2013
DOI: 10.5923/j.jnpp.20120206.03
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Natural Radioactivity and Associated Dose Rates in Soil Samples of Malnichera Tea Garden in Sylhet District of Bangladesh

Abstract: The activ ity concentrations of naturally occurring radionuclides 226 Ra, 232 Th and 40 K, were measured by using a Broad Energy Ge (BEGe) detector for soil samples collected fro m the Malnichara tea garden in Sylhet district of Bangladesh. The average activity concentrations of 226 Ra, 232 Th and 40 K in soil samples were found to be 55.284±4.68, 125.270±5.81 and 497.91±43.83 Bqkg-1 , respectively. The results obtained for the corresponding nuclides are slightly higher than the world wide average values of 35… Show more

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Cited by 27 publications
(23 citation statements)
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“…The Ra eq in the study area ranges from 60.41 to 635.22 Bqkg Organization of Economic Cooperation Development (Miah et al, 2012 . This value is higher than the world average value of 60 nGyh -1 (UNSCEAR, 2000), which indicates that the dose from the study area is higher than most places in the world.…”
Section: Resultsmentioning
confidence: 99%
“…The Ra eq in the study area ranges from 60.41 to 635.22 Bqkg Organization of Economic Cooperation Development (Miah et al, 2012 . This value is higher than the world average value of 60 nGyh -1 (UNSCEAR, 2000), which indicates that the dose from the study area is higher than most places in the world.…”
Section: Resultsmentioning
confidence: 99%
“…Natural radionuclide in soil contributes a significant amount of the population through inhalation and ingestion. The main contributors of radionuclides are 40 K and 232 Th and these radionuclides are not uniformly distributed in soils and vary from region to region [Miah et al 2012]. Natural radioactivity is wide spread in the environment and it exists in various geological formations in soil, rocks, plants, water and air.…”
Section: Introductionmentioning
confidence: 99%
“…The absorbed dose rates in outdoor air (D) at about 1 m above the ground surface were calculated. The conversion factors used to compute absorbed gamma-ray dose rate in the air corresponds to 0.46 nGy h -1 for 226 Ra, 0.62 Gyh -1 for 232 Th and 0.042 nGyh -1 for 40 K. Therefore, D R can be calculated according to [1,3]: D R (nGyh -1 )=0.46 A Ra +0.62A Th +0.042 A K ( 3)…”
Section: Air-asorbed Dose Ratementioning
confidence: 99%
“…The 226 Ra subseries contribute about 98% of the external γ dose induced by whole 238 U series. Radiological hazard parameters are calculated based on the specific radioactivity of 40 K, 226 Ra and 232 Th in the soil samples [1][2][3]. The low resolution energy of the NaI(Tl) detector with full width at half maximum (FWHM) is 70 keV at the 1332 keV, there are many overlapping full energy peaks of natural radiation isotopes.…”
Section: Introduction mentioning
confidence: 99%