2005
DOI: 10.1016/j.jenvrad.2005.02.017
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Application of NaI(Tl) detector for measurement of natural radionuclides and 137Cs in environmental samples: new approach by decomposition of measured spectrum

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Cited by 11 publications
(8 citation statements)
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“…NaI(Tl) detectors are also being extensively used for the estimation of long lived fall out fission product nuclides like 137 Cs in environmental samples. Many gamma spectrometric methods are developed to experimentally determine these radio nuclides in samples employing different type of scintillation detectors [2,3]. The poor energy resolution of these detectors makes the analysis of the complex gamma ray spectrum very difficult especially when many nuclides are present.…”
Section: Introductionmentioning
confidence: 99%
“…NaI(Tl) detectors are also being extensively used for the estimation of long lived fall out fission product nuclides like 137 Cs in environmental samples. Many gamma spectrometric methods are developed to experimentally determine these radio nuclides in samples employing different type of scintillation detectors [2,3]. The poor energy resolution of these detectors makes the analysis of the complex gamma ray spectrum very difficult especially when many nuclides are present.…”
Section: Introductionmentioning
confidence: 99%
“…Further investigations are therefore carried out to improve the ability of a NaI(Tl) spectrometry for quantitative determination of radioelements. But even the method presented by Muminov et al (2005) still is based on subtraction of spectra and by taking into account mainly the total absorption peak. On the other hand, radioactive decay obeys Poisson statistics stating the relative error for n counts to be 1= ffiffiffi n p .…”
Section: Introductionmentioning
confidence: 99%
“…1) the measured spectra (1) into background (2), 226 Ra (3), 232 Th (4), and 40 K (5) components contained in the sample. To do this, we used time-normalized measurements of the spectra of inert samples (a Marinelli vessel filled with table salt) and standard samples of 226 Ra, 232 Th, and 40 K from the OMASN kit filled to densities similar to those of the samples being studied and the formula S n = S -F -Ra -Th -K [2], where S is the measured spectrum, F is the background spectrum, and Ra, Th, and K are the spectra of 226 Ra, 232 Th, and 40 K, respectively. The activities of the standard sources were A Ra = 2580 ± 180, A Th = 10 ± 4, A K = 560 ± 60, and A U = 90 ± 20 Bq/kg.…”
mentioning
confidence: 99%