2010
DOI: 10.1016/j.nima.2009.11.029
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A preliminary report on the determination of natural radioactivity levels of the State of Qatar using high-resolution gamma-ray spectrometry

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Cited by 30 publications
(33 citation statements)
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“…The value for 40 K is 347.3 76.0 Bq/kg, which is about 25% less the world mean value of 400 Bg/kg, while that for 137 Cs is 10.0 70.2 Bq/kg. The relatively high caesium activity concentration value from this sample could be related to 'soil factors' mentioned above, which effects the movement of rainwater (Wallbrink et al, 1994) The results are consistent with levels reported by Saad and AlAzmi (2002), and similar previous studies from the middle-eastern region (Bou-rabee and Bem, 1996;Bou-rabee, 1997;Tabassum et al, 2012, Al-Sulaiti et al, 2010. Results for all specific activities are less than the world average values.…”
Section: Radioactive Secular Equilibriumsupporting
confidence: 90%
“…The value for 40 K is 347.3 76.0 Bq/kg, which is about 25% less the world mean value of 400 Bg/kg, while that for 137 Cs is 10.0 70.2 Bq/kg. The relatively high caesium activity concentration value from this sample could be related to 'soil factors' mentioned above, which effects the movement of rainwater (Wallbrink et al, 1994) The results are consistent with levels reported by Saad and AlAzmi (2002), and similar previous studies from the middle-eastern region (Bou-rabee and Bem, 1996;Bou-rabee, 1997;Tabassum et al, 2012, Al-Sulaiti et al, 2010. Results for all specific activities are less than the world average values.…”
Section: Radioactive Secular Equilibriumsupporting
confidence: 90%
“…The results of specific of natural radioactivity concentration ( 226 Ra, 232 Th and 40 K) in the present study revealed the highest specific activity in granite samples of 226 Ra was 145.3 Bq/Kg for Chinese sample (GR10) while the lowest specific activity was 9.2 Bq/Kg for Indian sample (GR8), the results presented in Table- The variation of the specific activity concentration ( 226 Ra, 232 Th and 40 K) in the present study of flooring materials due to the geochemical characteristics (mineral content, materials) and geology of the region [18]. Table-3.…”
Section: Results and Discussion Specific Activitymentioning
confidence: 50%
“…The measured BIR values were as a result of terrestrial gamma contribution which were within the dose rate measurement of 10 nSv/hr to about 180 nSv/h obtained in the Southern and other regions of Nigeria except for Jos, Plateau State that is about 0.2 µSv/hr [36] due to mining activities. The calculated GDR arising from terrestrial gamma of BIR measurement for entire four zones of the study area was with mean of 9.312 nGy/hr which was lower when compared with world mean of 59 nGy/hr [32,35]. Also, the AEDR from both terrestrial outdoor and indoor gamma from absorbed gamma dose rate were subsequently estimated for outdoors with mean value of 6.83 mSv/yr, and the evaluated indoor AEDR with mean value of 21.85 mSv/yr were within admissible value when compared with world mean of 460 mSv.…”
Section: Discussion -Radiological Hazard Indicesmentioning
confidence: 70%
“…The major reason outdoor AEDR is lower than the AEDR indoor is that more time is spent indoors as well as radiation contributions from building materials. The acceptable annual effective dose for public without any constraint is 1 mSv/yr for the purpose of safety and with constraint of 0.5 mSv/yr [32,33,35]. Furthermore, the estimated ELCR evaluated was with the mean value of 0.05 × 10 -3 , which was lower when compared with world mean value of 0.29 × 10 -3 [32,35].…”
Section: Discussion -Radiological Hazard Indicesmentioning
confidence: 99%
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