Measurement of secondary cosmic-ray neutrons near the geomagnetic North Pole

Publication date: March 2019

Source: Journal of Environmental Radioactivity, Volume 198

Author(s): Richard S. Woolf, Laurel E. Sinclair, Reid A. Van Brabant, Bradley J.A. Harvey, Bernard F. Phlips, Anthony L. Hutcheson, Emily G. Jackson

Abstract

The spectrum of cosmogenic neutrons at Earth's surface covers a wide energy range, from thermal to several GeV. The flux of secondary neutrons varies with latitude, elevation, solar activity, and nearby material, including ground moisture. We report the results from a campaign to measure count rates in neutron detectors responding to three different energy ranges conducted near the geomagnetic North Pole at CFS Alert, Nunavut, Canada (82.5°N, 62.5°W; vertical geomagnetic cutoff rigidity, R_C = 0 GV) in June of 2016. In November 2016, we performed a follow-on measurement campaign in southern Canada at similar R_C (1.5 GV) and elevations. We conducted these measurements, at varying elevation and ground moisture content, with unmoderated and moderated ³He detectors for thermal and epithermal-to-MeV sensitivity, and with EJ-299-33 pulse shape discrimination plastic scintillator detectors for fast neutrons. Background gamma rays were monitored with NaI(Tl) detectors. Using these data sets, we compared the measured count rates to a predictive model. This is the first ever data set taken from this location on Earth. We find that for the thermal and epithermal-to-MeV neutron measurements the predictive model and data are in good agreement, except at one location on rock-covered ground near 1 km elevation. The discrepancy at that location may be attributable to ground moisture variability. Other measurements, during this campaign and prior, support the assertion that ground moisture plays a critical role in determining neutron flux.

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