switch.

The display box is mounted on the front of the snowmobile within the field of vision and easy reach of the operator. It receives the data streams from all of the metal detector units and, when prompted by the operator, records them for later analysis. The data are also processed in real time in order to provide visual and audio cues to the operator when a meteorite is detected by any of the detector units, identifying which panel has passed over the object.

All parts of the system were selected with reference to the agreed specifications, rated to operate at -40°C or less down to the printed circuit board (PCB) component level. Boxes are IP66 rated with PCBs, sockets, etc., mounted using nylon locking nuts to increase resistance to vibration. Sockets, cables and connectors were selected for their resistance to harsh environments.

System design

Coil simulation

A number of electromagnetic simulations were undertaken in order to determine the optimum coil configuration. A major constraint is posed by the fixed width of the panels; this is dictated by the limited space on a Twin Otter aircraft, which will be used to deploy the final system in Antarctica. In order to quickly and efficiently scan a large area, it was determined that the largest possible coil width should be employed. However, there is an important trade-off between the optimum sensitivity depth and coil dimensions. Generally speaking, as coil area increases, the sensitivity to larger objects also increases (at the expense of sensitivity to smaller objects); the magnetic field produced by the coil will also have a greater penetration depth, thereby allowing the potential to sense deeper and larger targets. It was consequently decided to allow a coil of the maximum permissible width (1 m) and to tune the overall length according to the optimal sensitivity to the desired target object.

The simulation was used to predict the system response based on the implementation of Biot-Savart law and using the magnetic polarizability tensor as described in Marsh et al. (Reference Marsh, Ktistis, Järvi, Armitage and Peyton2013) to represent the target object. A spherical target approximation was used to represent the meteorite, and a variety of different coil configurations were examined. Figure 3 shows two of the geometries investigated, namely the 1.0 m × 1.0 m coil and the 1.0 m × 0.5 m coil. In each simulation, an object is scanned across the centre of the coil with respect to the 1 m width, with the distance between the coil and object set at 300 mm.

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

The results of the simulations are shown in Fig. 4. It is possible to see that the coil of 1.0 m length is able to detect the meteorite for longer, demonstrated by the fact that the response is significantly above zero in the range of ± 0.6 m, whereas the coil of 0.5 m length only demonstrates an equivalent non-zero sensitivity range of ± 0.3 m. However, the sensitivity to the meteorite for the 0.5 m coil is significantly greater than that of the 1.0 m coil when the target is directly beneath the centre of the coil (0.00 m displacement). This is indicative of the fact that a 0.5 m coil is better suited to detecting objects at the target depth of 300 mm; it is known that the sensitivity as a function of object depth for this coil will tend towards zero more sharply than for the 1.0 m equivalent. As the specification for the system requires the detection of meteorites down to 300 mm, it is desired to select the coil design that offers the best sensitivity in this range. Consequently, the 1.0 m × 0.5 m coil was selected as the optimal design for this depth range.

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

Panel design

The design uses a single coil to transmit the excitation pulse and receive the signal from the buried object. The coil is constructed from 15 turns of 0.22 mm2 PVC-insulated copper wire, with the coil encapsulated into each panel using a two-part polyurethane potting compound, as shown in Fig. 5. As shown in Fig. 6, the coils are offset on neighbouring panels to reduce interference between adjacent coils.

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

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

Each panel also contains a temperature sensor and accelerometer, which are used for diagnostic purposes and to monitor the impact of temperature and vibration on the system. Using this arrangement, it is possible to discount any apparent metal detector signals that occur as a result of vibration, rather than from metallic targets.

Metal detector

The metal detector unit is controlled by a Red Pitaya single-board computer (SBC1). This device was chosen for its 14 bit, 125 MS s-1 analogue-to-digital convertors required for accurate measurement of the response signal and its powerful on-board processor needed to process the detector response for real-time detection. It was temperature tested in-house as fully operational down to -30°C prior to its inclusion in the system.

Figure 7 shows a block diagram of the metal detector unit. A 1 V excitation pulse with a repetition rate of 1 kHz and a 25% duty cycle is supplied from SBC1 and applied to the pulse driver circuit. The transmit–coil–receive part of the circuit is of a type widely documented elsewhere (Corbyn Reference Corbyn1980) and is built around a MOSFET switching circuit on the transmit side and diode clipping to reject the high-voltage part of the pulse on the receive side.

Fig. 7. Block diagram of the metal detector.

Initial amplification is provided by variable gain stage 1. Figure 8 shows the output of the stage with the gain set low to allow the full pulse response signal through. It can be seen that the presence of a metal object causes a change in the decay of the signal with maximum difference at ~0.265 ms. It is this change in the decay of the signal that is harnessed for metal detection. In normal operation, the gain of this stage is set high to amplify the change in the pulse decay. A DC offset is also introduced here in order to zoom in on the part of the signal of interest.

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

The summing amplifier sums the amplified and filtered pulse decay with a compensation signal. The compensation signal is generated in response to the signal received from the output of the summing amplifier and acts to reduce the output of the summing amplifier to near zero when no object has been detected. Two final variable gain stages are included in order to boost the amplitude of the signal sent back to SBC1 for processing.

The compensation signal is generated using a proportional controller on SBC1, based on the measured signal after the summing amplifier. The compensation signal is continuously updated such that the voltage at the output of the summing amplifier is near zero. The speed of convergence can be controlled by changing the "feedback gain or by changing the rate at which the compensation signal update routine is called, as it is not called for every input signal.

The nulling speed must be chosen such that it removes changes in the signal due to slow drift phenomena, but at the same time the nulling loop should not significantly reduce the signal from a buried target. The nulling loop also must limit its response to vibrations in the metal detector system as much as possible.

A band-pass filter is applied to the input waveform, primarily to reduce the effect of vibrations. A small number of points are then extracted from the data series and fed through moving-average filters. The detector output is derived from a linear combinations of these points. The exact time indices for these points were derived empirically in order to maximize object response and to minimize the response to vibrations. A combination of band-pass and low-pass filters are used to extract the envelope of the object response in the detector response, and this forms the final output of the system. The high- and low-pass filters are implemented using infinite impulse response Butterworth filters and applied forwards and backwards in time in order to cancel the phase response due to the filter. These filters are highly tuned to the speed of the snowmobile, which should therefore be kept as close to 15 km h-1 as possible.

In order to further mitigate against detector cross-talk, the metal detectors are all synchronized such that neighbouring detectors are not transmitting or receiving simultaneously. Figure 9 shows the sequencing of these pulses. The basic mode of operation is such that a master synchronization pulse provides a 1 kHz square wave. Several copies of this square wave are buffered, with some being inverted with respect to the master signal. Neighbouring detectors receive different synchronization signals, with a non-inverted signal being bordered by detectors firing using an inverted signal. Transmit pulses fire for 50% of the positive half of the detector's synchronization pulse, and a signal is acquired for the second half of the synchronization pulse; at all other times, the receive signal is ignored. This allows detectors that are not triggered to effectively ignore any induced voltages that originate from neighbouring coils. This, in combination with the aforementioned staggering of coils, allows for an effective method of interference prevention.

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

Display box

Figure 10 shows the display box for the system. The box is designed to be mounted on the front of the snowmobile within the field of vision and easy reach of the operator. Sealed toggle switches designed for outdoor use are employed in the construction, along with self-contained LED units rated to IP68. The display box features an external GPS aerial and a sealed 3.5 mm jack socket for the audio output.

Fig. 10. Metal detector display box.

The display box contains a BeagleBone Black, a second type of single-board computer (SBC2), along with a GPS unit and some of the signal conditioning hardware required to maintain synchronization of the metal detector units.

SBC2 is used as the main interface between the metal detector boxes and the switches and LEDs mounted on the display box. It also acts as the server for the Ethernet network that is used within the system. Each metal detector box transmits the metal detector response, current box temperature and vibration data from the accelerometer. This information is stored on SBC2, along with corresponding GPS data. The LEDs provide an indication of the total response of all metal detectors combined, and they also provide an indication of which detectors have triggered above a predefined threshold; this information is used to aid location of meteorites when the detector is triggered. SBC2 is also responsible for displaying status information, such as whether the GPS lock has been acquired and whether the system is currently set to log data, and it has some basic user inputs that allow logging to be toggled on and off; in addition, it resets any triggered metal detectors. A final key aspect of this box is that it sources the synchronization pulses that ensure that all metal detector transmit pulses fire in a predefined sequence so as to minimize cross-coupling of signals.

Interconnection box

The interconnection box provides a central hub for data connections, power distribution and switching. It is located on one of the pulk sledges along with the batteries, with the solar panels located on the other sledge (see Fig. 2). Sealed lead acid batteries rated at 12 V and 50 A h were selected as the most appropriate option, as this type of battery has been successfully used by BAS in similar applications. Two batteries connected in series provide the 24 V required to run the system and are connected to the solar panels for charging.

The interconnection box receives the synchronization pulse from the display box described above. This is buffered in order to compensate for the long cable runs and is sent out to all of the detector units. It also contains an industrial eight-port Ethernet switch in order to allow the metal detector units to transfer data to the display box and to allow the user to interface with any of the metal detector units and the display box.

Static testing

As a first assessment of the capabilities of the system, a number of static tests were carried out using six different iron-rich meteorites from the Campo del Ciolo meteorite field in Argentina. The samples range in weight from 2.56 to 128.1 g. As a guide, the mean composition of Campo del Cielo meteorites is 92.6% Fe and 6.67% Ni, with remainder being Co, P, Ga, Ge and Ir.

As shown in Fig. 11, the meteorites were placed in a plastic caddy and pulled across the detector coil on a wooden track with the track placed at different heights ranging from 5 to 60 cm between the meteorite and the coil. The system used was a simplified version of the system described in the ‘System design’ section, consisting of a battery, metal detector unit and a laptop for data acquisition.

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

Figure 12a shows a plot of the signal amplitude as the 128.1 g meteorite was passed across the coil at heights from 10 to 60 cm. It can be seen from the plot that at 10 cm the top of the curve is flattened, as the signal through the metal detector circuitry has exceeded the maximum amplitude. The maximum amplitude decreases as the distance between the coil and object increases, reducing to a negligible level at 60 cm.

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 12b shows a plot of the peak amplitudes of the meteorite responses with respect to the distance between the coil and object for all six meteorites. It can be seen from the plot that, as would be expected, the response decreases as the size of the object decreases. The inconsistencies in the response curves can be explained by the irregularly shaped (non-spherical) meteorites invoking different responses when passed through the detector at different orientations with respect to the coil. It can also be seen from the plot that the 2.56 g meteorite invokes some response at 5 cm, although this would fall below the noise floor in the final system, whereas the 10.2 g meteorite has a strong response at ≤ 10 cm. At the upper end of the weight range, the 49.3 g meteorite is clearly detectable at ≤ 30 cm, whereas the response to the 128.1 g meteorite levels off at distances greater than ~45 cm.

The results show that the target of detecting a 100 g meteorite at a depth of 30 cm should be attainable using this system. However, it should be noted that this test with a static coil and the meteorite moving with respect to the coil would give a favourable performance for the system. Once vibration and other factors are taken into account, performance is expected to decrease significantly.

UK field testing

In July 2018, an outdoor trial of the system was conducted in the UK. The test was conducted on an open, grassy surface, and the air temperature was ~25°C; consequently, this test was not considered to be fully representative of conditions in Antarctica. The main purpose of the testing was to provide an evaluation of the performance of the detector when subjected to the stress caused by dragging at representative target speeds.

A single-coil panel and metal detector box were connected to the system, and this system was towed behind a car; sufficient length was allowed such that the metallic components in the car did not interfere with the performance of the detector. A total of seven 100 g cylindrical iron meteorite surrogates were buried at depths ranging from 0 cm (flush to the ground) to 30 cm; the experimental arrangement is shown in Fig. 13.

Fig. 13. Test setup for UK outdoor testing.

The ground was checked with a handheld metal detector, a Vallon Minehound VMH3CS (https://www.vallon.de/en/metal-detectors-and-magnetometer/vmh3cs-compact-metal-detector), prior to conducting the test in order to confirm that the mineral content of the ground would not interfere with the detector and to perform an initial check for any scrap metallic components.

A representative plot showing the detector response is shown in Fig. 14a. The regions in which the detector was stationary, moving in a metal-free zone and moving over the target zones are indicated in shaded red, yellow and green areas, respectively. In an ideal case, the responses in the red and yellow areas would be indistinguishable from one another; this would demonstrate complete vibration resilience from the system. It can be seen that there is a small yet noticeable difference between these two states. The flush targets and those buried down to 20 cm are all clearly visible above the background noise level and follow the anticipated trends. However, the peak in the region labelled as 30 cm is inconsistent with the expected response. The response would be expected to continue the decreasing trend shown by the other targets, and consequently it should be lower than the peak identified at 20 cm. This peak was measured repeatedly across several scans and is closer to the 20 cm peak than would be expected from the experimental setup. The location of the peak does not correlate with any peaks from the accelerometer data and is therefore not considered to be the result of vibration. The most probable cause for this is that a scrap piece of metallic clutter was present in the ground at this location; given that the signal response is comparable with that of a meteorite surrogate buried to a depth of 20 cm, this could correspond to either a very small object close to the ground or a larger, deeply buried object. It is expected that a search with the Vallon Minehound VMH3CS would find any small metallic targets in the scan region; however, as the coil used in the meteorite detection system is considerably larger than the sensor head of the Vallon Minehound VMH3CS, it is expected that the meteorite detection system will be more sensitive to objects buried at depth. With this in mind, it is probable that this signal is caused by an object larger than the meteorite surrogate.

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

The difference in magnitude of the flush targets is not considered to be a cause for concern. A truly identical response would only be observed if the coil took exactly the same trajectory over each target. This, coupled with the fact that the sensitivity gradient is sharpest in regions closest to the coils (thus small positional errors can have a large impact on object response), means that these results are considered valid. The 0–20 cm target responses also demonstrate a typical sensitivity drop-off with respect to distance from the detector.

Figure 14b shows the temperature and accelerometer data for the test shown in Fig. 14a. The detector temperature remains at a constant 38°C. It should be noted that localized heating causes this to be significantly above ambient temperature; this is by design to assist the final system in coping with polar climates. It is possible to see that the accelerometer measures constant values when the detector is static, but varies significantly during motion, with a peak acceleration of 4.75 g. This peak is caused by the initial motion of the panel as the vehicle sets off. Whilst Fig. 14a demonstrated that the detector response was not completely immune to the effects of vibration, it is possible to see that the variation is considerably smaller than that measured by the accelerometer.

Initial Antarctic testing

In January 2019, some preliminary testing of the developed system was carried out at the Sky-Blu field station, Antarctica (74°50‘59‘‘S, 71°34‘0‘‘W). Figure 15 shows the full five panel metal detector being towed behind a snowmobile, configured as shown in Fig. 2. During the tests, the power consumption of the full system was measured as 80 W (peak).

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

Figure 16a shows some representative data for one of the metal detectors. In this experiment, two of the same 100 g iron surrogates used in the UK-based testing were buried flush to the ice surface and to a depth of 10 cm. The results show that both targets are clearly detectable above the noise floor of the system. This result is particularly encouraging, as the level of vibration experienced by the detector during these trials was significantly greater than in the UK-based testing, as shown in Fig. 16b. This provides confidence in the ability of the system to reject noise due to vibration, as is a fundamental requirement of the final system. Full environmental sensor data for the metal detector measurements in Fig. 16a are shown in Fig. 16b. These results show that the objects remained detectable despite a variation in velocity of ~3 km h-1 during the 25 s scan time. Also of note is the fact that the detector electronics were operating at approximately 7°C, despite an outdoor air temperature of approximately -10°C. It is known that the detectors produce some localized heating, and the electronics have clearly transitioned freezing point to reach this value from a cold start. The fact that the electronics have passed through this condensation point without any concerns is also particularly encouraging.

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

Summary

The design and initial testing of a bespoke metal detection system to locate iron-rich meteorites buried in a subsurface ice layer in the Antarctic has been detailed in this paper. The system will be used to investigate the underrepresentation of iron-rich meteorites in samples collected from the Antarctic. The future deployment of this system in the Antarctic poses significant challenges and constraints that have to be considered during the design and evaluation process. For example, the requirement that the system should be capable of being disassembled, packed into a Twin Otter aircraft and reassembled in the field poses constraints on the size of the coils, and the prevailing weather conditions require a wide range of operating and storage temperatures.

The system has been designed with the aim to detect meteorites weighing ~100 g down to 30 cm below the surface while the system is moving at a speed of ~15 km h-1. Based on the width of the system (6 m) and the target speed, it is expected that an area of 1 km2 can be scanned in ~11 h.

Electromagnetic simulations were used to determine the optimal coil size for the detection problem at hand. The width of the coils is constrained at 1 m due the available space on the Twin Otter aircraft, and it was decided to use the full width available. Based on the simulations, it was decided that a coil length of 0.5 m would give the optimal response to targets buried down to 30 cm.

The metal detectors are based on PI technology in order to reduce the impact of vibration-induced noise on the measurements. A summing amplifier is used to back off the background signal, caused mostly by the primary field, electronically using an out-of-phase output calculated and generated by a Red Pitaya single-board computer. A polyurethane compound is used to encapsulate the coils into high-molecular-weight polyethylene panels measuring 2.0 m × 1.1 m. The electronics for the PI detector are mounted in a box on the panels, making each panel a self-contained metal detector. The final system is made up of five panels, with an interconnection box to connect all of the panels together. Finally, an indicator box is mounted on the snowmobile to provide real-time audio-visual feedback to the operator.

Initial tests were performed with the object moving relative to the coil, which was static. This represents the ideal scenario for this system, because the coil was not experiencing any vibration. These tests showed that it is possible to detect 100 g targets to distances of 30 cm. Subsequent testing was performed in the UK and at Sky-Blu field station in the Antarctic.

In the UK, a car was used to drag a single panel over a grassy surface with buried objects ranging from 0 to 30 cm in depth. This test was not a fully representative test, but was used to verify the operation of the system when subjected to the mechanical stresses of being dragged at the target speed. In these tests, the system was able to detect objects down to at least 20 cm. While a clear peak in the signal can be seen at 30 cm, the response differs from the expectation, suggesting that it may have been caused by a piece of metallic clutter rather than the buried target.

In the Antarctic, the full mechanical arrangement was evaluated, with five panels being dragged behind a snowmobile at ~15 km h-1 over blue ice. The air temperature was also representative of what the final system may encounter at -10°C. In these tests, the system clearly detected buried targets at 0 and 10 cm depths, respectively. The outcome of this test was very encouraging, as it was the first test of the full system in Antarctic conditions.

In both of these tests, the acceleration experienced by the panel was recorded using an accelerometer. Based on these measurements, it appears that the system experienced stronger vibrations on ice than on the grassy surface. This suggests that more work may have to be done in order to harden the final system against vibration, either through mechanical means or in the form of post-processing of the recorded data.

Prior to the deployment of the system to Antarctica, more system testing will be performed in the Arctic in March 2019. Data captured during that trial will be used to further refine the system, in particular the processing algorithms, in order to maximize the detectability of buried targets despite vibration. The final deployment of the system to search for buried iron-rich meteorites will take place during the austral summer of 2019–20.

Acknowledgements

This work was conducted under ‘The Lost Meteorites of Antarctica’ grant from Leverhulme Trust no.: RPG-2016-349. The authors would also like to recognize the contribution from ESPRC project EP/R002177/1 ‘Reducing the Threat to Public Safety: Improved metallic object characterisation, location and detection’.

Author contributions

JWW, LAM and WvW designed and built the equipment and took the lead in writing the manuscript. All authors provided critical feedback. GE, ARDS, LAM, WvW and JWW carried out UK field trials. MCR and GE carried out Antarctic field trial. MCR advised on Antarctic ruggedization of the equipment. AJP helped to supervise the work. GE proposed and led the work.

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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.

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

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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.

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

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