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A particle detector array deployed to the Murchison Widefield Array in Inyarrimanha Ilgari Bundara, the Murchison Radio-astronomy Observatory

Published online by Cambridge University Press:  24 April 2026

J. Edwin Dickinson
Affiliation:
International Centre for Radio Astronomy Research, Curtin University, Australia
Justin D. Bray
Affiliation:
Jodrell Bank Centre for Astrophysics, Dept. of Physics & Astronomy, University of Manchester, UK
David Kenney
Affiliation:
International Centre for Radio Astronomy Research, Curtin University, Australia
Tom Booler
Affiliation:
International Centre for Radio Astronomy Research, Curtin University, Australia
John Edgley
Affiliation:
Jodrell Bank Centre for Astrophysics, Dept. of Physics & Astronomy, University of Manchester, UK
David Emrich
Affiliation:
International Centre for Radio Astronomy Research, Curtin University, Australia
Amir R. Forouzan
Affiliation:
International Centre for Radio Astronomy Research, Curtin University, Australia
Tegan Gould
Affiliation:
International Centre for Radio Astronomy Research, Curtin University, Australia
Andrew McPhail
Affiliation:
International Centre for Radio Astronomy Research, Curtin University, Australia
Paul Roberts
Affiliation:
Astronomy and Space Science, Australia Telescope National Facility, Commonwealth Scientific and Industrial Research Organisation, Space and Astronomy, Australia
Ralph E. Spencer
Affiliation:
Jodrell Bank Centre for Astrophysics, Dept. of Physics & Astronomy, University of Manchester, UK
Luke Verduyn
Affiliation:
International Centre for Radio Astronomy Research, Curtin University, Australia
Robert Watson
Affiliation:
Jodrell Bank Centre for Astrophysics, Dept. of Physics & Astronomy, University of Manchester, UK
Andrew Williams
Affiliation:
International Centre for Radio Astronomy Research, Curtin University, Australia
Keith Grainge
Affiliation:
Jodrell Bank Centre for Astrophysics, Dept. of Physics & Astronomy, University of Manchester, UK
Andreas Haungs
Affiliation:
Institute for Astroparticle Physics, Karlsruhe Institute of Technology, Germany
Tim Huege
Affiliation:
Institute for Astroparticle Physics, Karlsruhe Institute of Technology, Germany Astrophysical Institute, Vrije Universiteit Brussel, Brussel, Belgium
Clancy W. James*
Affiliation:
International Centre for Radio Astronomy Research, Curtin University, Australia
Steven J. Tingay
Affiliation:
International Centre for Radio Astronomy Research, Curtin University, Australia
*
Corresponding author: Clancy James; Email: clancy.james@curtin.edu.au
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Abstract

We report the design and functionality of the Murchison Widefield Array Particle Detector Array (MWA PDA), an array of eight particle scintillation detectors deployed to Inyarrimanha Ilgari Bundara, the Murchison Radio-astronomy Observatory (MRO). The purpose of the instrument is to identify cosmic ray extensive air showers (EAS) occurring over the core of the MWA radio telescope and generate a trigger to allow radio data on the event to be captured and analysed. The system also acts as a pathfinder for a much larger instrument to be deployed in the core of the low-frequency component of the Square Kilometre Array, SKA-Low, by the SKA’s ultra-high-energy particles science working group. Here, we describe the instrument and associated infrastructure, which has been verified to comply with the strict radio-frequency emissions requirements of the MRO, and was deployed in November 2024. We present calibration data, which demonstrates the ability of each detector to identify individual atmospheric muons at the expected rate, and we characterise the temperature dependence of the system. We describe a sample of 35 500 EAS identified using multi-detector coincidence over a 13-d period, and show how the detector data can be used to reconstruct the arrival directions and approximate energies of these events. We conclude that the particle detector array can reliably trigger on and reconstruct EAS contained within the $\sim$$103 \times 90$ m$^2$ core region, arriving within 20$^{\circ}$ of zenith, at primary cosmic ray energies above $\sim$4 PeV. We have also verified that the detector array can generate triggers, allowing the capture of radio data from the MWA correlator for offline analysis.

Information

Type
Research Article
Creative Commons
Creative Common License - CCCreative Common License - BY
This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (https://creativecommons.org/licenses/by/4.0/), which permits unrestricted re-use, distribution and reproduction, provided the original article is properly cited.
Copyright
© The Author(s), 2026. Published by Cambridge University Press on behalf of Astronomical Society of Australia
Figure 0

Table 1. Data on the deployed detectors, giving detector positions in degrees decimal minutes (ddm), optical lengths of fibre-optic cable to the DAQ, corresponding time-delays relative to Detector 4 due to signal propagation along the fibre, and fibre link loss. The detectors are located at approximately 377.8 m elevation above sea level.

Figure 1

Figure 1. An illustration of the distribution of the detectors #1–8 of the PDA, situated between the tiles of the core and of the east and south hexes of the MWA. All detectors are cabled to the power supply and fibre connection point shown. Also marked is the prototype particle detector described in previous work (Bray et al. 2020). Background features in the image are access roads and vegetation. Imagery from Siwei, processed by SkyFi.

Figure 2

Figure 2. An illustration of the interior of a particle detector. The scintillator material is coloured blue, the bars of wavelength shifter green, and the positions of the SiPMs red. The exit point for the fibre waveguide, and gland plate for supply voltage, are located in the lower left. The RFoF emitters sit in the space to the left of the scintillator. The nine larger circles are feet located on the underside of the box; the four smaller circles on the scintillators are plastic supports keeping the scintillator in place, with the aid of plastic straps (thick grey vertical lines) kept taut with springs (thick black lines crossing the green wavelength shifter). Four handles are attached for ease of transport.

Figure 3

Figure 3. A photograph of Detector 3 as deployed to the MWA.

Figure 4

Figure 4. Photograph of the Bedlam digital signal processing board (top right) mounted in its rack while undergoing lab testing.

Figure 5

Figure 5. Signals seen from an SiPM board in a dark box for four applied voltages.

Figure 6

Figure 6. An example histogram representing the distribution of peak signals from an SiPM board with its SiPM array viewing a bar of wavelength shifter sandwiched between two quadrants of scintillator within a detector. The data were collected on an oscilloscope using a muon paddle placed below one of the quadrants of scintillator as a trigger. The muon paddle was used to sample the sensitivity of the detector across the quadrant. Signal in the first few bins can be attributed to instrumental noise. The remaining data are fit by a Landau function (shown in red) to return the most probable value (mpv) for the response to a single charged particle.

Figure 7

Figure 7. Histograms representing the distributions of peak signal from an SiPM board whose SiPM array was viewing a quadrant of scintillator directly. The SiPM array was positioned at the bottom of the figure between the third and fourth columns of histograms.

Figure 8

Figure 8. The top panel illustrates the transformation of signal between the output of the SiPM board and the output of the optical receiver board. The signal at the output of the SiPM board is shown in red, and that at the output of the optical receiver board in blue. The baselines of both signals are centred on a voltage of zero. The signal path between these points contains a 10 dB in-line attenuator, the master board which incorporates an optical transmitter, a short optical path, and the optical receiver board. The lower panel plots the maximum of the blue trace against the minimum of the red trace, taken over multiple signals, again relative to the baseline voltages at each location. The gain is given by the magnitude of the gradient of the linear fit (red line).

Figure 9

Figure 9. The rates at which signals from a complete detector are exceeded for a range of thresholds and SiPM voltages. The vertical dashed black line represents the most probable signal amplitude (0.0133 V) for a muon traversing the scintillator. The horizontal dashed black line shows the muon flux through the detector sensitive area of $\sim$0.9 m$^{2}$ for a muon flux at sea-level of 1 muon per square cm per minute. The saturation of the rates at around 4 x 104 is the maximum rate at which the oscilloscope could process the data segments.

Figure 10

Figure 10. Raw data describing an event recorded on the 18th February 2025 at 09:59 UTC. Signal is evident in all eight of the traces. The channels number off from top to bottom. The largest signals are seen in Detectors 4, 5, 6 and 7 and it is likely that the core of the shower was within the array. The mean, $\mu$, and standard deviation, $\sigma$, values are calculated from the first 512 samples in the signal buffer, and the maximum and minimum signal heights are also reported. The signals in Channels 1, 2, 3 and 8 are consistent with response to a single particle.

Figure 11

Figure 11. Means of 512 bin samples of system noise. Means for Detectors 1–8 are shown in rows 1–8, respectively.

Figure 12

Figure 12. Standard deviations of 512 bin samples of system noise.

Figure 13

Figure 13. The event rate across the 13 d that the array was operational is shown in black. The peaks in the event rates correspond to early morning at the MRO when temperatures were lower. The red trace shows the air temperature at the site on an inverted scale.

Figure 14

Figure 14. Fraction of triggered events with a contributing signal in each detector (plotted inrows 1–8, respectively), calculated in four-hourly intervals.

Figure 15

Figure 15. Altitude (horizon at $0^{\circ}$, zenith at $90^{\circ}$) and azimuthal (North at $0^{\circ}$, East at $+90^{\circ}$) distributions of reconstructed event arrival directions.

Figure 16

Figure 16. Example of the LDF fit of Equation (1) to an example event with seven measured intensities. Uncertainties on the measurements are dominated by the Poisson statistics of detecting a given number of muons, with smaller contributions expected from the stochastic energy loss of individual muons, and contributions from the electromagnetic component, which we have not quantitatively estimated.

Figure 17

Figure 17. Example of a reconstructed event. Detected signals are shown for each detector, with area proportional to amplitude, and color indicating relative arrival time in microseconds. The direction of the wavefront normal is given by the blue arrow, while the star indicated the estimated impact point. Purple lines correspond to regions of equal particle intensity.

Figure 18

Figure 18. Histogram of reconstructed impact positions on the array, showing the core region only.

Figure 19

Figure 19. Histogram of our energy reconstruction, showing successive cuts, from the initial sample of 11 798 events, after distance cuts (6 147 events), cuts on shower age (3 680 events), and cuts on relative shower age error (1 272 events).

Figure 20

Figure 20. Spectrum of energy proxy assuming a purely muonic component, $E_\mu$, for EAS passing all selection cuts, compared to a power-law fit.

Figure 21

Figure 21. Histogram of zenith angle $\theta_z$ for events passing final selection cuts, compared to a fit of form $\sin \theta_z \cos \theta_z$.