FIELD: applied nuclear geophysics, geology, geochemistry, and metallurgy. SUBSTANCE: gamma- spectrometry technique includes recording of natural or induced gamma- radiation by means of detectors, measuring intensity of spectral fluxes within preset energy spaces of each spectrum whose boundaries are determined by position of reference γ-line in first-detector spectrum. First detector is enclosed by screen that functions to absorb gamma-rays and lighting up X- rays. γ-spectra from each of detectors are recorded simultaneously in two energy ranges; to this end, threshold selection and signal amplification at gain factors of K1 and K2 are conducted; then channel numbers of gamma- radiation peaks of naturally radioactive nuclides are found in full γ-spectra, and energy scales of first-detector n1-spectrum are calculated in first approximation using position of chamber number , maximum of X-ray peak E1, and its energy γ- from definite formula. Minimal-error peak is found in main high-energy spectrum and approximate values of energy are calculated from definite formula using energy scale value. Minimal-error energy peak E
Authors
Dates
2000-11-20—Published
1997-03-26—Filed