Article, 2024

Calibration of buried NaI(Tl) scintillator detectors for natural radionuclide measurement based on Monte Carlo modelling

Radiation Physics and Chemistry, ISSN 1878-1020, 0969-806x, 1359-0197, Volume 222, Page 111803, 10.1016/j.radphyschem.2024.111803

Contributors

Chambon, Amalia 0000-0002-3733-3226 (Corresponding author) [1] Klinkby, Esben Bryndt 0000-0002-1908-5644 [1] Bu, M. [1] Murray, Andrew Sean 0000-0001-5559-1862 [2] Kook, Myung-Ho 0000-0002-5558-3405 [1] Olesen, H. [1] Nielsen, K.B. [1] Lauritzen, Bent 0000-0001-7173-1650 [1]

Affiliations

  1. [1] Technical University of Denmark
  2. [NORA names: DTU Technical University of Denmark; University; Denmark; Europe, EU; Nordic; OECD];
  3. [2] Nordic Laboratory for Luminescence Dating
  4. [NORA names: Unclear Universities; University; Denmark; Europe, EU; Nordic; OECD]

Abstract

Measurements of naturally occurring concentrations of 40K, and of the decay series of 238U and 232Th, are of interest in the earth sciences in general, and in particular, scintillator-based gamma spectrometers can be used for the low cost determination of burial dose rates in natural geological samples. We are currently developing a robust, portable, wireless detector specifically intended for field measurement of natural radionuclide concentrations and hence, the calculation of dose rates. One of the challenges in developing and applying such an instrument is reliable calibration. Most calibrations of field instruments depend on access to non-finite matrices of known K, U, Th activity concentrations, in either a 4π or 2π geometry; these are only available at a few facilities around the world. Here we investigate an alternative approach, based on the measurement of small samples containing well-known activity concentrations of only K or U or Th, and Monte-Carlo radiation transport modelling to convert the observed spectra into those expected from specific activity concentrations in a non-finite 4π geometry. We first validate our modelling procedure by simulating these observed spectra. The non-finite matrix calibration spectra are then predicted, and least-squares fitted to the spectrum observed at the centre of a 1 m3 of granite chips; the resulting predicted U, Th and K activity concentrations are compared with independently known values.

Keywords

Carlo model, Earth, Monte, Monte Carlo model, Monte-Carlo, NaI(Tl) scintillation detector, Th, Th activity concentrations, activity, activity concentrations, alternative approach, approach, calculation of dose rates, calculations, calibration, calibration of field instruments, calibration spectra, centre, challenges, chip, concentration, decay, decay series, detector, dose rate, earth sciences, facilities, field, field instruments, field measurements, gamma spectrometer, geological samples, geometry, granite, granite chips, instrument, least squares, low-cost determination, matrix, measurements, model, modeling procedure, natural geological samples, natural radionuclide concentrations, observed spectra, predicting U, procedure, radiation transport model, radionuclide concentrations, radionuclide measurements, rate, samples, science, scintillation detector, series, spectra, spectrometer, transport model, values, wireless detector, world

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