Radioactive characterization of phosphogypsum from Imbituba, Brazil

This research aims to characterize the content of natural occurring radionuclides in phosphogypsum stacks at Imbituba, Santa Catarina state, Brazil. 226Ra, 228Ra, 40K, 238U and 232Th were determined in PG, soils and sediment samples by gamma spectrometry using the hyper pure germanium detector and n...

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Bibliographic Details
Published in:Journal of environmental radioactivity Vol. 126; pp. 188 - 195
Main Authors: Borges, Renata Coura, Ribeiro, Fernando Carlos Araujo, Lauria, Dejanira da Costa, Bernedo, Alfredo Victor Bellido
Format: Journal Article
Language:English
Published: Kidlington Elsevier Ltd 01-12-2013
Elsevier
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Summary:This research aims to characterize the content of natural occurring radionuclides in phosphogypsum stacks at Imbituba, Santa Catarina state, Brazil. 226Ra, 228Ra, 40K, 238U and 232Th were determined in PG, soils and sediment samples by gamma spectrometry using the hyper pure germanium detector and neutron activation. The migration of radionuclides in the phosphogypsum profile did not show the same behavior for all sampling sites. The mean activity concentration of 226Ra was 95 Bq kg−1, which is far below the limit recommended by the U.S. Environmental Agency (USEPA) for its application in agriculture (370 Bq kg−1) and the Brazilian Commission of Nuclear Energy Resolution 113 that established a reference level of 1000 Bq kg−1 of 226Ra or 228Ra for the use of PG in agriculture as well as building materials. •Concentration of 238U and 232Th in the PG stack 1 indicated an igneous origin.•The origin of the stack 2 cannot be determined due the similar values.•Concentration of 226Ra is below the limit recommended for use in agriculture.•Distribution of radionuclides through the stacks profile was very heterogeneous.•Low concentrations of 226Ra and 228Ra in soils of the areas surrounding the stacks.
Bibliography:http://dx.doi.org/10.1016/j.jenvrad.2013.07.020
ObjectType-Article-1
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ISSN:0265-931X
1879-1700
DOI:10.1016/j.jenvrad.2013.07.020