1887
Volume 30, Issue 3-4
  • ISSN: 0812-3985
  • E-ISSN: 1834-7533

Abstract

In their ascent to the aircraft detector system, the gamma-rays recorded in airborne radiometric surveys are attenuated, first by the surface materials wherein they originate, then by the intervening atmosphere. Increased ground-clearance thus entails reduced count-rates. It also implies diminished spatial resolution, because the same cone of incident radiation derives from progressively larger ‘footprints’ that, for a given sampling rate, increasingly overlap. But suitable post-processing of the gridded, twodimensional imagery can be used to correct these types of height-dependent degradation and hence produce sharper, quantitatively useful maps of radioactive isotope distribution. An essential prerequisite for such inverse filtering is noise-suppression, achieved here through maximum-noise-fraction (MNF) transformation of multi-channel data. High-frequency noise amplified by the deconvolution step is brought under control by a variant of Wiener filtering. The combined de-noising and deconvolution process is illustrated by application to an airborne gamma-ray survey from the Marble Bar area, Western Australia.

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1999-09-01
2026-01-13
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  • Article Type: Research Article
Keyword(s): Deconvolution; gamma-radiometry; inverse filtering; Wiener filter

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